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| DOI | 10.1002/2015GL066728 | ||
| Año | 2016 | ||
| Tipo |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
We employ high-resolution, high-precision, helicopter-borne gravity observations of the Northern (NPI) and Southern Patagonia Icefields (SPI), South America, to infer ice thickness and bed topography using a three-dimensional model constrained by Fjord and lake bathymetry, and a land-ice mask. The results reveal thicker ice than the reflecting horizon of radar sounders, with 1 km deep ice for Glaciar San Rafael and Colonia (NPI) and 1.5 km deep ice for Glaciar Occidental (SPI). These bedrock troughs channelize fast motion of ice from the plateaus. Combining ice motion and thickness, we calculate balance accumulation levels of 3–6 m/yr water equivalent for the plateaus. Bed elevation remains below sea/lake level 15–20 km inland for Jorge Montt and O’Higgins, which favors retreat, and is at sea level for San Rafael, which halted its retreat. The results demonstrate the utility of airborne gravity surveys for providing critical data on ice volume, bed elevation, and balance accumulation of temperate ice masses.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | Gourlet, P. | - |
University of California, Irvine - Estados Unidos
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| 2 | Rignot, Eric | Hombre |
University of California, Irvine - Estados Unidos
Jet Propulsion Laboratory - Estados Unidos |
| 3 | RIVERA-IBANEZ, ANDRES | Hombre |
Centro de Estudios Científicos - Chile
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| 4 | CASASSA-ROGAZINSKI, GINO | Hombre |
Geoestudios - Chile
Universidad de Magallanes - Chile |
| Fuente |
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| Gordon and Betty Moore Foundation |
| National Aeronautics and Space Administration |
| CECs |
| California Institute of Technology |
| Jet Propulsion Laboratory |
| University of California, Irvine |
| University of California Irvine |
| Agradecimiento |
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| This work was performed at the University of California Irvine under grant 3280 from the Gordon and Betty Moore Foundation and at the Jet Propulsion Laboratory, California Institute of Technology under a grant with NASA. We thank R. Zamora and D. Ulloa from CECS for their assistance, and N. Glasser and one anonymous reviewer for comments on the manuscript. The gravity data are available upon request from the authors and at the National Snow and Ice Data Center, Boulder CO. |