Glacier decline in the Central Andes (33°S): Context and magnitude from satellite and historical data
Central Andes (33°S) represent a water-scarce region. During arid years, glacier runoff may constitute the main hydrological input at warm season and hence a steadfast deglacierization may represent a decrease in the regional water-budget. Ice-retreat enables landscape transitions from proglacial to...
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Published in | Journal of South American earth sciences Vol. 94; p. 102249 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.10.2019
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Subjects | |
Online Access | Get full text |
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