Variations of Zonal Gravity Field, Global Sea Level and Polar Motion Benson, C.S., "Stratigraphic studies in the snow and firn of the Greeniand ice sheet
Abstract. Satellite Laser Ranging (SLR) data have been analyzed by ourselves and other groups to provide ~imstes of the secular variations in the zonal harmonics of the geopotential field. While the SLR data available frum late-1992 onward me superior in satellite and temporal coverage (two station...
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| Format: | Text |
| Language: | English |
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1962
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.631.179 http://www.ncu.edu.tw/~ncu5680/deans/class/eng/1998-Phy Chem Earth.pdf |
| Summary: | Abstract. Satellite Laser Ranging (SLR) data have been analyzed by ourselves and other groups to provide ~imstes of the secular variations in the zonal harmonics of the geopotential field. While the SLR data available frum late-1992 onward me superior in satellite and temporal coverage (two station shifts in operation by the NASA Network), SLR alma extending back to the mid-1970s have been utilized by some of the analysis centers. Two solutions for secular zonals and the SPACE'93 secular polar motion rates are evaluated to provide constraints on geophysical models describing post-glacial rebound (PGR) and ice sheet ma~s balanceJsea level rise using an inverse method. The observed secular ate of glohal sea level change is also used as a constraint in various solutions. The benefits of forward modeling the water impoundment in reservoirs and the contributions of the moantain glaciers to the observed secular terms are discussed. Although the number of well resolved time dependent geopotential terms is limited, the inverse solutions are promising and provide results consistent with IPCC estimates of ice sheet mass balance and optimal estimates of mantle viscosity contrasts. |
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