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Here we present a new study to quantify the ice mass evolution of the antarctica and greenland ice sheets (ais and gis) and gulf of alaska (goa) glaciers from a grace global mascon solution. We provide a new analysis of glacial isostatic adjustment (gia) with the goal of assembling the model uncertainty statistics required for rigorously extracting trends in surface mass from the gravity recovery and climate experiment (grace) mission. Fingerprints are physical basis functions that allow separation of gia from pd signals in grace
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The pd trend has little sensitivity to lower mantle viscosity Paper, we reiterate the relations that are being used to obtain gridded gia products, discuss all the possible pdsmc estimates that can be obtained from a given grace product and a gia model, and finally comment on the accuracy of each estimate of pdsmc and the need for consistency. The estimated pole tide can provide an independent estimate for modelling purposes.
