Accelerating Glacier Area Loss Across the Andes Since the Little Ice Age

Author:

Carrivick Jonathan L.1ORCID,Davies Morwenna1,Wilson Ryan2,Davies Bethan J.3ORCID,Gribbin Tom45ORCID,King Owen3,Rabatel Antoine6ORCID,García Juan‐Luis7,Ely Jeremy C.8ORCID

Affiliation:

1. School of Geography and water@leeds University of Leeds Leeds UK

2. Division of Geography University of Huddersfield Huddersfield UK

3. School of Geography Politics and Sociology Newcastle University Newcastle Upon Tyne UK

4. British Geological Survey Environmental Science Centre Keyworth UK

5. School of Geography Earth and Environmental Sciences University of Birmingham Edgbaston Birmingham UK

6. University Grenoble Alpes CNRS IRD INRAE Grenoble‐INP Institut des Géosciences de l’Environnement (IGE, UMR 5001) Grenoble France

7. Instituto de Geografía Facultad de Historia Geografía y Ciencia Política Pontificia Universidad Católica de Chile Santiago Chile

8. Department of Geography The University of Sheffield Sheffield UK

Abstract

AbstractAndean glaciers are losing mass rapidly but a centennial‐scale context to those rates is lacking. Here we show the extent of >5,500 glaciers during the Little Ice Age chronozone (LIA; c. 1,400 to c. 1,850) and compute an overall area change of −25% from then to year 2000 at an average rate of −36.5 km2 yr−1 or −0.11% yr−1. Glaciers in the Tropical Andes (Peru, Bolivia) have depleted the most; median −56% of LIA area, and the fastest; median −0.16% yr−1. Up to 10 × acceleration in glacier area loss has occurred in Tropical mountain sub‐regions comparing LIA to 2,000 rates to post‐2000 rates. Regional climate controls inter‐regional variability, whereas local factors affect intra‐region glacier response time. Analyzing glacier area change by river basins and by protected areas leads us to suggest that conservation and environmental management strategies should be re‐visited as proglacial areas expand.

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

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