Glaciología

Glaciares de Chile

Antártica

"Glacier fluctuations in extratropical South America during the past 1000 years"

Masiokas, M., Rivera, A., Espizúa, L.,Villalba, R., Delgado S., and J.C. Aravena. (2009) : “Glacier fluctuations in extratropical South America during the past 1000 years” Palaeogeography, Palaeoclimatology, Palaeoecology, 281, 242 – 268.

Resumen / Abstract.

This paper presents an updated, extensive review of glacier fluctuations during the past 1000 years in the extratropical Andes of South America between ca. 17° and 55°S. Given the variety of environmental conditions and evidence available for glacier fluctuations across this wide latitudinal range, regional accounts are given for the Desert Andes (∼17°–31°S), the Andes of central Chile and Argentina (31°–36°S), and the North (36°–45°S) and South (45°–55°S) Patagonian Andes. The techniques, dating limitations, and interpretations of the glacier records along this transect are also discussed. Information on glacier fluctuations in the Desert Andes is limited to the 20th century. Documentation on past glacier variations is more abundant in the Central Chilean-Argentinean Andes, but the number of chronologies dealing with glacier fluctuations prior to the 1900s is also limited. Most records indicate that glaciers were generally more extensive prior to the 20th century, with dates of maximum expansion ranging from the 16th to the 19th centuries. The number and extent of glaciers increase significantly in the Patagonian region, where theevidence available for dating glacier variations during the past centuries is more abundant and the dating control for glacier events is generally better than in the northern parts of the study area. 




 

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