Glaciares de Chile
- Glaciares del Volcán Melimoyu
- Glaciares del Nevado de Queulat
- Glaciares del Volcán Mentolat
- Glaciares del Volcán Cay
- Glaciares del Volcán Macá
- Glaciares del Volcán Hudson
- Glaciar Erasmo
- Glaciar San Rafael
- Glaciar San Quintín
- Campo de Hielo Norte
- Glaciar Nef
- Glaciar Colonia
- Lago Cachet II
- Glaciar Steffen
- Glaciares del Monte San Lorenzo
- Glaciar Jorge Montt
- Glaciar Lucía
- Glaciar Los Moscos
- Glaciar Bernardo
- Glaciar O’Higgins
- Glaciar Chico
- Campo de Hielo Sur
- Campo de Hielo Sur
- Glaciar Témpanos
- Glaciar Pío XI
- Glaciar Viedma
- Glaciar Perito Moreno
- Glaciar Dickson
- Glaciar Olvidado
- Glaciar Grey
- Glaciar Amalia
- Glaciar Pingo
- Glaciar Tyndall
- Glaciar Balmaceda
- Isla Desolación
- Glaciares de la Isla Santa Inés
- Seno Gabriel
- Glaciar Schiaparelli
- Glaciar Marinelli
- Fiordo Parry
- Cordillera Darwin
- Glaciar Garibaldi
- Glaciar Roncagli
- Glaciares Isla Hoste
Antártica
"Glacier variations in the Southern Patagonia Icefield and their Relation with Climate"
Casassa, G., Rivera, A. & Carrasco, J. (2000) : “Glacier variations in the Southern Patagonia Icefield and their Relation with Climate” In: Sixth International Conference on Southern Hemisphere Meteorology and Oceanography, pp. 312-313.
Resumen / Abstract.
Glacier variations during the past 50 years have been determined for the major 48 outlet glaciers of the Southern Patagonia Icefield, southern South America. Most glaciers exhibit a clear retreat, a few are in near-equilibrium and one has been advancing. These variations are analyzed in relation to air temperature and precipitation records of stations around the icefield. The main conclusion is that the generalized glacier retreat is a direct response to regional warming and also to a decrease in precipitation observed this century.
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