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Chapter and Conference Paper
Determination of Mass Balance of Polar Ice from Gravity
We use satellite solutions to the low degree zonal coefficients of the Earth’s gravitational potential, J 2 through J 7, to reveal large scale f...
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Article
MASS BALANCE OF POLAR ICE FROM LONG WAVELENGTH FEATURES OF THE EARTH'S GRAVITATIONAL FIELD
We have used satellite solutions to the low degree zonal harmonics of the Earth's gravitational potential, and rates of surface accumulation to partially constrain, by means of repeated forward solution, the t...
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Chapter
Constraints on Long-Period Sea Level Variations from Global Tide Gauge Data
We use monthly, global tide gauge data archived at the Permanent Service for Mean Sea Level to search for: (1) the 18.6-year ocean tide; (2) the 14-month pole tide in the deep ocean and in the North Sea region...