Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.12544/1938
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Kochtitzky, William H.
Edwards, Benjamin R.
Enderlin, Ellyn M.
Mariño Salazar, Jersy
Manrique Llerena, Nélida
Nevado Coropuna
Arequipa
Perú
Andes
2019-01-17T22:19:23Z
2019-01-17T22:19:23Z
2018-04
https://hdl.handle.net/20.500.12544/1938
Accurate quantification of rates of glacier mass loss is critical for managing water resources and for assessing hazards at ice-clad volcanoes, especially in arid regions like southern Peru. In these regions, glacier and snow melt are crucial dry season water resources. In order to verify previously reported rates of ice area decline at Nevado Coropuna in Peru, which are anomalously rapid for tropical glaciers, we measured changes in ice cap area using 259 Landsat images acquired from 1980 to 2014. We find that Coropuna Ice Cap is presently the most extensive ice mass in the tropics, with an area of 44.1 km2, and has been shrinking at an average area loss rate of 0.409 km2 a−1 (~0.71% a−1) since 1980. Our estimated rate of change is considerably lower than previous studies (1.4 km2 a−1 or ~2.43% a−1), but is consistent with other tropical regions, such as the Cordillera Blanca located ~850 km to the NW (~0.68% a−1). Thus, if glacier recession continues at its present rate, our results suggest that Coropuna Ice Cap will likely continue to contribute to water supply for agricultural and domestic uses until ~2120, which is nearly 100 years longer than previously predicted.
application/pdf
eng
Cambridge University Press
urn:issn:1727-5652
info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Instituto Geológico, Minero y Metalúrgico – INGEMMET
Repositorio Institucional INGEMMET
Desglaciación
Geocronología
Geomorfología de volcán
Glaciología
Paleoclima
Volcanes
Estratovolcán
Nevados
Glaciological natural hazards
Mountain glaciers
Remote sensing
Improved estimates of glacier change rates at Nevado Coropuna Ice Cap, Peru
info:eu-repo/semantics/article
Geología
GB
https://doi.org/10.1017/jog.2018.2
Journal of Glaciology
Peer reviewed
Journal of Glaciology, v.64, n, 244, abril 2018, pp. 175-184.

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