TY - JOUR

T1 - Local gravity field continuation for the purpose of in-orbit calibration of GOCE SGG observations

AU - Pail, Roland

PY - 2003

Y1 - 2003

N2 - The use of ground gravity data in wellsurveyed areas, continued upward to satellite altitude, is one of the most promising external absolute in-orbit calibration/validation methods for GOCE satellite gravity gradient (SGG) observations. Based on a synthetic gravity test environment - providing in addition to statistical error information also absolute error estimates - several upward continuation methods, e.g. least squares collocation, equivalent source techniques using point masses or area density distributions defined on a spherical surface section, are described, assessed and compared. It turns out that all these strictly local approaches fail to work sufficiently accurate. Consequently, a combined adjustment strategy is proposed, supporting the high-quality gravity field information within the well-surveyed test area with a low-accuracy, but globally defined Earth model. Under quite realistic assumptions the upward continuation is performed with rms errors in the order of 1 mE. The most crucial limiting factor of this method is spectral leakage in the course of an adequate representation of the initial gravity information, which can be overcome by an enlargement of the parameter model in combination with a priori filtering of the initial gravity data.

AB - The use of ground gravity data in wellsurveyed areas, continued upward to satellite altitude, is one of the most promising external absolute in-orbit calibration/validation methods for GOCE satellite gravity gradient (SGG) observations. Based on a synthetic gravity test environment - providing in addition to statistical error information also absolute error estimates - several upward continuation methods, e.g. least squares collocation, equivalent source techniques using point masses or area density distributions defined on a spherical surface section, are described, assessed and compared. It turns out that all these strictly local approaches fail to work sufficiently accurate. Consequently, a combined adjustment strategy is proposed, supporting the high-quality gravity field information within the well-surveyed test area with a low-accuracy, but globally defined Earth model. Under quite realistic assumptions the upward continuation is performed with rms errors in the order of 1 mE. The most crucial limiting factor of this method is spectral leakage in the course of an adequate representation of the initial gravity information, which can be overcome by an enlargement of the parameter model in combination with a priori filtering of the initial gravity data.

KW - Calibration

KW - GOCE

KW - Least squares adjustment

KW - Satellite gravity gradiometry

UR - http://www.scopus.com/inward/record.url?scp=33748050151&partnerID=8YFLogxK

U2 - 10.5194/adgeo-1-11-2003

DO - 10.5194/adgeo-1-11-2003

M3 - Article

AN - SCOPUS:33748050151

SN - 1680-7340

VL - 1

SP - 11

EP - 18

JO - Advances in Geosciences

JF - Advances in Geosciences

ER -