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Oceans
Sea-level fingerprint of continental water and ice mass change from GRACE
Article first published online: 12 OCT 2010
DOI: 10.1029/2010GL044770
Copyright 2010 by the American Geophysical Union.
Additional Information
How to Cite
, , , and (2010), Sea-level fingerprint of continental water and ice mass change from GRACE, Geophys. Res. Lett., 37, L19605, doi:10.1029/2010GL044770.
Publication History
- Issue published online: 12 OCT 2010
- Article first published online: 12 OCT 2010
- Manuscript Accepted: 23 AUG 2010
- Manuscript Revised: 17 AUG 2010
- Manuscript Received: 22 JUL 2010
Keywords:
- sea-level change;
- fingerprints;
- GRACE
[1] The Gravity Recovery and Climate Experiment satellites (GRACE) provide, for the first time, a method to directly measure mass exchange between the land and oceans over time. The dominant components of this exchange are due to continental ice loss/gain and land hydrology. Here, we determine the secular trend in these two components during the GRACE measurement era: 2003–2009. For each component, we model the distinct regional signatures or fingerprints of relative sea-level (RSL) change, obtaining maxima at low latitudes between ±40° N/S, but with particularly strong regional patterns. We estimate that the total ice and water mass loss from the continents is causing global mean sea-level to rise by 1.0 ± 0.4 mm/yr. Isolating the ice and hydrological signals, we find that the former is the sole net contributor to the global mean, while the latter dominates regional RSL changes in many coastal areas.