The South
America Geoid 2000 workshop held at Escola Politécnica, Universidade de São
Paulo, from May 17 to19, 2000, was organized by IGeS (International Geoid
Service), SCGGSA (Sub-Commission for Gravity and Geoid in South America), CDC
(Committee for Developing Countries) and it was also supported by IAPSO
(International Association of the Physical Science of the Ocean). The workshop
had the following objectives:
·
To
assemble as many countries as possible from South America to compute a geoid
model.
·
To
encourage cooperation between oceanographers and geodesists for the computation
od geoid in coastal areas.
·
To
encourage every country to cooperate with SCGGSA for data delivery.
·
To
encourage every country to compute a local geoid model with the data available.
·
To
discuss different efforts for data acquisition in the continent.
The
countries that participated to the activities were the following:
Argentina,
Brazil, Chile, Ecuador, Paraguay and Uruguay.
The program
of the workshop (attached) addressed special attention to the geoid, but,
airborne gravity and the next special satellites: Champs, GRACE and GOCE
received attention too in a lecture.
A decisive
contribution to the success of the workshop came from the participation of
Riccardo Barzaghi (Italy), René Forsberg (Denmark) and Ole Andersen (Denmark).
One day and
half was dedicated to geoid computations. Every country had a computer
available with softwares to accomplish the different tasks: Stokes numerical
integration, fast Fourier techniques and fast collocation.
A few
meetings were also organized to discuss the following topics: SIRGAS, CDC, the
new structure of IAG and airborne gravity.
D. Blitzkow.
REPORT
OF THE 14TH INT. SYMPOSIUM ON EARTH TIDES (ETS2000)
The 14th
International Symposium on Earth Tides (ETS2000) was successfully held in
Mizusawa, Japan, during the period from August 28 to September 1, 2000. 137
participants from 21 countries reported fully on their results of continuing
researches on Earth tides and thus contributed to the progress of further
research of Earth and Planetary Tides.
1. Officers of the Commission
The President of the IAG Commission V (Earth Tides) was elected by the Council of IAG at the IUGG/IAG General Assembly held in Birmingham, UK, in July 1999.Before the opening session of the ETS2000, the President consulted opinion of the National Representatives of the Commission on proposal to ask Jacques Hinderer and Olivier Francis to continue their office until the next IUGG/IAG General Assembly to be held in Sapporo, Japan, in July 2003, and obtained their approval.
At the opening session of ETS2000, the Commission elected J. Hinderer as Vice-President and Francis as Secretary without a dissenting voice. Congratulation to Jacques Hinderer and Olivier Francis, and the best wishes for their future work.
3. ETC Homepage
Now, the ETC Homepage can be seen through the following address,
http://www-geod.kugi.kyoto-u.ac.jp/iag-etc/
4. 2nd ETC Medal
The ETC steering committee decided to award the 2nd ETC Medal (ETC Medal 2000) to the late Prof. Hans-Georg Wenzel for his outstanding contribution to international cooperation in earth tide research. His contribution to gravity and Earth tides researches is so well known through the papers more than 150. He is famous by development of a new tidal potential catalogue, a worldwide synthetic gravity tides model, and the Earth tides data processing package so called ETERNA. With grateful appreciation for the numerous services rendered by Prof. Hans-Georg Wenzel during his lifetime, all participants of ETS2000 paid one-minute's tribute to him with deepest sympathy. The ETC awarded the 2nd ETC Medal to Ms Marion Wenzel at the Opening Session of ETS2000 on August 28 2000 at Mizusawa, Japan.
5. ETC Working Groups
At the opening session of ETS2000, chairpersons of following Working Groups reported their activities,
Working Group 4 "Calibration of Gravimeters", (M.van Ruymbeke),
Working Group 5 "Global Gravity Monitoring", (B. Richter),
Working Group 6 "Earth Tides in Geodetic Space Techniques, (H. Schuh),
Working Group 7 "Analysis of Environmental data for the interpretation of gravity measurements", (G. Jentzsch).
The Earth Tide Commission thanks all members and chairpersons of WGs which have been active during the last period, for their fruitful work.
ETC accepted the conclusions of the reports of the Working Groups and decided according to their wishes:
To close Working Group 4 (Calibration of Gravimeters, Chairperson: M.van Ruymbeke).
To close Working Group 5 (Global Gravity Monitoring, Chairperson: B. Richter).
To extend for another 4 year term the activities of the Working Group 6 (Earth Tides in Geodetic Space Techniques) under the new chairperson-ship.
To extend for another 4 year term the activities of the Working Group 7 (Analysis of Environmental data for the interpretation of gravity measurements) under the new chairperson-ship.
To create Working Group 8 on "Gravitational
Physics" under the chairperson-ship of Prof. Lalu Manshinha to tackle
among others the following scientific problems: The Problem of Aberration: Modern
tidal position catalogs assume that the true position of the tide causing body
is responsible for the tidal forces, rather than the apparent position, as in
optical astronomy. The problem
may have consequences, as it may imply relative velocities between the gravity
and optical signals. This is a case for experts in Celestial Mechanics and in
Earth Tides. The Gravitational Shielding:There is currently no accepted theory
of gravity that incorporates or predicts gravitational shielding. The problem
is possibly different from the absorption of gravitational radiation by matter.
The Earth Tide community should think about, and search for, the consequences
of shielding.
6. Directing Board of the International Center for Earth Tides (ICET)
The ICET Directing Board (S.Takemoto (Chair), B.Ducarme, T.F.Baker, D.Crossley, H.T.Hsu and O. Francis (Non-voting member)) met together on August 29, 2000 at the Z-hall in Mizusawa. The main subject for discussion was "Future activity of ICET and re-organization of the IAG services". ICET-DB discussed on the GFFS (Gravity Field and Figure of the Earth Service) proposed by Prof. F. Sanso, which is a new Service including activities of BGI, IGeS and ICET.
Because of a restriction of time, ICET-DB could not draw a conclusion at Mizusawa and decided to continue our discussion by E-mail. ICET-DB will draw a conclusion not later than the end of October 2000.
7.
RESOLUTIONS adopted by the Earth Tide Commission
The Earth Tide Commission has adopted the following resolutions at the closing session of the 14th International Symposium on Earth Tides, August 28 - September 1, 2000, Mizusawa, Japan.
1/ Recognizing the importance of the
observation of tidal effects and of the determination of tidal parameters by
space geodetic techniques,
the ETC recommends
to continue this observational effort;
to compare the results obtained by different space geodetic techniques between each other and with the results of ground based tidal measurements.
2/ Recognizing the importance of the new international services on space geodetic techniques
the ETC recommends
that WG6 establishes or intensifies the cooperation with the analysis coordinators of these international services concerning the tidal modelling.
3/ Considering the new fields of tidal research in lunar and planetary geodesy
the ETC recommends
that the tidal community should take an active part in space missions related to lunar and planetary geodesy ;
requests a proper archiving of the data and metadata acquired during those missions and normal access to the world-wide geodetic community.
4/ Considering the increasing interest of the tidal community to lunar and planetary researches
the ETC recommends
that a session on tides on the planets should be included in the future earth tides symposia.
5/ Recognizing the importance of a global Earth coverage with superconducting gravimeters
for the study of weak geophysical signals,
for the determination of the liquid core resonance parameters,
for the study of the polar motion effects on gravity,
for the intercomparison of the load vectors derived from recent ocean tides models,
for the study of global and regional gravity changes to validate the results of the dedicated satellite missions,
the ETC recommends
to extend the GGP observation period for an
additional 6 year period starting July 2003, to maintain the existing sites and
to encourage the installation of new GGP stations especially in the Southern
hemisphere and in polar regions.
6/ Recognizing the fact that presently the calibration of the superconducting gravimeters participating to the world-wide GGP project is not homogeneous
the ETC recommends
that systematic calibration campaigns with absolute gravimeters should be planned and realized before the end of the current GGP observation period, through an international cooperative effort.
7/ Recognizing the importance to keep in operation several calibration techniques for gravimeters to allow a mutual accuracy control,
the ETC recommends
that inertial calibration platforms and moving mass calibration devices should continue to be developed or maintained besides more usual calibration methods such as intercomparison with absolute or well-calibrated relative instruments.
8/ Recognizing the importance of environmental data for the interpretation of tidal measurements the ETC recommends:
a/ to record the following parameters:
- The barometric pressure, temperature,
precipitation, and ground water level. The sampling rate for the recording of
environmental parameters should correspond to the sampling rate of the
geodynamic data observed. A sufficient resolution and accuracy of the
measurements of the environmental parameters should be granted.
- Although the difficulties of monitoring soil
moisture are recognized, its is recommended to undertake efforts to realize a
continuous monitoring of this parameter.
- The monitoring of wind is also recommended because wind might produce short-period noise as well as long-period modulations.
b/ to correct gravity data in long term studies
for local (diameter 100 km), regional (diameter 2000 km), and global
atmospheric pressure signals as all three produce significant effects.
c/ to develop correction models for gravity, tilt, and strain related to:
- ground water table variations
- snow, rain and soil moisture
- stress resulting from temperature variations
9/ Noting the importance for tidal measurements of accurate error estimates
and appreciating that such estimates can be made only if the power spectral density of the noise is known
the ETC recommends
to show noise spectra as Power Spectral Density expressed in unit 2/ frequency.
10/ On behalf of all participants of the 14th International Symposium on Earth Tides, the ETC thanks the Japanese National Committee for Geodesy, the Science Council of Japan, the Geodetic Society of Japan, the National Astronomical Observatory of Japan, the City of Mizusawa and the Iwate Prefecture for their generous support to the Symposium.
11/ ETC thanks the Local Organising Committee :
Masatsugu Ooe (Chairman), Tadehiro Sato (Secretary) , Jiro Segawa (President of
Geodetic Society of Japan) and the staff, for their wonderful welcome and their
many efforts in making the 14th International Symposium on Earth Tides a great
scientific success.
8. IAG
Travel Awards
The following 5 persons are winners of IAG Travel Award.
Alexander Kopaev, (Moscow, Russia), Janusz Bogusz, (Warsaw, Poland), Carla Braitenberg, (Trieste, Italy), Sun He-Ping (Wuhan, P.R. China), Zhigen Yang (Shanghai, P.R. Chin)
9.
Publication of the ETS2000
Proceedings of scientific papers will be published as a
special issue of the Jour. Geod. Soc. Japan. Other Report on the ETS2000 including the list of participants
will be appeared in the next issue of BIM
10. Next Symposium
During the ETS2000, Canadian Colleagues (Profs. D. Smylie, L. Mansinha and S. Pagiatakis) kindly offered to have the next (15th) International Symposium on Earth Tides in Canada in 2004. The Earth Tide Commission acknowledges the receipt of this invitation.
Shuzo Takemoto
IAG/IAPSO JOINT WORKING GROUP ON GEODETIC EFFECTS OF NONTIDAL OCEANIC
PROCESSES
Meeting
held on March 29, 2001 in Nice, France in conjunction with the XXVI General
Assembly of the European Geophysical Society (EGS) during which presentations
were given by R. Gross, T. Sato, B. Chao, and A. Brzezinski.
The oceans have a major impact on global
geophysical processes of the Earth. Nontidal changes in oceanic currents and
ocean-bottom pressure have been shown to be a major source of polar motion
excitation and also measurably change the length of the day. The changing mass
distribution of the oceans causes the Earth's gravitational field to change and
causes the center-of-mass of the oceans to change which in turn causes the
center-of-mass of the solid Earth to change. The changing mass distribution of
the oceans also changes the load on the oceanic crust, thereby affecting both
the vertical and horizontal position of observing stations located near the
oceans.
Recognizing
the important role that nontidal oceanic processes play in Earth rotation
dynamics, an IAG/IAPSO Joint Working Group on Geodetic Effects of Nontidal
Oceanic Processes was formed at the XXII General Assembly of the IUGG in Birmingham.
The objective of this IAG/IAPSO Joint Working Group is to investigate the
effects of nontidal oceanic processes on the Earths rotation, deformation,
gravitational field, and geocenter, and to foster interactions between the
geodetic and oceanographic communities in order to promote greater
understanding of these effects. R. Gross described the International Earth
Rotation Service (IERS) Special Bureau for the Oceans (SBO). The IERS Special
Bureau for the Oceans is one of seven Special Bureaus of the IERS Global
Geophysical Fluids Center
(GGFC)
which was established on January 1, 1998 in order to help relate dynamical
properties of the atmosphere, oceans, mantle, and core to motions of the Earth,
including its rotation. In particular, the IERS Special Bureau for the Oceans
is responsible for collecting, calculating, analyzing, archiving, and
distributing data relating to nontidal changes in oceanic processes affecting
the Earth's rotation, deformation, gravitational field, and geocenter. The
oceanic products available through the IERS SBO are produced primarily by
general circulation models of the oceans that are operated by participating
modeling groups and include oceanic angular momentum, center-of-mass, bottom
pressure, and torques. Through the IERS SBO web site at
http://euler.jpl.nasa.gov/sbo, oceanic data can be downloaded and a
bibliography of publications pertaining to the effect of the oceans on the
solid Earth can be obtained. Currently, two different oceanic angular momentum
data sets are available. The IERS SBO is one possible source of data that can
be used by the IAG/IAPSO Joint Working Group in their investigations on the
geodetic effects of nontidal oceanic processes.
T.
Sato discussed the effect of sea surface height variations on superconducting
gravimeter measurements. Good agreement with gravity measurements at 3
different sites were obtained using results from both an ocean model and from
TOPEX/POSEIDON measurements which had been corrected for the steric changes in
sea surface height that have no gravitational signature. This study of the
results of gravity observations clearly shows that gravity measurements from
satellites and on the ground have an important role to play when studying the
effects of oceanic variability on the local and global geophysical processes of
the Earth. He then presented plans for deploying ocean- bottom pressure
recorders off the coast of Japan at TOPEX and Jason-1 crossover points.
As
the mission scientist for the GRACE Mission Office, B. Chao discussed the use
of oceanic general circulation models to dealias GRACE gravitational field
measurements. The GRACE project is currently planning on producing
gravitational field solutions at monthly intervals. Since the distribution of
mass within the oceans changes more rapidly than this, the gravitational effect
of this rapid oceanic mass movement will be aliased in the monthly solutions
unless it is modeled and removed from the GRACE measurements. A barotropic, or
perhaps a baroclinic, ocean model driven by either NCEP or ECMWF surface winds
and fluxes will likely be operated by the GRACE project in order to model and
remove the high frequency variations in oceanic mass distribution that will not
be sampled by the GRACE monthly gravitational field solutions. Since this
scheme will most likely not be able to perfectly remove the aliased signals,
the user community should be cognizant of the uncertainties that will be
introduced by this procedure. Similar aliasing effects are also expected to
occur due to rapid atmospheric, hydrologic, and ocean-tidal mass movement, and
the GRACE project is also planning to use atmospheric and ocean tide models to
similarly remove these effects.
A.
Brzezinski summarized the results on the oceanic excitation of the Chandler
wobble that he and J. Nastula presented at the 33rd COSPAR Scientific Assembly
held in Warsaw, Poland during July 16-23, 2000 (to appear in Advances in Space
Research). Using the POLE98 polar motion series, the NCEP/NCAR reanalysis
atmospheric angular momentum series obtained from the IERS Special Bureau for
the Atmosphere, and the 11-year-long oceanic angular momentum (OAM) series of
Ponte et al. (J.Geophys. Res., vol. 104, pp. 23393-23409, 1999) obtained from
the IERS SBO, they demonstrated that the OAM series is highly coherent with the
lacking non-atmospheric excitation of the observed Chandler wobble signal. In
terms of the excitation power, the combined effect of the atmosphere and ocean
explains about 80% of the free wobble, which agrees to within 1-sigma uncertainty
with the result recently published by R. Gross (Geophys. Res.Lett., vol. 27, pp. 2329-2332,
2000).
The
next meeting is scheduled to be held in conjunction with the XXVII General
Assembly of the EGS that will be held in Nice, France during April 22-26, 2002.
The exact date and time of this meeting will be announced later. In order to
receive announcements of this and all future meetings, please contact Richard
Gross at richard.Gross@jpl.nasa.gov.
R.
Gross
FIRST INTERNATIONAL SYMPOSIUM ON ROBUST STATISTICS AND FUZZY TECHNIQUES
IN GEODESY AND GIS, ZURICH, SWITZERLAND, MARCH 12-16, 2001
The
'First International Symposium on Robust Statistics and Fuzzy Techniques in
Geodesy and GIS' took place at the Swiss Federal Institute of Technology (ETH)
in Zurich, Switzerland, from March 12-16, 2001. It was initiated by the members
of the Special Study Group (SSG) 4.190 of the International Association of
Geodesy (IAG) on 'Non-probabilistic assessment in geodetic data analysis'. It
was organized by Prof. A. Carosio, ETH Zurich,, and Dr. H. Kutterer, DGFI
Munich, chairman of the SSG. Nearly 60 participants from 15 countries attended
the symposium.
The
program of the meeting consisted of applications of robust statistics and fuzzy
theory, mainly in the fields of geodetic engineering, deformation analysis,
geographic information systems, satellite-based positioning (GPS),
and
photogrammetry. Therefore five technical sessions and a panel discussion were
organized. In advance, two tutorials were given on robust statistics (A.
Carosio) and on fuzzy logic (H. Kutterer, S. Schön) on monday, March 12.
The
symposium was opened on tuesday, March 13, with a welcome address by Prof. B.
Heck, University of Karlsruhe, president of the IAG section IV. Two invited
lectures followed. The first one was presented by Prof. F. Hampel, ETH Zurich,
who considered both the historical development of robust statistics and recent
mathematical problems. The second one was given by Prof. R. Viertl, Technical
University of Vienna, who motivated the non-precision approach and showed the
application of statistical methods to non-precise data based on the extension
principle of fuzzy theory. H. Kutterer gave the last lecture in this session on
a general viewpoint of uncertainty assessment.
In
the technical session on geodetic engineering four talks were focussed on
robust statistics: kinematic positioning (Y. Yang), the BIBER estimator (F.
Wicki), and the reliability of robust estimators (M. Berber, S. Hekimoglu). One
talk considered the use of interval mathematics for the measurement
uncertainties (S. Schön). L. Soukup discussed 'least squares without
minimization'.
The
second technical session on deformation analysis showed a variety of different
assessment methods: a conic fitting algorithm (O. Akyilmaz), inference on
deformation measures like strain tensors (J. Cai), fuzzy deformation analysis
(K. Heine), Plucker coordinates (R. Jurisch), artificial neural networks (J. B.
Miima), modelling alternatives in deformation measurements (D. Rossikopoulos),
and maximum correlation adjustment (F.
Neitzel).
The third session which was on Geographic Information Systems (GIS) consisted of four talks, three using fuzzy logic (G. Joos, S. Keller, E. Stefanakis) and one on robust estimation techniques (E. Kanani). The following session was dedicated to GPS data processing and analysis: real-time prediction of failures (C. Dacheng), robust techniques (A. Wieser, Y. Yang), and fuzzy methods (S. Leinen, H. Kutterer).
The last technical session of the symposium was on photogrammetry, remote sensing, and image processing. F. Sanso discussed the Wiener-Kolmogorov prediction problem with the application to digital terrain models. L. Mussio considered semantic ambiguity questions for pattern recognition. M. Scaioni showed the use of the LMS estimator for outlier rejection in automatic aerial triangulation.
The
last day of the symposium started with an introductory talk by F. Sanso on the
challenges for the IAG in data analysis in the fields of geodesy and GIS,
especially regarding the modelling of uncertainty by probabilistic and
non-probabilistic
techniques. A panel discussion on data analysis within IAG closed the
symposium.
The
proceedings of the symposium are published as Report No. 295 of the Institute
of Geodesy and Photogrammetry of the Swiss Federal Institute of Technology
Zurich (ETH). Further information can be found on the website of the IAG SSG
4.190. The address is www.dgfi.badw.de/ssg4.190. Last but not least a warm
thanks goes to the local committee around A. Carosio at the ETH Zurich for the
excellent organization of the symposium.
H. Kutterer
IAG Subcommission
for Europe (EUREF)
The 11th symposium of the EUREF Subcommission
was held in Dubrovnik from 16. - 19.5.2001. Proceedings will
be published in AMitteilungen des Bundesamtes für Kartographie und Geodäsie@.
On this symposium the following resolutions were
adopted:
Resolution No. 1
The IAG Subcommission for Europe (EUREF)
recognising that
-in May/June 1994 the
EUREF-SLOCRO-94 campaign in Slovenia and Croatia was observed,
-in September/October
1995 the Slovenia-95 and CROREF-95 campaigns in Slovenia and Croatia were
observed,
-in August/September
1996 the CROREF-96 campaign in Croatia was observed,
and all the results
were submitted to the EUREF Technical Working Group as a combined
EUREF-CRO-94/95/96 solution, where
it was accepted as class B standard (about 1 cm at the epoch of observations)
endorses the
subsets of points for Croatia submitted to the EUREF Technical Working Group as
improvements and extensions of EUREF89,
but considering that two points in
Croatia observed during the EUREF-CROSLO-94 campaign were destroyed,
recommends that all
old Croatian points should be deleted from the EUREF database and replaced by
the subset of points selected from the EUREF-CRO-94/95/96 solution.
Resolution No. 2
The IAG Subcommission for Europe (EUREF)
considering
- the
availability of the ITRF2000 as an improved and accurate realisation of the
ITRS,
-the improved
determination of the rotation of the Eurasian plate using ITRF2000 site
velocities,
recommends to
replace the NNR-NUVEL-1A rotation rate values by the ones derived from ITRF2000
in the transformation formula linking ETRS89 to ITRS.
Resolution No. 3
The IAG Subcommission for Europe (EUREF)
recognising the significant
practical and scientific value of the EVRS
noting the usefulness of improving its realisation
EVRF2000
asks national levelling data providers to UELN/EUVN
to inform the Technical Working Group on the tidal system and other corrections
used,
recommends that in the future
levelling data be submitted in the zero tidal system according to the EVRS
definition and corresponding IAG resolution 16, 1983.
Resolution No. 4
The IAG Subcommission for Europe (EUREF)
recognising
-the European
Vertical GPS Reference Network (EUVN) with its GPS-derived ellipsoidal heights
and levelled connections to UELN,
-the definition of
the European Vertical Reference System EVRS with its first realisation UELN
95/98, called EVRF2000,
considering
-this implicit
pointwise realisation of a European geoid consistent with both ETRS89 and EVRS,
-the existence of a
large number of regional and local geoids in Europe,
-the urgent need by
the navigation community for a height reference surface,
asks its Technical
Working Group and the European Subcommission of the IAG IGGC (International
Gravity and Geoid Commission) to take all necessary steps to generate a
European geoid model of decimetre accuracy consistent with ETRS89 and EVRS.
Resolution No. 5
The IAG Subcommission for Europe (EUREF), which held
its eleventh EUREF symposium in Dubrovnik from May 16-18, 2001, expresses its
heartfelt thanks to the Local Organising Committee, its chairman Zeljko Bacic and the State Geodetic
Administration, as well as the Cadastre Office in Dubrovnik and the
International Centre of Croatian Universities, for organising the symposium and
for the excellent arrangements resulting in a very successful meeting.
Joao Agria Torres, Lisbon: jatorres@ipcc.pt
Helmut Hornik, Munich: hornik@dgfi.badw.de
FIRST INTERNATIONAL SYMPOSIUM ON ROBUST
STATISTICS AND FUZZY TECHNIQUES IN GEODESY AND GIS
ZURICH,
SWITZERLAND, MARCH 12-16, 2001
The
'First International Symposium on Robust Statistics and Fuzzy Techniques in Geodesy
and GIS' took place at the Swiss Federal Institute of Technology (ETH) in
Zurich, Switzerland, from March 12-16, 2001. It was initiated by the members of
the Special Study Group (SSG) 4.190 of the International Association of Geodesy
(IAG) on 'Non-probabilistic assessment in geodetic data analysis'. It was
organized by Prof. A. Carosio, ETH Zurich, and Dr. H. Kutterer, DGFI Munich,
chairman of the SSG. Nearly 60 participants from 15 countries attended the
symposium.
The
program of the meeting consisted of applications of robust statistics and fuzzy
theory, mainly in the fields of geodetic engineering, deformation analysis,
geographic information systems, satellite-based positioning (GPS), and
photogrammetry. Therefore five technical sessions and a panel discussion were
organized. In advance, two tutorials were given on robust statistics (A.
Carosio) and on fuzzy logic (H. Kutterer, S. Schön) on monday, March 12.
The
symposium was opened on tuesday, March 13, with a welcome address by Prof. B.
Heck, University of Karlsruhe, president of the IAG section IV. Two invited
lectures followed. The first one was presented by Prof. F. Hampel, ETH Zurich,
who considered both the historical development of robust statistics and recent
mathematical problems. The second one was given by Prof. R. Viertl, Technical
University of Vienna, who motivated the non-precision approach and showed the
application of statistical methods to non-precise data based on the extension
principle of fuzzy theory. H. Kutterer gave the last lecture in this session on
a general viewpoint of uncertainty assessment.
In
the technical session on geodetic engineering four talks were focussed on
robust statistics: kinematic positioning (Y. Yang), the BIBER estimator (F.
Wicki), and the reliability of robust estimators (M. Berber, S. Hekimoglu). One
talk considered the use of interval mathematics for the measurement
uncertainties (S. Schön). L. Soukup discussed 'least squares without
minimization'.
The
second technical session on deformation analysis showed a variety of different
assessment methods: a conic fitting algorithm (O. Akyilmaz), inference on
deformation measures like strain tensors (J. Cai), fuzzy deformation analysis
(K. Heine), Plucker coordinates (R. Jurisch), artificial neural networks (J. B.
Miima), modelling alternatives in deformation measurements (D. Rossikopoulos),
and maximum correlation adjustment (F. Neitzel).
The
third session which was on Geographic Information Systems (GIS) consisted of
four talks, three using fuzzy logic (G. Joos, S. Keller, E. Stefanakis) and one
on robust estimation techniques (E. Kanani). The following session was
dedicated to GPS data processing and analysis: real-time prediction of failures
(C. Dacheng), robust techniques (A. Wieser, Y. Yang), and fuzzy methods (S.
Leinen, H. Kutterer).
The
last technical session of the symposium was on photogrammetry, remote sensing,
and image processing. F. Sanso discussed the Wiener-Kolmogorov prediction
problem with the application to digital terrain models. L. Mussio considered
semantic ambiguity questions for pattern recognition. M. Scaioni showed the use
of the LMS estimator for outlier rejection in automatic aerial triangulation.
The
last day of the symposium started with an introductory talk by F. Sanso on the
challenges for the IAG in data analysis in the fields of geodesy and GIS,
especially regarding the modelling of uncertainty by probabilistic and
non-probabilistic techniques. A panel discussion on data analysis within IAG
closed the symposium.
The
proceedings of the symposium are published as Report No. 295 of the Institute
of Geodesy and Photogrammetry of the Swiss Federal Institute of Technology
Zurich (ETH). Further information can be found on the website of the IAG SSG
4.190. The address is www.dgfi.badw.de/ssg4.190. Last but not least a warm
thanks goes to the local committee around A. Carosio at the ETH Zurich for the
excellent organization of the symposium.
H.
Kutterer
SECOND INTERNATIONAL SYMPOSIUM: GEODYNAMICS OF THE ALPS-ADRIA AREA BY MEANS OF TERRESTRIAL AND SATELLITE METHODS
Last autumn
the beautiful city of Dubrovnik became a meeting point of the international
geodetic community again. It was after a long interruption lasting almost
exactly 9 years. In 1989 the participants of the First International Symposium
on Gravity Field Determination and GPS-Positioning in the Alps-Adria Area left
the Dubrovnik Inter-University Centre, the venue of the symposium, with a
believe that they will reconvene at the same place in four years. However, the reality
and the difficult time in this area prepared another development.
Only last year the reconstructed
Inter-University Centre of Dubrovnik became the venue of the Second
International Symposium: Geodynamics of the Alps-Adria Area by means of
Terrestrial and Satellite Methods which was held here between September 28 and
October 2, 1998. The symposium was sponsored by the International Association
of Geodesy and it also had a generous local support. In total 43 interesting
papers were presented by scientists coming from 9 different countries to the
audience of over 70 participants. The meeting was organized by Prof. K. Èoliæ
(as the local organizer, University of Zagreb) and Prof. H. Moritz (as the
international co-organizer).
At the opening session a number of
addresses was presented by local and international representatives. Then the
participants of the symposium heard a very interesting lecture by K. Èoliæ and
H. Moritz on Rudjer Boškoviæ (1711-1787), a native of Dubrovnik and a
remarkable figure in the history of modern European science who also made
considerable contributions to geodesy and geophysics.
The symposium itself was subdivided
into 10 session: 3 sessions were devoted to Geodynamics and chaired
subsequently by H. Seeger, G. Rossi and C. Marchesini. Then G. Schmitt chaired
a session on Geoid, F. Vodopivec a session on GPS, P. Holota a session on
Positioning and Gravity, P. Pesec chaired a session on CERGOP, E. Groten a
session on the Theory and finally two session devoted to practical works were
chaired by A. Zeman and K. Kaniuth.
The
first session on Geodynamics started with a paper by Hussein A. Abd-Elmotaal who discussed inverse
Vening Meinesz Moho depths for the Eastern Alps. Then Z. Altiner et al.
presented a talk on crustal deformations in the Adriatic sea area as inferred
on the basis of GPS observations. Subsequently, E. Groten and St. Leinen
treated deformation monitoring around a large viaduct close to Istambul using
GPS and levelling. Finally, F. Vodopivec and D. Kogoj discussed the geodynamics
in Slovenia and A. Zeman approached a problem of estimating vertical dynamics
on the territory of former Austro-Hungarian empire on the bases of results of
historical levellings.
The
second session on Geodynamics was opened by A. Caporali who in his talk attacked a problem of
constraining the rheology of continental lithosphere near Orogens with the use
of Bouguer gravity anomalies. The programme of the session continued with a
paper by D. Miškoviæ on problems of national reference frame and geodynamic
investigations in Slovenia. Then B. Richter et al. discussed absolute gravity
measurements in Croatia approached as a standardized base net for geodynamic,
height and gravity studies. Finally, G. Schmitt and C. Marchesini informed
about geodetic activities with respect to geokinematics in Friuli and the
Eastern Alps.
At
the last session on Geodynamics E. Prelogiæ et al. treated recent tectonic movements and earthquakes in
Croatia and then G. Rossi and M. Zadro discussed geodynamic processes at the
northern boundary of Adria plate, especially strain-tilt measurements and
modelling. The session was closed with a paper by P. Vyskoèil (presented in
absentia by H. Moritz) on the map of vertical movements of Dinaridies Eastern
Alps, Pannonian Basin and the Bohemian Massif.
As already mentioned, together with
geodynamics oriented sessions there were also sessions on closely related
topics in Dubrovnik.
The paper by H. Abd-Elmotaal et al.
stared the Geoid session. The talk
was devoted to the influence of implementing the seismic Moho depths in geoid
computation. K. Arsov and H. Sünkel approached the problem of influence of the
resolution of DEM in gravity reduction. They used fractal models of the
topography for their analyses. E. Groten and K. Seitz discussed a detailed
geoid of Germany based on EGM96. N. Kühtreiber presented a recent geoid
computation for Audtria and N. Kühtreiber et al. then concluded the session
with results of a geoid computation for the central part of the Alps-Adria
area.
At
the GPS session A.
Caporali devoted his talk to an analysis of a GPS network along the Alpine Arc.
K. Kaniuth and Stuber attacked the problem of accuracy and reliability of
height estimates in regional GPS networks. H. Seeger et al. contributed with
results of a re-computation of the EUREF GPS campaigns in Croatia and Slovenia.
Finally, M. Marjanoviæ and Lj. Rašiæ discussed the results of the EUREF 1997
GPS campaign in Croatia.
Also
the Gravity was discussed at a separate session. Here J. Flury brought an information on a
local gravity filed determination in the Estergebirge. E. Gueguen and C.
Doglioni discussed the geodynamic evolution of the Appeninic subduction. R.
Marjanoviæ-Kavanagh contributed with experiences with a new digital tiltmeter
and G. and G.K. Walach presented a Bouguer gravity map of Styria.
The
session on CERGOP
was opened by D. Miškoviæ et al. They presented results of the GPS-measurements
in the Bovec-Tolmin earthquake region. H. Düller and P. Pesec contributed with
information on the Austrian permanent GPS-network. P. Pesec then summarized the
current status of the Austrian IDNDR project (Crustal dynamics of the Adriatic
microplate and the adjacent East-Alpine area). Finally, J. Šimek discussed
possible topics for the international cooperation within CEI/CERGOP on the
background of current European project.
Within
theory oriented session the audience heard a contribution by P. Holota on Galerkin's method in
the determination of the disturbing potential. Then an analysis of a straight
line equation by M. Lapaine and new concepts of boundary value problems of
physical geodesy after GPS presented by H. Moritz.
Finally, two working sessions were devoted to practical works. Here K. Èoliæ
et al. contributed with two talks: on the survey of the Plitvice-lakes (the
phenomenon in the Karst of the Dinaric Alps with satellite and terrestrial
measurements) and on the 3-D geodynamic network of broader area of the city of
Zagreb. Then Z. Kapoviæ et al. presented results of the geodynamic research of
the historical center in the city of Dubrovnik with precise geometric
levelling. Subsequently M. Plazibat approached linear transformation between
old and new national networks by means of finite elements and M. Solariæ
discussed a visibility analysis of GPS satellites in Central Europe.
At the closing session (chaired by
B. Gajèeta) the participants adopted a number of important resolutions. They
are as follows:
Resolution 1 - The Symposium,
recognizing the need of a regular exchange of
ideas and research results in the field of the ‘tectonic scenario’ in the wider
Alps-Adriatic region and
having in mind the hospitality of the Croatian
colleagues,
recommends regular meetings in a four years
cycle in the city of Dubrovnik, with one intermediate meeting at a different
place between two of these symposia.
Resolution 2 - The Symposium,
recognizing the need of further research
concerning the ‘tectonic scenario’ in the wider Alps-Adriatic region and of
studies concerning earthquake disaster prevention in this region,
recommends the establishment of a
corresponding Special Study Group in Section V ‘Geodynamics’ of IAG, with due
relation to CERGOP.
Resolution 3 - The Symposium,
considering
that the area of the Plitvice Lakes is not only a National Heritage under the
patronage of UNESCO (No. 148), but also very important for different reasons
such as Dinaric Karst geology, effect of tourism etc. and
considering
that important geodetic and geodynamical studies have already been performed by
the Geodetic Faculty of Zagreb University,
recommends that
this area be declared an International
Geodynamic Test Area in which all relevant geodetic methods are to be
applied.
Resolution 4 - The Symposium,
recognizing the need of permanent GPS stations and
considering the existence of such stations e.g. in Croatia
and Slovenia.
recommends the establishment of at least one permanent
GPS station on the territory of Bosnia and Herzegovina.
Resolution 5 - The Symposium,
recognizing the great and successful efforts of
Prof. Èoliæ and Prof. Moritz and their staff in preparing and organizing this
symposium and
appreciating the importance of the topics under
consideration for applied and theoretical surveying, geodesy, geodynamics and
related practical activities by universities and state organizations in and
around the Alpine-Adriatic Area up to the Panonnian Basin,
expresses its sincere thanks for the
wonderful days in the beautiful city of Dubrovnik, which is under the patronage
of UNESCO (No. 149), and in the stimulating environment of IUC in free Croatia.
The
scientific programme of the symposium was enriched by the presentation of the
book by H. Horitz: Science, Mind and the Universe (U. Wichmann Vlg.,
Heidelberg, 1995) and its translation into Croatian. On this occasion an
introductory lecture was held by Acad. N. Trinajstiæ who gave an interesting
outline of philosophy and discussed its contemporary trends.
The participants of the symposium
spent nice and well organized time together and during an interesting excursion
had a possibility to learn more about the marvelous city of Dubrobnik and its
beautiful surrounding. The symposium was a clear success. The Proceedings will
be published by the Geodetic Survey of Croatia.
P. Holota
REPORT ON THE INTERNATIONAL CONFERENCE ON
TECHNICAL ASPECTS OF MARITIME BOUNDARY DELINEATION AND DELIMITATION, INCLUDING
UNCLOS ARTICLE 76 ISSUES (ABLOS), MONACE, 9-10 SEPTEMBER, 1999.
Seventy-six attendees from twenty-nine
countries were present at the Conference. In addition the International
Hydrographic Bureau (IHB) personnel, members of the UN Commission on the Outer
Limits of the Continental Shelf and the UN Division of Ocean Affairs and Law of
the Sea participated. The sessions and papers were organised by the Conference
Committee chaired by P. Vaniçek, chairman of ABLOS, and the Conference
Proceedings, containing the 26 paper presented, will be produced by the IHB.
The Conference was divided into four sessions over a span of two days. In the first session, “Issues concerning the UN Commission on the Limits of the Continental Shelf”, convened by G. Carrera, topics related to the approach of the UN CLCS to submissions made by coastal states were considered in contributions presented by members of the Commission. The following papers were delivered: CROKER, Peter, CLCS Member (Ireland), “The mandate and work of the Commission on the Limits of the Continental Shelf”.HINZ, Karl, CLCS Member (Germany), “A review of continental margins of the world”. LAMONT Iain, CLCS Member (New Zealand), “Formulating the New Zealand Continental Shelf Claim: A First Step”. BREKKE, Harald, CLCS Member (Norway), "Uncertainties and errors in sediment thickness”. CARRERA, Galo, CLCS Member (Mexico) “Wide continental margins of the world: a survey of marine scientific requirements and international regional cooperation needs posed by the implementation of Article 76 of UNCLOS”. ALBUQUERQUE, Alexandre and CARRERA, Galo, CLCS Members (Brazil and Mexico) “Information on the outer limits of the extended continental shelf”.
The second session, “Geodetic issues, with emphasis on errors in maritime boundaries and how to reduce them”, convened by B.G. Harsson, dealt with specifically geodetic problems of delineation and delimitation of maritime boundaries. The following papers were delivered: CARRERA, Galo, (Canada) "The impact of the seabed roughness on the location of the outer limits of the extended continental shelf". GROTEN, Erwin, (Germany) "Coastal Boundaries and Vertical Datums. VANIÇEK, Petr, (Canada) "Propagation of errors from shore baselines seaward”.SJOBERG, Lars, M Fan and Milan Horemuz, (Sweden) "Accuracy of computed points on a median line, factors to be considered", MURPHY, Brian, Philip Collier, David Mitchel andl Bill Hirst., (Australia) "Maritime zone boundary generation from straight baselines defined as geodesics”. OSZCZAK, Stanislaw, A.Wasilewski, Z.Rzepecka (Poland) " RTK/ DGPS service in maritime boundary delimitations". ELEMA, I. and Kees de JONG, (The Netherlands) "The determination of boundaries at sea between Belgium and The Netherlands".
The third session, “Tools needed for boundary
delimitations”, convened by R. Macnab, dealt specifically with hardware and
software that would be necessary to obtain the data to substantiate a
continental shelf claim. The following papers were delivered: PALMER, Hal,
Lorin Pruett, and Kurt Christensen, (USA), "GIS applications to maritime
limit and boundary delimitation”. MONAHAN, David, Michael S. Loughridge,
Meirion T Jones, Larry Mayer, (Canada, USA, UK) “A
model for using publicly available data and methodologies to begin preparing a
claim to an extended continental shelf under article 76 of the United Nations
Convention on Law of the Sea (UNCLOS)”. MONAHAN, David and Larry Mayer,
(Canada) “An examination of publicly available bathymetry data sets using
digital mapping tools to determine their applicability to Article 76 of
UNCLOS”. HIRST, Bill, Brian Murphy and Phil Collier, (Australia) "An
Overview of Australian Maritime Zone Boundary Definition”. BORISSOVA, Irina
Philip A. Symonds, Robin Gallagher, Bruce C. Cotton and Gail Hill, (Australia)
"A set of integrated tools based on ArcView for defining the outer limit
of Australia's continental shelf". BENNETT, John, (USA) “Contrast of the
‘Surface of Directed Gradients’ with the ‘Surface of Maximum Curvature’ to
compute the foot of the continental slope”. HARDING, Jennifer, Herman Varma,
John Hart and Ron Macnab, (Canada) “The HH code: facilitating the management,
manipulation, and visualization of bathymetric data”.
In the last session, “Other issues and case
studies (not necessarily related to Article 76)”, convened by C. Rizos,
specific issues and case studies were the subjects of discussion. The following
papers were delivered: MONAHAN, David and David Wells, (Canada) “Achievable uncertainties
in the depiction of the 2500m contour and their possible impact on continental
shelf delimitation”. MACNAB, Ron, (Canada)
"Article 76 in the Arctic - a catalyst
for international collaboration". CHERKASHOV, Georgi, A., Gramberg I.S.
Makorta A.P., Kaminsky V.D., Naryshkin G.D., Poselov V.A., Sorokin M.Yu.
(Russia) “Bathymetry and Deep Structure of the Arctic Continental Margin of
Russia in the context of article 76 UN Convention on the Law of the Sea”.
COAKLEY, Bernard, (USA) “Contribution of the SCICEX Project Towards the
Implementation of Article 76 of the UN Convention on the Law of the Sea in the
Arctic Ocean”. SYMONDS, Phil, (Australia) “Austalia’s approach to defining its
extended continental shelf: progress and issues arising”.
The Conference, staged in the beautiful new
offices of IHB, was considered a great success and a possibility that a
bi-annual ABLOS-sponsored conference could become a regular international
venture in Monaco was discussed. It was the first time that the IHB offices have
been utilised for a conference of this format and it was evident that the
facilities would not be adequate to support a conference wit a larger number of
participants. It is anticipated that the assistance of the Principality of
Monaco will have to be sought if this was to become a regular venture.
P.
Vaniçek
MEETING REPORT OF THE IAG/IAPSO JOINT WORKING GROUP ON GEODETIC EFFECTS
OF NONTIDAL OCEANIC PROCESSES HELD IN CONJUGATION WITH THE EGS XXV GENERAL
ASSEMBLY, NICE, FRANCE, APRIL, 2000.
The oceans have a major impact on global geophysical
processes of the Earth. Nontidal changes in oceanic currents and ocean-bottom
pressure have been shown to be a major source of polar motion excitation and
also measurably change the length of the day. The changing mass distribution of
the oceans causes the Earth's gravitational field to change and causes the
center-of-mass of the oceans to change which in turn causes the center-of-mass
of the solid Earth to change. The changing mass distribution of the oceans also
changes the load on the oceanic crust, thereby affecting both the vertical and
horizontal position of observing stations located near the oceans. Products of
oceanic general circulation models (OGCMs) have been used to study these and
other geodetic effects of nontidal oceanic processes. Data assimilation systems
similar to those employed in numerical weather prediction are beginning to be
used with OGCMs to improve their fidelity. In the near future, time-varying
gravitational field measurements, which over the oceans can be interpreted as
time-varying ocean-bottom pressure measurements, will be available from the
CHAMP and GRACE satellites. The assimilation of these new data types into OGCMs
can be expected to further improve the accuracy of global ocean models, and
hence the accuracy of the predicted effects of oceanic processes on the Earth's
rotation, deformation, gravitational field, and geocenter.
Recognizing the important
role that nontidal oceanic processes play in Earth rotation dynamics, an IAG/IAPSO
Joint Working Group on Geodetic Effects of Nontidal Oceanic Processes was
formed at the XXII General Assembly of the IUGG in Birmingham. The objective of
this IAG/IAPSO Joint Working Group is to investigate the effects of nontidal
oceanic processes on the Earth_s rotation, deformation, gravitational field,
and geocenter, and to foster interactions between the geodetic and
oceanographic communities in order to promote greater understanding of these
effects. A meeting of this IAG/IAPSO Joint Working Group was held on April 27,
2000 in Nice, France in conjunction with the 25th General Assembly of the
European Geophysical Society during which presentations were given by Rui
Ponte, Chris Hughes, and Richard Gross.
Rui Ponte discussed an
oceanographic data assimilation system being created by collaborators from the
Massachusetts Institute of Technology (MIT), the Scripps Institution of
Oceanography, and the Jet Propulsion Laboratory. The ocean model component of
the data assimilation system, originally developed at MIT, is currently run on
a 2x2 degree horizontal grid with constant mixing coefficients and a simple
convective adjustment scheme. Future improvements will include finer
resolution, more realistic mixed layer physics and eddy parameterizations, and
relaxation of the volume conserving formulation. The oceanographic data
currently being assimilated include altimetric measurements of sea surface
height, hydrographic sections, and sea surface temperature measurements. Other
types of data (e.g., floats, XBT profiles) will also be included in the future.
Routine calculation of oceanic angular momentum and torque quantities from the
output of the assimilation system is envisioned.
Chris Hughes described the
GLObal Undersea Pressure (GLOUP) data bank. For more information about GLOUP
and/or to obtain the series of historical ocean-bottom pressure measurements
see the GLOUP home page at http://www.pol.ac.uk/psmslh/gloup/gloup.html.
Richard Gross described
the International Earth Rotation Service (IERS) Special Bureau for the Oceans
(SBO). The IERS Special Bureau for the Oceans is one of seven Special Bureaus
of the IERS Global Geophysical Fluids Center (GGFC) which was established on
January 1, 1998 in order to help relate dynamical properties of the atmosphere,
oceans, mantle, and core to motions of the Earth, including its rotation. In
particular, the IERS Special Bureau for the Oceans is responsible for
collecting, calculating, analyzing, archiving, and distributing data relating
to nontidal changes in oceanic processes affecting the Earth's rotation,
deformation, gravitational field, and geocenter. The oceanic products available
through the IERS SBO are produced primarily by general circulation models of
the oceans that are operated by participating modeling groups and include
oceanic angular momentum, center-of-mass, bottom pressure, and torques. Through
the IERS SBO web site at http://euler.jpl.nasa.gov/sbo, oceanic data can be
downloaded and a bibliography of publications pertaining to the effect of the oceans
on the solid Earth can be obtained. Currently, two different oceanic angular
momentum data sets are available. The IERS SBO is therefore one possible source
of data that can be used by the IAG/IAPSO Joint Working Group in their
investigations on the geodetic effects of nontidal oceanic processes.
Meetings of the IAG/IAPSO
Joint Working Group on Geodetic Effects of Nontidal Oceanic Processes are
planned to be held twice-per-year in conjunction with major conferences in
order to foster interactions on this topic between the geodetic and
oceanographic communities. These meetings, which are open to all interested
individuals, will generally be held in the Spring in conjunction with the EGS
conference in Europe and in the Fall in conjunction with the Fall AGU
conference in the United States. The next meeting will be held in conjunction
with the Fall 2000 AGU conference in San Francisco, California during December
15-19, 2000 with the exact date and time to be announced later. In order to
receive announcements about this and all future meetings, please contact
Richard Gross by sending an email message to him at Richard.Gross@jpl.nasa.gov. R. Gross
WORKING
MEETING OF THE IAG SSG 4.190 ON NON-PROBABILISTIC ASSESSMENT IN GEODETIC DATA
ANALYSIS
The first working meeting of the IAG SSG
4.190 took place at the Geodetic Institute, University of Karlsruhe (GIK), on
April 7, 2000. 11 members and corresponding members were participating. The
meeting was opened with a welcome note by B. Heck, president of the IAG Section
IV on General Theory and Methodology. H. Kutterer, chairman of the SSG,
continued with a short review of the terms of reference and objectives. The
main part of the meeting consisted of oral presentations by members of the SSG
on the topics fuzzy-theory (E. A. Shyllon, K. Heine), robust estimation (A.
Carosio), artificial neural networks (J. B. Miima), interval mathematics (S.
Schön), GIS for local geoid computation (M. Brovelli), and on general
uncertainty theory (H. Kutterer).
It
was decided to have annual closed working meetings of the SSG. Besides, it is
planned to organize an open international workshop on robust and fuzzy
techniques in March 2001 in Zürich.
The
financial support of the stay of E. A. Shyllon by the IAG is gratefully
acknowledged as well as the sponsoring of the organization of the meeting by
the GIK.
H. Kutterer
Minutes of the Organizational Meeting for African
Reference System "AFREF"
Held April 27, 2000, Centre Universitaire Mediterranean
(CUM), Nice, France
Meeting Objective:
Discuss possible organization of a project to establish
a common geodetic reference system throughout Africa compatible with the
International Terrestrial Reference System (ITRF). Discuss ways to involve the
international geodesy community to work with African nations to develop a
single, uniform, continental geodetic reference
system meeting international standards to replace the
myriad national reference systems, many of which have not been maintained, and
are out of date and inaccurate.
Meeting Organization:
Called by Claude Boucher, head of Commission X of the
International Association of Geodesy (IAG) "Global and Regional
Networks", also head of the ITRF and the representative of the
International Earth Rotation Service (IERS) to the International GPS Service
(IGS). The IGS is active globally in supporting the mission of the IAG &
IERS/ITRF through the techniques and applications of the Global Positioning
System (GPS). GPS is the most economical and widely accessible modern geodetic
technology for realizing a continental reference network throughout Africa.
Executive Summary
The decision was taken at this preliminary meeting to
pursue the coordination of a project designated "AFREF", the
objective of which is to establish a continental, robust and homogenous
geodetic reference system throughout Africa. Africa remains the only continent
with paucity of satellite geodetic measurements, especially GPS observations,
either episodic, or continuous. There are a few notable exceptions: locations
in South Africa, single stations in Malindi, Kenya; Mas Palomas, Canary
Islands, Spain; Libreville, Gabon and at previous times a station each in Ghana
and Cote 'd Ivorie.
Difficulties of in-country support, communications,
reliable infrastructure and lack of resources hinder permanent, high quality
GPS station implementations a Helwan, Egypt; Adis Ababa, Ethiopia; Rabat,
Morocco; and Kampala, Uganda, for example, where equipment have been installed.
This meeting and earlier ad-hoc discussions have
highlighted the importance of a renewed effort to realize a reference system
for this continent through international collaboration directly with the
African nations. It was emphasized that the must truly be a joint effort with
Africans to be successful and that it must focus on the
transfer of appropriate technology to sustain the
references with modern instrumentation, e.g. GPS and other satellite
techniques. It is also noted that resources will be required to enable
organizational participation and project activities (e.g. travel, equipment,
technical support, etc.)
The meeting attendees agreed to further explore and
pursue a joint project 'AFREF' with the Africans and other international
partners, and that such a project should:
Ruth Neilan, acknowledging contributions from Jim
Slater
Minutes of the SIRGAS (Sistema de Referencia Geocentrico para Las Americas) committee meeting, held on october 21 and 22, 2002 Santiago, Chile
The
president of the Committee highlighted the financial support given by the
International Association of Geodesy (IAG), decisive for holding the meeting.
The Pan-American Institute of Geography and History (PAIGH), which had approved
funds for the project in 2002, could not honor this commitment due to financial
difficulties that it is currently facing. Therefore IAG responded to our last
minute request, enabling the attendance of eight participants of seven
countries of South America, which was decisive for the success of the meeting.
All annexes can be found under http://www1.ibge.gov.br/home/geografia/geodesico/sirgas/principal.htm
or http://www.ibge.gov.br/sirgas
1.
Status on the integration of the South American
countries to SIRGAS (R. Barriga, President of the WG II) (Annex I)
2.
Presentation of the SIRGAS 2000 GPS campaign
results by the processing centers
2.1 IBGE (S. Costa) (Annex II)
2.2 DGFI (K. Kanniuth)
The coordinates obtained in the individual solutions of each processing
center (DGFI with Bernese, DGFI with GIPSY and IBGE with Bernese) shown a
consistency between each other of about 5 mm in the horizontal components and
7.5 mm in the vertical component.
Resolution: The SIRGAS Committee
decided that the final solution of the SIRGAS 2000 GPS campaign will be
generated by the combination of three solutions: DGFI´s, using the Bernese
software; DGFI´s, using the GIPSY software; and IBGE´s, using the Bernese
software.
3.
Combination of the processing centers´ results
(H. Drewes/K. Kanniuth/S. Costa)
3.1 Combination strategy and connection to ITRF2000
M. Kumar, from NIMA,
presented the following issue: the ITRF solutions are generated using the
tide-free system, which is not realistic and contradicts the IAG Resolution 16
of 1983 (Annex III)
Resolution: To keep using the
tide-free system in the SIRGAS 2000 results and to formally suggest to IAG to
manage with the International Earth Rotation Service (IERS) the solution of
this issue.
3.2 Determination of velocities
According to H.
Drewes, it is not enough to consider the results of the SIRGAS 1995 and 2000
campaigns for the determination of the SIRGAS stations velocities.
Resolution: The SIRGAS Committee
approves H. Drewes´ proposal of considering the observations of permanent GPS
stations and of geodynamic campaigns, in addition to the results of the SIRGAS
1995 and 2000 campaigns, for the determination of the velocity field of the
South American continent.
3.3 Final results (coordinates and velocities)
Resolution: The SIRGAS
Committee accepts in advance as official the final combined results of the
SIRGAS 2000 GPS campaign, to be generated by the processing centers in near
future.
Resolution: The SIRGAS
Committee defines the date of December 20, 2002, as the deadline for the
processing centers to release the final combined results of the SIRGAS 2000 GPS
campaign.
Resolution: The SIRGAS
Committee defines the date of March 28, 2003, as the deadline for DGFI to
release the results of the velocity field for the South American continent.
Resolution: The procedures
to generate the official results of the SIRGAS 2000 GPS campaign will be
described in a final report, similarly to that released during the IAG
Scientific Assembly, held in Rio de Janeiro, in 1997.
Resolution: The SIRGAS
Committee proposes to include in the SIRGAS 2000 GPS campaign final report a
special acknowledgment to the processing centers – DGFI and IBGE – by the
enormous efforts carried out and by the excellence of the results obtained.
4.
Use of the SIRGAS 2000 final results (H. Drewes, Representative of IAG)
Resolution: The SIRGAS
Committee proposes to include in the SIRGAS 2000 GPS campaign final report
detailed instructions about how to use the campaign final results.
It was recommended that, for countries that have not adopted yet SIRGAS
1995 as reference system, they should adopt the system based on the SIRGAS 2000
results, reference epoch 2000.4.
5.
Presentations of the Working Group III
“Vertical Datum” (L. Sanchez, President of WG III, and H. Drewes, Representative
of IAG)
5.1 Introduction (Annex IV)
5.2 Urgent need of a modern vertical reference system (Annex V)
5.3 Computation of geopotential numbers and physical heights (Annex VI)
5.4 Reference surface: considerations regarding W0 (Annex
VII)
5.5 Future activities (Annex VIII), recommending
to countries:
·
Geodetic leveling of the SIRGAS2000 stations
·
Connection of leveling networks between neighboring countries
·
Identification and typing of all leveling lines that connect SIRGAS2000
stations
·
Typing of the national leveling networks
·
Identification of the network nodes
·
UNIFIED determination of the quasi-geoid
·
Determination of the sea surface topography (SSTop) (GPS positioning of
tide gauges)
The WG III president
offered support to the member countries of the SIRGAS Committee regarding the
computation of geopotential numbers and help with parallel tasks. It is
emphasized that the height differences to be used in computations are the observed
ones, WITHOUT any error distribution or adjustment.
6. Continuation of the discussion on the new statute proposal (L. Fortes
and C. Brunini)
Resolution: The
SIRGAS Committee approves the new project Statute, corresponding to the version
originally proposed by the representation of Argentina, with the modifications
discussed during the meeting in Santiago del Chile.
With the approval
of the Statute (Annex IX), the substitute
representative of Argentina in the Committee, Claudio Brunini, proposed the
names of Luiz Paulo Souto Fortes, from IBGE/Brazil, and Eduardo Andrés Lauría,
from IGM/Argentina, respectively for president and vice-president of the
project for the next term (2003-2007). The current president of the SIRGAS
Committee will contact all countries embraced by the project in order to
confirm the names of the representatives in the Committee and, consequently, to
define the necessary quorum for electing the new project authorities. This
election will be carried out by electronic mail and the elected authorities
will be installed in office in July 2003, at the General Assembly of the International
Association of Geodesy.
7. Closing
(L. Fortes)
Resolution: The
SIRGAS Committee acknowledges the Instituto Geográfico Militar of Chile for the
excellent organization of the meeting and for the support to the Committee
members.
L. Fortes, IBGE Brazil
Ninth Business Meeting of
Ablos, held at the Hydrographic and Oceanographic Department
Japan Coast Guard, Tokyo,
October 23-25, 2002
Meeting report is available
at: http://www.gmat.unsw.edu.au/ablos/minutes02.pdf
X IAG International
Symposium on Recent Crustal Movements, Helsinki, Finland, August 27-31, 2001
The tenth IAG
(International Association of Geodesy) International Symposium on Recent
Crustal Movements (SRCM) was held in Helsinki, Finland, August 27.-31., 2001.
The main organizer of the Symposium was the Finnish Geodetic Institute.
Co-organizers were the Department of Geology, University of Helsinki,
Department of Geophysics, University of Helsinki, and Department of Surveying,
Helsinki University of Technology. Scientific programme was planned together
with Prof. Susanna Zerbini, University of Bologna, Italy, the president of the
IAG Section V, Commission XIV, Crustal Deformation.
More than 70 participants, and 60 presentations during the symposium
show the importance and wide variety of the topic. Natural and athropozenic
hazards was one of the topics, as a part of the crustal movements can be
violent and rapid, causing both human and materaial losses. Some movements,
although slow but still of a great importance, such as the postglacial rebound
or the eustatic rise of the sea level, can help us to study and understand
global changes, such as warming and its causes, and deglaciation. The
proceedings of the Symposium will be published in the Journal of Geodynamics
(JoG), an official journal of the European Geophysical Society.
Markku
Poutanen, Finnish Geodetic Institute, Secretary of the SRCM symposium
Report of the International Congress on Geodesy and
Cartography, Caracas, Venezuela
18-22 March, 2002 (IAG sponsored)
Co-Sponson: Instituto
Geográfico de Venezuela Simón Bolívar (DIGECAFA), Dirección de Hidrografía y
Navegación (DHN), Fundación Venezolana de Investigaciones Sismológicas
(FUNVISIS), Petróleo de Venezuela (PDVSA), Sociedad Venezolana de Ingenieros
Geofísicos (SOVG), Instituto Nacional de Canalizaciones (INC), Colegio de
Ingenieros de Venezuela (CIV), Asociación Venezolana de Ingenieros Geodestas
(ASOVIG),
Organized by:
Venezuelan Association Of Geodetic Engineers (ASOVIG)
General Program
Opening Ceremony, Session I and II –Reference
Systems, Geoid, Session III
and IV–Satellite Techniques, Session V and VI –Geographical
Information Systems, Session
VII–Cadastre, Session VIII –Interdisciplinary Applications, Session IX–Photogrammetry and
Cartography, Session X–Cartography and Remote Sensing, Session XI–Remote
Sensing, Session XII–Geodetic Measurements in Engineering
Statistics
There were 72 oral paper presentations from 123
Authors, 62 University students, and 152
registrated participants.
Oral presentations:
In the following, there were presented 72
individual and multinomial papers. The paper titles and their authors are (not
in chronological and schematic order):
Acuña (Venezuela), Bosch (Germany): Improving comparisons
of satellite altimeter observations and tide gage registrations for unifying
height systems in the Caribbean area. Alves,
Blitzkow, (Brazil): Modern concepts and techniques of control and forms to
monitor tide gage stations with GPS. Alves, Blitzkow,
et al. (Brazil): Sea level
determination 1831 and 2000 with GPS, leveling and tide gage observations. Arrieche, (Venez): Experiences of
hiperspectral remote sensing in the Venezuelan Oil Industry. Azcarate, Martinez, et al., (Venez): Design
and application of an interactive system of digital images. Blanco, Gajardo, et al., (Venez): Geotechnical,
geophysical and hydraulic studies to define the stability of Mamo Mesa
Venezuela. Blanco, Gajardo, et al.,
(Venez): Observation system of Viaduct No.1 of highway Caracas-La Guaira. Orlando, Barromé, (Venez): Geodetic and
instrumental control of the Hydroelectrical Complex of the Lower Caroni River. Buyana, Guevara, et al., (Venez):
Methology of Geoid ondulation determination with heterorgenic geodetic data. Clayton, Jacques, et al., (Brazil): Methodology
to locate the most favorable areas for installation of small hydropower systems
in a GIS environment. Cardozo,
Núñez, et al., (Brazil): Orthomosaic
generation from a digital, nonmetric camera. Carvalho., et al., (Brazil): Methology
for hydraulic works registration of Bahia State, Brazil. Carvalho, et al., (Brazil): Fluvial dynamics of Sao Francisco River
using Landsat 7/ETM + images. PimenteL et
al., (Brazil): Digital cartography for management of water distribution
networks. Pimentel, Ferreira, (Brazil): Teodoro Sampaio and the beginning of
systematic cartography in Brazil. Pimentel, Nero, (Brazil): Cartographic
documents: Determination of geometric quality in Brazil. Correa E Castro, Blitzkow, (Brazil): Recovery of South American
gravity nets by Chile and Paraguay. Daal, Balcázar, et al. (Venez), TREMEL (Germ): GPS
Campaign REGVEN 2000. Carvalho et al. (Brazil): Geobotanical analysis
of geological structures using hyper spectral images. Cogliano, Galban, et al., (Argentina): First comparison of height
networks between Chile and Argentina. Laura
Delgado et al. (Venez): Remote
Sensing – Digital terrain models and GIS: Tools for Malaria control. Do
Nacimiento et al. (Brazil): Morphologic
analysis of the Grande River basins as subsidy for ecological zoning using
GIS. Dolande, Montezuma, et al. (Venez): Cartographic cover of
Esequibo territory by Landsat TM and ETM.
Dominguez et al., (Venez): Calibration
of position equipments for offshore seismic surveys. Fontes, et al., (Brazil): Use
of GIS in management of National Park in Brasilia. Francoso, et al.,
(Brazil): GIS for historical rescue. Francoso, et.al., (Brazil): GIS en Sao
Paulo State. Freitas, et al., (Brazil): Cartographic
actualization with IKONOS, using IKONOS 2 satellite for cartographic actualization
in maps up to 1:2500. Fuenmayor, et al.,
(Venez): SIRGAS – REGVEN point densification for PDVSA. Gechele,
Nixon, et al., (Venez): GIS implantation by GPS in coastal areas of
Maracaibo lake. There were considered Hydro Pro, Pathfinder Office, Auto Cad
and Arcview. Gonzalez, Digecafa, (Venez): Evaluation of quick static positioning
for medium distances. Guerra, et al., (Venez): The homogeneous
treatment unit (UHT), an SIG tool for perforation dispositions.Guevara, et al., (Venez): Evaluation of
precision of image orthorectification of IKONOS Satellite in urban areas of
Caracas. Guillen, et al., (Venez): System
implantation and proof for vehicle control by GPS. Henneberg (Venez): Geodetic measurements of neotectonics and recent
crustal movements. Hernandez, (Venez): Evolution
and actual situation of Venezuelan geocentric reference system. Hoyer, Hernandez, et al., (Venez): Geoid determination in Venezuela by minimum
square collocation. Hoyer, et al., (Venez): GPS measurements
processing of REGVEN project. Hoyer, et
al., (Venez): RENDON: GPS measurements in the area of the Yacambú-Quibor
hydraulic system. Jauregui, et al., (Venez):
Elaboration of digital stereo-orthophotos. Liberal, (Venez): Three
dimensional geodetic model and GPS application. Lopez, et al., (Venez): Optimization
of GPS applications in the Venezuelan Oil Industry. Marquez, Mecinca, (Venez): DIN 18723 and application for
certification of theodolites and level instruments Martin, et al., (Venez): Impact of the new official DATUM of
Venezuela (SIRGAS – REGVEN ) in geodetic activities of PDVSA. Alves,
Pimentel, (Brazil): Digital terrain model. Nero, Pimentel, (Brazil):
Map digitalizations: Comparitive studies of methodologies. Ordóñez,
et al., (Colombia): Deformation measurements of GALERAS Volcano,
Colombia. Ordóñez, et al., (Colombia): GPS measurements for micro gravity
studies of Galeras volcano, Colombia. Mora, et al., (Colombia): Satellite geodesy
for tectonic deformation measurements in NE of South America. Oropeza, (Venez): Digital rural cadastre
of watering systems in Falcón State, Venezuela. Rincon, Et Al., Hoyer, et al., (Venez): Satellite altimeter studies
of the Atlantic Front of Venezuela Rios,
(Venez): GIS tendency in geography.
Rivas, et al., (Venez): GIS for sub
terrain installations in urban areas. Rivas,
et al., (Venez): Use and methology of multimedia to execute technical
evaluation of road communication systems. Rivas,
et al., (Venez): Measurements, analysis and composition of the atlas of
road systems. Rivas, et al., (Venez): Application
of ISO VALUE Lines for residential buildings using a GIS system. Stamato, (Brazil): Is an electronic
atlas a geographic information system? Swanston,
(Venez): An approximation to a new cadastral registration system. Swanston, (Venez): Quality control of
radar orthoimagery. Taylhardat, Hernandez, (Venez): GIS-Exploration
processes. Vallee, Parra, (Venez): Cartography
of hydrocarbon emanations. PRAOG,
TIESZEN, (USA): Development of exploration, access and dissemination of geospace
data (clearinghouse) in different Central American countries caused by
hurricane Mitch.Vera, et al. (Venez): Geomorphological
vision of North and South America. Wildermann, et al., (Venez): Comparison
of different height systems in Venezuela. Gavel (USA): Data evaluation
for space positioning for oil wells.
Special presentations:
Henneberg, (Venez): Marine Geodesy. Drewes, (Germ): Why do we need a new height system? Guevara,
(USA): The Geospace paradigm and its impact on a bearable progress. Rendon,
(Venez): The project for modernization of the national seismology network. Drewes, (Germ): The international
reference system ITRF and its continental amplification (SIRGAS). Vera,
(Venez): Technological promotion –
Air transportable remote system for “Alto Resources Venezuela, C.A.” Prelat,
(USA): Hyper spectral technology
for evaluation of national resources and environment.
Heinz Henneberg,
National IAG Representative
Report on IAG 2001 Scientific Assembly of the International Association
of Geodesy,
Budapest, Hungary, 2--7 September 2001
by J.
Adam and K.-P. Schwarz
It
was in September 1906 that the predecessor of the IAG, the 'Internationale
Erdmessung', organized its 15th General Assembly at the Hungarian
Academy of Sciences in Budapest. It was 95 years later, in September 2001 that
the IAG returned to this beautiful city to hold its Scientific Assembly, IAG
2001, in the historical premises of the Academy. The meeting took place from
September 2-7, 2001 and continued the tradition of Scientific Assemblies,
started in Tokyo (1982) and continued in Edinburgh (1989), Beijing (1993) and
Rio de Janeiro (1997). Held every four years at the midpoint between General
Assemblies of the IAG, they focus on giving an integrated view of geodesy to a
broad spectrum of researchers and practitioners in geodesy and geophysics. The
convenient location of the main building of the Hungarian Academy in downtown
Budapest and the superb efforts of the Local Organizing Committee contributed
in a major way to the excellent atmosphere of the meeting.
In the opening session of the IAG 2001
Scientific Assembly, participants were welcomed by Attila Mesko, Deputy
Secretary-General of the Hungarian Academy of Sciences, Fernando Sanso,
president of the International Association of Geodesy (IAG); Klaus-Peter
Schwarz, Chairman of the Program Committee and Jozsef Adam, Chairman of the
Local Organizing Committee (LOC). The welcome address of the IAG president
Fernando Sanso is attached to this report.
As at previous meetings, the scientific
part of the program was organized as a series of symposia, which, as a whole,
provided a broad overview of actual geodetic research activities. To emphasize
an integrated view of geodesy, the symposia did not follow the pattern of the
IAG Sections, but focussed on current research topics to which several IAG
Sections could contribute. Each symposium had 5 sessions with presented papers
and poster sessions on two consecutive days. Since the majority of papers were
presented as posters, an effort was made to give ample exposure to this form of
presentation. Besides having each poster up for two consecutive days in the
main hall of the building, it was also decided that no parallel sessions would
be scheduled during the poster sessions. This gave considerable exposure to the
poster presentations and led to good interactions between authors and
participants.
The
scientific program dealt with the following topics:
Symposium
A: Fine-tuning Reference Frame Implementation, Convenors: C.K. Shum (USA) and
A.H. Dodson (UK)
·
A1
Space Techniques: Coordination and Combination Methods, Chair: H. Drewes
(Germany), Co-chair: J. Hefty (Slovak Rep.)
·
A2
Non-tidal Earth Gravitation and Geocenter Motion, Chair: B.F. Chao (USA),
Co-chair: P. Biro (Hungary)
·
A3
Regional Reference Networks, Chair: R. Weber (Austria), Co-chair: L.W. Baran
(Poland)
·
A4
Vertical Datums: Determination Techniques and Unification, Chair: C. Jekeli
(USA), Co-chair: J. Ihde (Germany)
·
A5 Is
there a Need for a Geodetic Datum 2000?, Chair: C. Boucher (France), Co-chair:
E. Groten (Germany)
·
AP
Poster Session, (Responsible: A.H. Dodson)
Symposium
B: From Eotvos to Satellite Gradiometry - New Vistas in Measuring and Modeling
the Earth's Gravity Field, Convenors: M.G. Sideris (Canada) and B. Heck
(Germany)
·
B1
Advances in the Theory of Gravity Field and Geoid Determination, Chair: P.
Holota (Czech Rep.), Co-chair: A. Marchenko (Ukraine)
·
B2
Use of Gravity Data from Earth and Planetary Satellite Missions, Chair: H. Ilk
(Germany), Co-chair: M.Petrovskaya (Russia)
·
B3
Airborne Gravimetry, Chair: L. Bastos (Portugal), Co-chair: A. Kopaev (Russia)
·
B4
Advanced Technologies for High-resolution Global and Regional , Digital
Elevation Models (DEM), Chair: P.A.M. Berry (UK), Co-chair: I.N. Tziavos
(Greece)
·
B5
Advances in Numerical Techniques and Approximation Methods, Chair: R. Klees
(The Netherlands) Co-chair: J. Zavoti (Hungary)
·
BP
Poster Session (Responsible: B. Heck)
Symposium
C: Geometry and Beyond - Using Global Navigation Satellite
System
(GNSS) in New Ways, Convenors: C. Rizos (Australia) and J. Adam (Hungary)
·
C1
Probing the Atmosphere with GNSS, Chair: H. vander Marel (The Netherlands),
Co-chair: A. Kenyeres (Hungary)
·
C2
Low Earth Orbiter Satellite Missions, Chair: P. Schwintzer (Germany), Co-chair:
J.B.Zielinski (Poland)
·
C3
New Concepts in Engineering Geodesy, Chair: H. Kahmen (Austria), Co-chair: Á.
Detrekoi (Hungary)
·
C4
Probabilistic and Non-probabilistic Assessment in Data Analysis, Chair: H.
Kutterer (Germany), Co-chair: A. Dermanis (Greece)
·
C5
Biases in GNSS Positioning, Chair: M. Stewart (Australia), Co-chair: S.
Tatevian (Russia)
·
CP
Poster Session (Responsible: J. Adam)
Symposium
D: Modeling Earth Processes and Global Change
Convenors:
C. Wilson (USA) and V. Dehant (Belgium)
·
D1
Ocean-Solid Earth Interactions, Chair: R. Gross (USA), Co-chair: P.Varga
(Hungary)
·
D2
Variations in Earth Orientations, Chair: J. Vondrak (Czech Rep.), Co-chair: A.
Brzezinski (Poland)
·
D3
Global and Regional Sea-level Changes, Chairs: A. Cazenave (France) and D.P.
Chambers (USA), Co-chair: M.Poutanen (Finland)
·
D4
Global and Regional Plate Motions and Deformations, Chairs: S. Zerbini (Italy)
and C. Wilson (USA), Co-chair: I. Joo (Hungary)
·
D5
Satellite Altimetry for Oceanography and Geodesy, Chair: C.Hwang (Taiwan), Co-chair:
M.Vermeer (Finland)
·
DP
Poster Session (Responsible: V. Dehant)
Special
Sessions
·
E1
Scientific Cooperation in Geodesy and Geophysics in Central and Eastern
European Countries (CEEC), Chair: J. Sledzinski (Poland), Co-chair: F.
Vodopivec (Slovenia)
·
E2
Research Challenges for Young Scientiests, Chair: K.P. Schwarz (Canada)
·
E3
Information Session on the New Structure of the IAG, Chair: G. Beutler
(Switzerland)
The
scientific program of the meeting was organized by the symposium conveners and
the chairpersons of the session. The symposium conveners decided on the
acceptance of the submitted abstracts and, in cooperation with the session
chairs, on the final program. The session chairs took an active role in
soliciting papers for their sessions and were responsible for the selection of
papers for oral presentation and the review process. In addition, they
organized the review process for the topic of their respective session. This
was a major job, considering that a total of 126 oral and 254 poster presentations
were made. Special thanks are therefore expressed to all symposium conveners
and session chairpersons for organizing the symposia and sessions.
For the first time in the history of the
General and Scientific Assemblies, two best student paper awards were announced
by the IAG, one to the author of a paper presented orally, and the other to the
author of a poster paper. The award for the orally presented paper went to
Michael Kern of the University of Calgary, Canada, and the award for the poster
paper to Suzanne N. Lyons of the Scripps Institution of Oceonography, USA.
Congratulations to both of them.
The IAG Executive Committee decided to
select about 100 representative papers, for publication in the reviewed
IAG/Springer proceedings series. The selected papers were reviewed by the same
review process used for the Journal of Geodesy. Special thanks are expressed to
all session chairpersons for getting the reviews in under a very tight time
schedule. The co-operation of both authors and reviewers in trying to meet the
deadlines was highly appreciated. It made the timely publication of these
proceedings possible. The volume contains a representative sample of 93
reviewed papers from all sessions, as well as nine papers presented in the
special sessions. This volume (number 125) will be available by the end of
March. Note that a CD containing all papers that were submitted for publication
in time (deadline: November 30, 2001) was issued and mailed already to all
conference participants early in February, 2002.
During the IAG 2001 Scientific Assembly,
in addition to IAG Bureau and Executive Committee meetings, 21 Special Study
Groups, Special Commission, Commission and Ad hoc group specially organized
meetings for discussions and exchanges. Furthermore, meetings of the Joint
Board of Sister Societes and the Editorial Board of the Journal of Geodesy took
place in Budapest.
Full- and half-day excursions were offered
for the participants and accompanying persons to explore Budapest and the
countryside (Danube Bend and Godollo Palace). A Welcoming Reception at the
Picture Gallery Hall of the Academy and an IAG Banquet at the Citadella
Restaurant on the top of Gellert Hill were organized for participants and
accompanying persons.
In the closing session of the IAG 2001
Scientific Assembly, the IUGG President Masaru Kono addressed the participants.
Following that, brief summaries of the symposia were given by conveners (C.K.
Shum, B. Heck, C. Rizos and C.R. Wilson). Finally, closing remarks were
presented by J. Adam, Chairman of the LOC and Prof. F. Sanso, President of the
IAG.
The meeting attracted a larger number
of participants (449 registered participants from 54 countries) and papers
(380) than previous Scientific Assemblies. This is in part due to the generous
financial and promotional support given by a number of agencies. It made the
support of students and colleagues from developing countries possible and gave
the social events an additional touch of hospitality. Special thanks go to the
International Association of Geodesy (IAG), the Hungarian Academy of Sciences
(HAS), the European Space Agency (ESA), the US National Aeronautics and Space
Administration (NASA), the Jet Propulsion Laboratory (JPL), the Budapest
University of Technology and Economics (BUTE), the Eotvos Lorant and
Geophysical Institute (ELGI), the Hungarian Scientific Research Fund (OTKA),
and the Ministry of Education. IAG, HAS, ESA and NASA are thanked for their
financial contributions.
As decided at the last General Assembly of
the IAG in Birmingham in1999, a special IAG Council Meeting took place after
the conference in order to make a decision on the proposed restructuring of the
IAG. The proposal, presented by the chairman of the Restructuring Committee,
Gerhard Beutler, and supported by the IAG Executive, was accepted with small
modifications.
The responsibility for organizing this
conference was shared by the Program Committee (chairman: Klaus-Peter Schwarz,
members: Alan H. Dodson, Che-Kwan Shum, Michael G. Sideris, Bernhard Heck,
Clark R. Wilson as IAG Section Presidents) and the Local Organizing Committee
(chairman: Jozsef Adam, members: Ivan I. Mueller as IAG Representative, Laszlo
Banyai, Gusztav Hencsey, Ambrus Kenyeres, Gabor Papp, Viktor Richter, Gyula
Toth). The credit for the professional running of the conference goes to the
staff of the conference bureau of the Computer and Automation Research
Institute of the Academy. Special thanks are expressed to the Head of this
Department, Gusztav Hencsey, and to staff member Viktor Richter for their
efficient and friendly organization.
Those interested in more details of the
program may consult the web site http://www.sztaki.hu/conferences/iag2001. The
reviewed proceedings will be published by Springer Verlag and will be available
at the end of March 2002.
Geodesy on the Move
Presidential address to the IAG Scientific
Assembly in Budapest
F. Sanso
DIIAR, Sez. Rilevamento, Politecnico di Milano, Piazza
Leonardo da Vinci 32, I-20133 Milano, Italy.
Ladies
and Gentlemen, dear Friends and Colleagues,
it
seems yesterday that we were leaving the IUGG General Assembly in Birmingham
outlining the work program for the next four years and announcing that we would
meet here in Budapest to verify whether we were marching in the right
direction.
Six lines
have been put down as the main streets along which to develop the IAG action:
·
the
first, institutional and most obvious is to develop Geodesy as science in
itself,
the
others are
·
to
improve the relations with other sciences and their organization,
·
to
improve the IAG impact in terms of Services towards other sciences and the
society in general,
·
to
improve IAG penetration into the developing countries,
·
to
improve the internal IAG organization,
·
to
widen the scientific manpower on which IAG is based.
I will
try to review these in short with one warning: this talk has been prepared a
few days ago in the Alps while I was in the so-called ``vacations'' and I had
with me only little material, so it is based mainly on my memory which is
scarce and even fading.
I hope I still have clear the overall
design, but I am pretty sure that I am forgetting important names and facts, so
please accept my apologies for that and take this presentation more as a
collection of examples rather than being exhaustive.
Point
1:to develop
geodesy as a science in itself.
I
will dwell little on that because this item is maybe more appropriate for the
last session of this Assembly, when we will have a more precise overview on
what is going on in geodesy and surroundings, yet I cannot refrain from saying
at least two small things.
Trivializing,
we could say that our job is:
·
to
survey the earth (and the planets) with new advanced techniques in a consistent
worldwide way,
·
to
develop new methods to describe our measurement models and to analyze the
available data both theoretically and numerically, which means qualitatively
and quantitatively.
For
the first point I would say that what we already have and we already planned to
have in a few years, is what we were dreaming of only few years ago.
Just think of the continuous monitoring of
GPS permanent stations by IGS, the global survey by SAR of all the continental
topography (I am talking of the SRTM mission) as well as the moinitoring of the
oceanic surface by the many altimetric missions and, not to be forgotten, the
complete imaging of the earth's global gravity field with CHAMP and
subsequently GOCE, including its time variations by the GRACE mission. This is
really an age of globalization of Geodesy against which none can protest!
As for the second point the production of
new ideas in Geodesy is at the same time too narrow (I will talk about that in
the meeting with the young geodesists) and too large to be mentioned in detail.
I just want to quote the names of Chris Kotsakis and Rudiger Lehman because
they share this year the prize for the bast paper award. I believe it is
consulating to see that computers have not killed our thinking in Geodesy
letting our beautiful tradition of the Hotine, Marussi, Baarda, Moritz and
Krarup continue.
Point
2: to improve
the relation with other sciences and their organization.
Are
we moving in this direction?
·
Planetology
I would say we are in strict and even improving relation.Last spring I was
sitting in a room in Matera, listening to Dave Smith that took the audience on
a fly across mountains and channels of Mars, I mean the true topography
computed by NASA, not science fiction! We know that a new ``train'' is leaving
for Mars under an ESA project, where our last Bomford prize awarde, Veronique
Dehant, is playing a very important role. If I can mention it, there is another
mission, Mercury orbiter, approved by ESA, where Italian geodesists have the
same role too. But let us come to the other geophysical sciences.
·
Solid
Earth Physics we share the whole subject of geodynamics to which we contribute
all the information coming from the ballet of the earth barycenter, the polar
motion and the spinning rate as well as the time variations of the first
harmonics of the gravity field. This is our contribution to global dynamics,
which we primarily provide through the International Earth Rotation Service. To
this we have to add the information on plate tectonics, which is basically
coming from the IGS international network of GPS permanent stations, jointly with
the other space techniques. Not to be forgotten all the other information on
crustal deformation and gravity field variations which complete the picture at
a local level. On the earthquakes we have important things to say with the new
ideas of combining GPS, and SAR information; think of the Colfiorito earthquake
in Italy and that of Izmit inTurkey,
·
Oceanography
we share again a large number of subjects of common interest; our definition of
height datum, the geoid, was historically based on the abstract concept of mean
sea level and, unfortunately, we are still discussing about this definition. I
do not think I need to underline the importance of altimetric satellite
missions for both sciences; I just want to mention that still after many years
IAG and IAPSO seem to me like two dogs one running after the tail of the other.
We believe that from altimetry we can subtract the dynamic height of oceans to
get the geoid there to construct global models, the oceanographers believe that
we can provide them a high resolution geoid by our global models so that they
can constrain the geostrophic part of the motion. It is a little more
complicated than that, but only the forthcoming gravity missions will be able
to cut this Gordian knot. Certainly the relations between the two associations
are excellent: we have joint symposia and a proposal to run a joint Scientific
Assembly could come for the next time, even geophysical associates that were
thought to be traditionally far from IAG, like the hydrologists or the atmospheric
physicists have discovered that Geodesy is useful to them.
Just
six weeks ago at the IUGG Executive Meeting H.C. Davies, the president of
IAMAS, has claimed that, contrary to all his expectations, he had to admit that
important information could come from GPS or SAR sounding of the atmosphere,
and he prized us for that.
So this is the traditional line of ``good
relations'' with geophysical associations, with which we share the union
organization as well as with the other geophysical societies and we have the
impression that we are serving well this traditional field of action.
But there is the other side of our life
which is the relation of Geodesy to Surveying, Photogrammetry, Remote Sensing,
Cartography and so forth, all the more applied and engineering disciplines that
were borne as particular techniques, with associations taking care of the
relations with the world of professions. They drifted away, maybe too much,
particularly across the Eighties and early Nineties, and this has been a
mistake which our executive has tried to counteract by increasing the contacts
and the joint activities with FIG, ISPRS and so on. We had joint symposia,
schools, and study groups and not only because we think that we have something
to teach, but also because we have something to learn. I am thinking for
instance of a nice Symposium on Non-standard Non-probabilistic Methods
organized in Zurich by Kutterer (SSG 4.190) together with Alessandrio Carosio
who's specialty is GIS theory.
We should never forget that it is in IAG
genome to be an interface between geosciences and engineering applications, and
whenever we forget it we loose as a science and as an organization.
Point
3: to improve
the IAG impact in terms of Services towards other sciences and the general
society.
I
already mentioned the fantastic work performed by the International Earth
Rotation Service and the International GPS Service; they are based on a very
large international cooperation and give to IAG quite a substantial
contribution in the effort of maintaining its outstanding position among
geosciences.
It is incredible that, in spite of the
continuous threat of the supporting organizations to cut their budget, they
have always been able to evolve facing new challenges and providing new
products of larger and larger utility.
We would like to be more powerful and
authoritative to say to the supporters that they have to continue their effort
because it is a honour to be able to serve such a large community in such a
good manner! Nor one should forget the relatively new Services like the Laser
Ranging Service and the VLBI Service, who play specific essential roles within
the same general subjects. Nor I want to forget the Services related to the
gravity field like the glorious Bureau Gravimetrique which, together with the
International Geoid Service and the International Center for Earth Tides, will
join into a new International Gravity Field Service, already here in Budapest;
this also with the support of new centers provided by NIMA and GFZ.
To close this point let me at least
mention two Services with a clear strong interdisciplinary character: the
Permanent Service for the Mean Sea Level and the Bureau International des Poids
et Mesures (Time section).
I
will explain in a few minutes the enhanced role that Services will play in IAG
structure.
Point
4: to improve
the diffusion of IAG organization into Developing Countries.
This
is not a ritual statement that we repeat every time to keep our soul free of
any sense of guilt.
This
is a real line for our organization and we proved it by stimulating important
projects of international cooperation.
Let us think for instance of SIRGAS and
then to the many scientific activities in South America, including the choice
of bringing our Scientific Assembly in Rio. We have now a very active South
American community which is showing everywhere at the international level.
Similar success we had in the South-East Asia Pacific area, where not only our
Services and, for instance, International Schools have done very well but also
the development of IAG has been boosted by leading nations of the area like
Japan, China, Australia.
Nevertheless
we always had problems with the African continent.
Despite the historical enterprise of ADOS,
despite the many bilateral contacts, we never had a real IAG organization
there. At least till recently. However, thanks to the efforts of our Commission
X (on Global and Regional Geodetic Networks) and XIV (on Crustal Deformation),
as well as of the action of IGS for the full internationalisation of the Earth
Reference Frame and our Committee on Developing Countries, we finally see a
centripetal motion in Africa around geodetic themes.
In particular, from seven to eight nations
in South Africa and six nations in North Africa are setting up joint international
geodetic structures under the auspices of IAG and of the Organization Africain
de Cartographie et Teledetection.
It was the end of May when I was sitting
in Algiers in a room with 150 African colleagues for the Duexieme atelier nord
africain de geodesie. We only need to improve our efforts there because we are
getting a very positive response; only we still have to think a little bit of
the linguistic barrier, but I believe this will be quickly overcome with
younger generations.
To achieve that, these nations need
support and for sure IAG has not the possibility of financing projects.
However, I am proud to say that most of our budget goes to support travels to
allow people from developing countries to participate in international
meetings. This is a policy with general consensus but we have to acknowledge
the particularly firm action of our Secretary General in this direction.
Point
5: to improve
the internal IAG organization.
It is
not a mania of esthetic order, but the response of a living organism to its
needs of growth.
To
accomplish what we have illustrated we need:
·
a
swifter structure in IAG where people from our or other disciplines,
particularly young people, could easily find their place if they are
interested.
This
implies reducing the number of layers and bureaucracy in IAG;
·
a
structure where Services would be more free to act, to set up projects,
schools, to penetrate into new nations on behalf of IAG by contacting the
national agencies and, more generally, the users of geodetic products, by
affiliating them directly and giving them an international stage where to
report their new findings;
·
a
structure where developing countries could better find scientific support to
finally stand on their own legs and contributing back to the IAG evolution.
Along
these lines new statutes and bylaws have been elaborated by a commission under
the leadership of our Vice President, Gerhard Beutler. They have been discussed
by the Executive and then publicized through the IAG home page. I am glad to
say that we received reactions, comments and suggestions very sensible and
appropriate.
So a
final version will be submitted to the IAG Council, which is holding an
extraordinary meeting here in Budapest and, in case of approval, they will be
already applied in Sapporo at the next IUGG General Assembly.
Also,
in this way we feel we have accomplished a mandate by our Assembly in
Birmingham, to widen the scientific manpower on which IAG is based. While
closing the XXII General Assembly I said to the audience “Come all several and
plenty, come to IAG in Budapest and bring your best piece of geodetic work”.
Dear
friends, this is the Fifth scientific Assembly, after Tokyo, Edinburgh, Beijing
and Rio.
In
Tokyo we had 360 people and 177 papers, in Edinburgh 360 and 250 papers, in
Beijing 350 people and 295 papers, in Rio 350 people and 279 papers; in
Budapest we have up to 3 days ago 472 registrations and 427 papers, and I
believe that counting the last minute registration we will end up well over
500!
I do not want to be triumphal but I think I am allowed to
congratulate with you, because you are moving exactly in the direction you have
chosen in Birmingham and though the way is still long I want to say welcome
Geodesy to open your march.
--------------------------------------------------------------------------------------------------------------
IAG/IAPSO Joint Working Group on
Geodetic Effects of Nontidal Oceanic Processes
The oceans have a major impact on global geophysical
processes of the Earth. Nontidal changes in oceanic currents and ocean-bottom
pressure have been shown to be a major source of polar motion excitation and
also measurably change the length of the day. The changing mass distribution of
the oceans causes the Earth's gravitational field to cange and causes the
center-of-mass of the oceans to change which in turn causes the center-of-mass
of the solid Earth to change. The changing mass distribution of the oceans also
changes the load on the oceanic crust, thereby affecting both the vertical and
horizontal position of observing stations located near the oceans.
Recognizing the important role that
nontidal oceanic processes play in Earth rotation dynamics, an IAG/IAPSO Joint
Working Group on Geodetic Effects of Nontidal Oceanic Processes was formed at
the XXII General Assembly of the IUGG in Birmingham. The objective of this
IAG/IAPSO Joint Working Group is to investigate the effects of nontidal oceanic
processes on the Earth’s rotation, deformation, gravitational field, and
geocenter, and to foster interactions between the geodetic and oceanographic
communities in order to promote greater understanding of these effects. A
meeting of this IAG/IAPSO Joint Working Group, its fifth, was held on April 7,
2003 in Nice, France in conjunction with the 2003 Joint Assembly of the
European Geophysical Society (EGS), the American Geophysical Union (AGU), and
the European Union of Geosciences (EUG) during which presentations were given
by R. Gross, and O. de Viron.
R. Gross described the
International Earth Rotation Service (IERS) Special Bureau for the Oceans
(SBO). The IERS Special Bureau for the Oceans is one of eight Special Bureaus
of the IERS Global Geophysical Fluids Center (GGFC) which was established on
January 1, 1998 in order to help relate dynamical properties of the atmosphere,
oceans, mantle, and core to motions of the Earth, including its rotation. In
particular, the IERS Special Bureau for the Oceans is responsible for
collecting, calculating, analyzing, archiving, and distributing data relating to
nontidal changes in oceanic processes affecting the Earth’s rotation,
deformation, gravitational field, and geocenter. The oceanic products available
through the IERS SBO are produced primarily by general circulation models of
the oceans that are operated by participating modeling groups and include
oceanic angular momentum, center-of-mass, bottom pressure, and torques. Through
the IERS SBO web site at <http://euler.jpl.nasa.gov/sbo>, oceanic data
can be downloaded, software to compute the oceanic angular momentum,
center-of-mass, and bottom-pressure from the modeled temperature, salinity, and
horizontal velocity fields can be obtained, and a bibliography of publications
pertaining to the effect of the oceans on the solid Earth can be retrieved.
Currently, three different oceanic angular momentum data sets and two different
oceanic center-of-mass data sets are available. Links are also provided to
related web sites from which observed and modeled ocean-bottom pressure data
sets are available. The IERS SBO is one possible source of data that can be
used by the IAG/IAPSO Joint Working Group in their investigations of the
geodetic effects of nontidal oceanic processes. O. de Viron described the
nontidal effect of the oceans on geodetic parameters using the CLIO model. The
Coupled Large-scale Ice Ocean (CLIO) model is a baroclinic Boussinesq model
developed at the Universite Catholique de Louvain in Belgium to study ocean
dynamics and, in particular, the interaction between sea-ice and the oceans. It
has been adapted in order to account for the oceans' response to atmospheric
pressure forcing. The results presented at the meeting come from an 11-year
simulation spanning 1992 to 2002. The model is forced using NCEP reanalysis
data: 6 hourly pressure and friction drag, daily surface air temperatures and
wind speeds, and monthly climatologies of relative humidity, cloud fraction,
precipitation rate, and river
runoff. It was shown that the model is adequate to
study the oceans' effect on geodetic quantities: the derived oceanic angular
momentum (OAM) is similar at low frequency to other OAM series and the
omparison between the model-derived ocean-bottom pressure is similar to the few
measurements that are available. On the other hand, the model seems to be
overreacting by a factor of two at periods less than 5 days. This is still
under investigation.
R. Gross discussed the oceanic contribution to Earth
rotation changes using the ECCO model. As part of JPL's participation in the
Estimating the Circulation and Climate of the Ocean (ECCO) consortium, ocean
models are being used to simulate the general circulation of the oceans.
Oceanic angular momentum computed from these models have been compared to
observed changes in the Earth's rotation during 1980-2000. Although nontidal changes in the Earth's
length-of-day on time scales of a few days to a few years are primarily caused
by changes in the angular momentum of the zonal winds, other processes such as
oceanic current and bottom pressure changes can be expected to cause the
length-of-day to change as well. On intraseasonal time scales, atmospheric
surface pressure, oceanic currents, and ocean-bottom pressure are found to be
about equally effective in causing the length-of-day to change, while upper
atmospheric winds are found to be less effective than these mechanisms. On
seasonal time scales, the upper atmospheric winds are more important than the
sum of currents and bottom pressure in causing the length-of-day to change,
and, except at the annual frequency, are even more effective than surface
pressure changes. On interannual time scales, oceanic currents and bottom
pressure are found to be only marginally effective in causing the length-of-day
to change. For polar motion, a remarkable 70% of the observed polar motion excitation
variance during 1993-1999 is explained by the sum of atmospheric and oceanic
angular momentum, with the coherence between the observed and modeled
excitation being dramatically improved across a broad frequency band when the
angular momentum of the oceans is added to that of the atmosphere.
Meetings of the IAG/IAPSO Joint
Working Group on Geodetic Effects of Nontidal Oceanic Processes have been held
during the past four years in conjunction with major conferences in order to
foster interactions on this topic between the geodetic and oceanographic
communities. A report of the activities of the Joint Working Group will be
presented at the XXIII General Assembly of the IUGG to be held in Sapporo,
Japan during June 30 to July 11, 2003. In order to receive a copy of this
report, please contact Richard Gross at <Richard.Gross@jpl.nasa.gov>.
R. Gross
Report of the International Workshop
on Satellite Altimetry for Geodesy, Geophysics and Oceanography: Summer Lecture
Series and Scientific Applications, Wuhan,
China September 8 to 13, 2002.
The www address is http://space.cv.nctu.edu.tw/altimetryworkshop/altimetry.htm.
The workshop was hosted by the Wuhan
University with Dr JC Li as the chair of the LOC. The scientific program was
organized by the Scientific committee chaired by C Hwang. The workshop’s aim is to offer free lectures
on various aspects of altimetric research for beginners and for advanced
researchers, and to provide a forum for presentations and discussions of latest
results in satellite altimetry.
A total of 60 abstracts were
received and 65 people participated in this workshop. These participants are
from Austria (2), Australia (1), Canada (1), China (26), Czech Republic (1),
Denmark (2), France (1), Germany (2), Italy (2), Japan (1), Korean (2),
Netherlands (2), Taiwan (13), UK (1), and USA (7).
On Sep 9 and 10, 2003, five
three-hours lectures were delivered by CK Shum (principles of altimetry), K.
Matsumoto (ocean tides), O.B. Andersen (marine gravity and geoid), P. Berry
(waveform retracking) and DT Sandwell (bathymetry estimation). Three keynote
speeches were delivered by W Bosch (geodetic applications), A Cazenave (sea
level change) and LL Fu (ocean dynamics from altimetry).
The scientific sessions began on Sep
11 and contains Sessions G1 (chaired by C Zhao), G2 (W Bosch), G3 (EL Mathers)
, GO1 (H Schuh), GO2 (J Klokocnik), GO3 (C Hwang), O1 (C Zuffada) and O2 (HZ Xu) with 37 papers presented.
Chair of Org committee: C. Hwang, Taiwan.