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Local Recovery of Sub-Crustal Stress Due to Mantle Convection from Satellite-to-Satellite Tracking Data

Šprlák M., Eshagh M.

Acta Geophysica

2016

Vol. 64, no. 4

904--929

Two integral transformations between the stress function, differentiation of which gives the meridian and prime vertical components of the sub-crustal stress due to mantle convection, and the satellite-to-satellite tracking (SST) data are presented in this article. In the first one, the SST data are the disturbing potential differences between twin-satellites and in the second one the line-of-sight (LOS) gravity disturbances. It is shown that the corresponding integral kernels are well-behaving and therefore suitable for inversion and recovery of the stress function from the SST data. Recovery of the stress function and the stress components is also tested in numerical experiments using simulated SST data. Numerical studies over the Himalayas show that inverting the disturbing potential differences leads to a smoother stress function than from inverting LOS gravity disturbances. Application of the presented integral formulae allows for recovery of the stress from the satellite mission GRACE and its planned successor.

Ewolucja modeli pola grawitacyjnego uzyskanych na podstawie misji satelitarnych

Kraszewska K., Kozakiewicz M.

Materiały Budowlane

2013

nr 11

65--66

W artykule zaprezentowano wyznaczanie modeli pola grawitacyjnego z wykorzystaniem misji satelitarnych: GOCE, GRACE i CHAMP i pokazano, jak pomiary satelitarne wpłynęły na dokładność wyznaczenia kolejnych modeli w skali całego globu oraz obszaru południowej Europy.

This article shall determine the subject matter of the gravity field models using satellitemissions: GOCE, GRACE and CHAMP. As shown in the satellite measurements affect the precision of the following models for the entire world and for the area of southern Europe.