Surface Time-Variable Gravity Signals And Possible Sources Including Core Mass Flow

Details Surface Time-Variable Gravity Signals And Possible Sources Including Core Mass Flow Surface Time-Variable Gravity Signals And Possible Sources Including Core Mass Flow

Dec 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003agufm.g51c..06c&link_type=abstract

American Geophysical Union, Fall Meeting 2003, abstract #G51C-06

Physics

1213 Earth'S Interior: Dynamics (8115, 8120), 1227 Planetary Geodesy And Gravity (5420, 5714, 6019), 1507 Core Processes (8115), 1510 Dynamo Theories

Scientific paper

Over two decades of geodetic satellite-laser-ranging (SLR) data show that the variation of the Earth's oblateness parameter J2 has a clear seasonal signal of amplitude of about 3e-10 and a secular decrease of about -2.8e-11/year, superimposed on some interesting interannual fluctuations. Physically, any change in mass distribution on/inside the Earth will be reflected in the time-variable gravity signal obtained outside the Earth, according to Newton's gravitational law. Therefore, such signal contains contributions from all geophysical sources that redistribute mass, on all temporal and spatial scales, including those from the core. Besides Earth rotation and geomagnetic field variations, the time-variable gravity also contains information linking Earth surface observations with internal core dynamical processes. The time scales of the gravity signal are critical in helping differentiate different contributions. The atmosphere and hydrosphere are responsible for the seasonal and much of the interannual and intraseasoanl fluctuations, while the secular trend is due mainly to the post-glacial rebound but possibly core mass flow. To estimate the latter effect, we use our MoSST (Modular, Scalable, Self-consistent, Three-dimensional) core dynamics model to forward simulate the core flow, and density variation due to the core convection. Our results suggest that, when upward continued to the surface, the J2 component of the core mass redistribution can reach an overall amplitude of e-11/year, approaching the SLR detectability and significant in geophysical terms. We also find a general westward drift of the mass flow, with a speed comparable to that of the geomagnetic westward drift.

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