http://www.geod.uni-bonn.de/SC7.html
K.H. Ilk (chair), P. Visser
(co-chair), J. Kusche (scientific secretary)
Abstract
This final report describes the
activities of the Special Commission VII “Satellite Gravity Field Missions”
during the past four years since the IAG General Assembly 1999 in Birmingham,
UK. There was a tremendous progress in preparing and realizing satellite-borne
gravity field missions in the past four years. In July 2000 the CHAMP mission
had been launched and after a commissioning phase and an International
Announcement of Opportunity the data of various product levels are accessible.
The results achieved during the past years proofed the expectations of the
scientific community. The first CHAMP progress meeting held in Potsdam in
January 2002 documented the progress in gravity and magnetic field and in
atmosphere research as well as in the techniques of orbit determination. In March
2002 the two GRACE satellites had been brought in nearly circular orbits. First
results confirmed the expectations of the scientific community expected from
satellite-borne gravity measurements and its value for unprecedented views of
the earth's gravity field. The preparation of ESA’s satellite gradiometry
mission GOCE is under way. Together with complementary geophysical data and
precise measurements of the surface of the oceans and ice regions, satellite
gravity data represent a "new frontier" in studies of the System
Earth. Scientific programs to take full advantage of these new information are
in preparation. It can be expected that the work of Special Commission VII with
a slightly modified task can be more successful in the coming years than in the
past. Indeed, the data available in the next future will attract many groups
with different analysis concepts and with various ideas to investigate
scientific and commercial applications of a very precise high resolution
gravity field. This is the reason that SCVII has the chance to support the
international exchange of ideas and to draw the greatest possible benefit out
of these new innovative data.
Introduction and background
SC VII is a continuation of a
Special Commission that existed already during the four years period before
1999 and had been established occasional the IAG General Assembly in Boulder,
USA, in the year 1995. The task at that time was to create a platform that
integrates all international activities related to gravity field determination
by satellite gravity gradiometry and to prepare the conditions for a future
mission. Around the year 1995 the common opinion was that only a dedicated
satellite gravity gradiometry mission could provide a gravity field which meets
the demands of the community. In the upcoming years since 1995 the situation
changed in so far as the cheaper satellite-to-satellite tracking concept gained
again more interest. This situation is also reflected in the change of the
subject of SCVII. Before 1999 it was dedicated to the “Gravity Field
Determination by Satellite Gravity Gradiometry” and in the follow-on period to
the more general topics of “Satellite Gravity Field Missions”. The last eight
years since 1995 showed a tremendous progress in preparing satellite-borne
gravity missions: today we not only have an accepted satellite gravity
gradiometry mission, GOCE, additionally, two satellite-to-satellite gravity
missions, CHAMP and GRACE are already realized and the scientific data partly
accessible to the interested community. The multi-purpose high-low
satellite-to-satellite mission, CHAMP, has been launched in July 2000, the
low-low satellite-to-satellite mission GRACE followed in March 2002 and the
satellite gravity gradiometry mission GOCE, at present in the scientific and
industrial preparation phase, will be realized in 2006. CHAMP, GRACE and GOCE
have the potential to revolutionize the knowledge of the system earth. Not only
the static part of the gravity field can be determined with unattained accuracy
also an eventual time dependency can be derived. The coming years, sometimes
defined as the “Decade of Geopotential Research” will represent an enormous
challenge for the geo-scientific community. During the present decade
additional satellite altimetry missions are already launched or will be
realized. The satellite altimetry missions Jason-1 and ENVISAT are already in
orbit since 2001 and 2002 respectively, and the cryosphere satellites ICEsat
(in orbit since 2003) and CryoSat (envisaged for 2004) will supply the gravity
field with important data of the geometry of the oceans and the ice regions.
The combination of these data will open new vistas for the geo sciences.
Objectives
The Special Commission VII was
envisaged to act as a platform of discussion and information exchange related
to the various missions mentioned above. Three main problem areas had been
defined; each of them consisted of several sub topics. It is indicated whether
specific problems are treated within a Special Study Group.
(i)
on the flight validation and calibration of satellite data of various
mission types – connections to SSG 2.193 “Cal/val of new gravity mission
instruments” (P. Visser, C. Jekeli) and the Working Group “Preparation of
Standard Procedures for Global Gravity Field Validation” (Th. Gruber),
(ii)
integrated sensor analysis - connections to SSG 2.162: Precise orbits
using multiple space techniques,
(iii)
new sensors (laser interferometers, alternative gradiometers and
accelerometers),
(i)
comparison of analysis techniques (global and regional),
(ii)
gravity field modeling aspects with view to the time dependency of the
gravity field – connections to SSG 4.187: Wavelets in geodesy and geodynamics
(W. Keller),
(iii)
combination of satellite data and (inhomogeneous) terrestrial data –
connections to SSG 3.185: Merging data from dedicated satellite missions with
other gravimetric data (N. Sneeuw),
(iv)
calibration of satellite derived data – connections to SSG 2.193
“Cal/val of new gravity mision instruments” (P. Visser, C. Jekeli) and the
Working Group “Preparation of Standard Procedures for Global Gravity Field
Validation” (Th. Gruber),
(v)
downward continuation aspects,
(i)
oceanographic aspects - connections to SSG 2.194: GPS water level
measurements (C. Jekeli),
(ii)
inversion of the gravity field,
(iii)
structure of atmosphere and ionosphere - connections to SSG 2.192: Spaceborne
atmospheric GNS soundings (R. Hanssen),
(iv)
temporal variations of the gravity field and the cryosphere,
(v)
temporal variations of the gravity field and the hydrosphere.
Besides these topics the Special
Commission was created also to act as a brain pool for ideas of future
developments in gravity field research. This encompasses not only applications
to various fields of geo sciences but also developments of future satellite
borne techniques to measure the gravity field.
Members
SC VII has 55 members and
corresponding members, respectively, including the chair, co-chair and
scientific secretary. The names of the members and corresponding members that
expressed their interest in the work of SCVII are given in the following list.
Chair/co-chair/scientific secretary:
Karl Heinz Ilk, Pieter Visser, Jürgen Kusche
Members/corresponding members:
Dimitri Arabelos (Greece), Georges Balmino (France), Srinivas Bettadpur (USA),
Johannes Bouman (The Netherlands), Ben F. Chao (USA), Jean Dickey (USA), René
Forsberg (Denmark), Willi Freeden (Germany), Yoichi Fukuda (Japan), Martin van
Gelderen (The Netherlands), Erik Grafarend (Germany), Richard S. Gross (UK),
Thomas Gruber (Germany), Roger Haagmans (Norway), Bernhard Heck (Germany),
Cheinway Hwang (Taiwan), Chris Jekeli (USA), Steve Kenyon (UK), Wolfgang Keller
(Germany), Roland Klees (The Netherlands), Rolf König (Germany), Radboud Koop
(The Netherlands), Ulrich Meyer (Germany), Federica Migliaccio (Italy), Jerry
X. Mitrovica (USA), Philip Moore (UK), Jürgen Müller (Germany), Steve Nerem
(USA), Helmut Oberndorfer (Germany), Erricos Pavlis (USA), Margarita
Petrovskaya (Russia), Dan Roman (USA), Reiner Rummel (Germany), Fernando Sansò
(Italy), E.J.O. Schrama (The Netherlands), Wolf-Dieter Schuh (Germany), Avri
Selig (The Netherlands), Abdel Sellal (Algeria), Peter Schwintzer (Germany),
C.K. Shum (USA), Martijn Smit (The Netherlands), Dru Smith (USA), Nico Sneeuw
(Germany), Hans Sünkel (Austria), Byron Tapley (USA), Pierre Touboul (France),
Christian C. Tscherning (Denmark), Illias Tziavos (Greece), John Wahr (USA),
Michael Watkins (USA), Martin Vermeer (Finland), Peiliang Xu (Japan).
Specific accomplishments
A first step of the activities of
SCVII was to establish a web site integrated into the IAG home page. National and
international activities related to the gravity field missions hade been
distributed to the interested community. Links to the most important addresses
related to these missions were given. Concerning the list of objectives of
SCVII only a view aspects could be worked off. The idea to establish a forum of
discussion could not be realized. There was only a minor feedback from the
members. Looking back we can say that this is understandable in so far as the
groups involved in the preparation and execution of the gravity satellite
missions have to work under competitive conditions and are to a certain amount
independent from the input of a broader community. Therefore, it remained the
service of SCVII for those who are not directly involved in a mission proposal
or a mission project. This is the reason that one initiative of SCVII related
to the generation of data sets of simulated CHAMP, GRACE, GOCE and 24 GPS
satellite orbits turned out to be quite successful. The generated data sets
cover a time period of 30 days and include the velocities, accelerations, and
for GOCE the tensor components for specified gravity fields and reference frame
specifications. As a first step, the mission scenarios were generated based on
very simple models concerning the reference systems and the noise models. In
2001 SRON, the Netherland’s Space Agency, provided various error models for the
tensor components of GOCE. Details were given in readme-files and additional
information material on mathematical details were included. It took some
iteration steps until the material was adapted to the needs of the users. The
data sets were planned to be used for investigations related to satellite borne
gravity field missions, especially to compare
In the starting phase the simulation
material was available in packed form on two CD-roms. It could be received
after demand or downloaded together with additional information material from
the SCVII web page. Later a FTP-server was created, where the simulation
material could be downloaded. The computation comparisons should be done for
global and regional analysis techniques. As regional example an area with a
rough gravity field in the South-East-Asian area has been selected (fig, geoid
heights in m):

The response to the offer to provide
the simulation scenarios was very encouraging. The CD-roms have been sent to 21
members of various institutions and countries on demand. Because of the fact
that the simulation material could be downloaded from the SCVII FTP-server the
detailed number of those who downloaded the material is not known. But it seems
that many used the data for comparisons and simulation computations. Besides
this activity the bibliography of SGG and SST related references had been
moderately improved. Unfortunately, there was not much response to report all
papers and articles to the SCVII chair to be included in the publication list.
This is the reason that the bibliography is not up-to-date by far, especially
concerning the huge number of papers published during the last years.
Nevertheless, the bibliography gives an overview of references from the early
days of SGG and SST activities. In 2001 a SC VII-meeting had been held
occasional the IAG General Assembly in Budapest.
Conclusions and outlook
The realization of the missions
CHAMP and GRACE and the fact that the real data are (partly) available made the
simulation material of these missions unnecessary, at least for most of the
applications. Nowadays, there are many groups around the world involved in the
development of software for analyzing satellite born gravity field
observations, as satellite gravity gradiometry observations,
satellite-to-satellite tracking data, either in the high-low or in the low-low
mode. To provide a simple platform for any scientist or for groups of
scientists of the international community with the task to check and to improve
his/their own developments or to compare the effectiveness of their procedures
to the procedures of others it seems still to be useful to use a unique data
set. For comparisons the simulated mission scenarios might be useful even
nowadays where real data are already available. It would be very useful to
compare the various approaches for global and regional gravity recovery
procedures, space-wise, time-wise, based on spherical harmonics, wavelets,
covariance functions or any other space-localizing gravity field
representation. More sophisticated simulation scenarios would be helpful
together with a selected set of real data. Another problem closely related to
the recovery procedure are the topics "calibration" and
"validation", but also data combination with terrestrial data or
alternative data sets. These topics should be important points for a task list
of a follow-on SC VII.