Constraining glacier elevation and mass changes in South America

Braun M, Malz P, Sommer C, Farías Barahona D, Sauter T, Casassa G, Soruco A, Skvarca P, Seehaus T (2019)


Publication Language: English

Publication Type: Journal article, Letter

Publication year: 2019

Journal

Book Volume: 9

Pages Range: 130–136

Journal Issue: 2

URI: https://www.nature.com/articles/s41558-018-0375-7?WT.feed_name=subjects_climate-sciences

DOI: 10.1038/s41558-018-0375-7

Abstract

Excluding the large ice sheets of Greenland and Antarctica, glaciers in South America are large contributors to sea-level rise1. Their rates of mass loss, however, are poorly known. Here, using repeat bi-static synthetic aperture radar interferometry over the years 2000 to 2011/2015, we compute continent-wide, glacier-specific elevation and mass changes for 85% of the glacierized area of South America. Mass loss rate is calculated to be 19.43 ± 0.60 Gt a−1 from elevation changes above ground, sea or lake level, with an additional 3.06 ± 1.24 Gt a−1 from subaqueous ice mass loss not contributing to sea-level rise. The largest contributions come from the Patagonian icefields, where 83% mass loss occurs, largely from dynamic adjustments of large glaciers. These changes contribute 0.054 ± 0.002 mm a−1 to sea-level rise. In comparison with previous studies2, tropical and out-tropical glaciers — as well as those in Tierra del Fuego — show considerably less ice loss. These results provide basic information to calibrate and validate glacier-climate models and also for decision-makers in water resource management3.

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How to cite

APA:

Braun, M., Malz, P., Sommer, C., Farías Barahona, D., Sauter, T., Casassa, G.,... Seehaus, T. (2019). Constraining glacier elevation and mass changes in South America. Nature Climate Change, 9(2), 130–136. https://dx.doi.org/10.1038/s41558-018-0375-7

MLA:

Braun, Matthias, et al. "Constraining glacier elevation and mass changes in South America." Nature Climate Change 9.2 (2019): 130–136.

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