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On-land ice loss and glacial isostatic adjustment at the drake passage: 2003-2009
(WILLIAM BYRD PRESS FOR JOHN HOPKINS PRESS, 2011)
Evolution of Glacial Lake Cochrane During the Last Glacial Termination, Central Chilean Patagonia (∼47°S)
(2022)
Large ice-dammed lakes developed along the eastern margin of the Patagonian Ice Sheet (PIS) during the Last Glacial Termination (T1). Their spatial/temporal evolution, however, remains poorly constrained despite their ...
Crustal deformation across the Southern Patagonian Icefield observed by GNSS
(Elsevier Science, 2016-10)
Geodetic GNSS observations at 43 sites well distributed over the Southern Patagonian Icefield region yield site velocities with a mean accuracy of 1 mm/a and 6 mm/a for the horizontal and vertical components, respectively. ...
Observed crustal uplift near the Southern Patagonian Icefield constrains improved viscoelastic Earth model
(American Geophysical Union, 2014-02)
Thirty‒one GPS geodetic measurements of crustal uplift in southernmost South America determined extraordinarily high trend rates (> 35 mm/yr) in the north‒central part of the Southern Patagonian Icefield. These trends have ...
On-land ice loss and glacial isostatic adjustment at the drake passage: 2003-2009JOURNAL OF GEOPHYSICAL RESEARCHJ GEOPHYS RES
(WILLIAM BYRD PRESS FOR JOHN HOPKINS PRESS, 2011)
Past ice stream and ice sheet changes on the continental shelf off the Sabrina Coast, East Antarctica
(Elsevier B.V., 2018)
Our understanding of the response of the Antarctic ice sheet to climate and ocean changes requires the
improvement of current ice-atmosphere-ocean models and the accurate determination of boundary conditions
such as ice ...
Past ice stream and ice sheet changes on the continental shelf off the Sabrina Coast, East Antarctica
(Elsevier, 2018)
Our understanding of the response of the Antarctic ice sheet to climate and ocean changes requires the improvement of current ice-atmosphere-ocean models and the accurate determination of boundary conditions such as ice ...
The rapid and steady mass loss of the patagonian icefields throughout the GRACE Era: 2002-2017
(MDPI, 2019-04)
We use the complete gravity recovery and climate experiment (GRACE) Level-2 monthly time series to derive the ice mass changes of the Patagonian Icefields (Southern Andes). The glacial isostatic adjustment is accounted for ...