DLR Hompage NASA Homepage GFZ Homepage CSR Homepage GRACE Homepage
GRACE - Gravity Recovery and Climate Experiment Homepage
Home Science Operations Mission Flight Systems CSR
Games Education Publications Gallery Search

RL05 Products (Updated: 2013-02-08)

The GGM03 Models

Science Data Products

Level-3 Data Products

Science Team Meeting

Gravity Measurement

GPS Occultation Measurement

Other Science Contributions

Technical Science Information

GRACE Partners

Download Adobe Acrobat Reader

SDS - internal

Science - internal
Update (July 14, 2004): The increased accuracy and resolution of GGM02 field compared to GGM01 is evident, for example, in the images of gravity anomalies across the Tonga trench.

For a more detailed description of such features, please see below.

Solid Earth Science

Tectonic features are now resolved by GGM01S that were previously unobservable in gravity models derived from geodetic satellites alone. These features represent various geophysical phenomena in areas such as the Tonga/Kermadec region (a subduction zone where one tectonic plate slides under another), the Himalayan/Tibetan Plateau region (an area of uplift due to colliding plates), and the mid-Atlantic ridge (an active spreading center in the middle of the Atlantic ocean where new crust is being created). Subduction zones, for example, were previously only observed in space-based gravity models as a broad area of high gravity due to the combined mass of the subducting slab beneath a volcanic arc. It is known from high-resolution terrestrial gravity measurements (e.g., from planes or ships), however, that complex, smaller scale gravity features can be observed in such regions. Previously, such insights from terrestrial measurements were limited to very localized areas (due to cost & accessibility) and interpretation over large regions was difficult.

Gravity anomalies from GGM01S reveal important geophysical features
These detailed geophysical features are being detected by GRACE with no surface gravity measurements. (July 21, 2003)

Looking specifically at the Tonga-Kermadec region as an example, there are now many of the classic gravity anomaly features of subduction evident from the space-based GGM01S gravity model. As we look from east to west across this region (starting from right-center of the left panel) we observe in the gravity anomaly map a high (yellow), a low (blue/green), a high (red), and drop to a smaller high (yellow). It is in this region that the Pacific Plate is being subducted under the Australian Plate and the gravity anomalies observed correspond to, in order from east to west:

  • a gravity high from the subducting Pacific Plate flexing upward before heading down beneath the Indian Australian plate
  • a gravity low from the Pacific Plate being thrust down. Water and low-density sediments now fill the space once occupied by denser oceanic plate
  • a gravity high from the dense subducting slab overlain by region of mountains and volcanoes.
  • a drop to a lower gravity anomaly magnitude in the Lau Basin as the Australian Plate is 'pulled' towards the Pacific Plate, forming a back-arc basin.

Tonga-Kermadec region Mariana trench
Tonga-Kermadec region Mariana trench
Similar features can also be easily seen along the Mariana Trench, considered the deepest known point in the ocean at 11,033 m (36,198 feet).

For further reading:

  • Kious, W.J. and R.I. Tilling, The Dynamic Earth: The Story of Plate Tectonics, USGS, Online Edition. http://pubs.usgs.gov/publications/text/dynamic.html
  • Fowler, C.M.R., The Solid Earth: An Introduction to Global Geophysics, Cambridge University Press, 1990.
  • Turcotte, D.L. and G. Schubert, Geodynamics, Cambridge University Press, 2nd ed., 2001.
Go to the UTopia web site
Go to University of Texas web site


The GRACE mission is jointly implemented by NASA and DLR under
the NASA Earth System Science Pathfinder Program.

Last Modified: Fri Oct 29, 2004