Glaciers of the outer and inner tropics: A different behaviour but a common response to climatic forcing

Details Glaciers of the outer and inner tropics: A different behaviour but a common response to climatic forcing Glaciers of the outer and inner tropics: A different behaviour but a common response to climatic forcing

Aug 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004georl..3116403f&link_type=abstract

Geophysical Research Letters, Volume 31, Issue 16, CiteID L16403

Other

14

Global Change: Climate Dynamics (3309), Hydrology: Glaciology (1863), Hydrology: Snow And Ice (1827), Meteorology And Atmospheric Dynamics: Boundary Layer Processes, Meteorology And Atmospheric Dynamics: Tropical Meteorology

Scientific paper

We have compared the annual surface energy balance (SEB) of Zongo Glacier (16°S, Bolivia, outer tropics) and Antizana Glacier 15 (0°S, Ecuador, inner tropics). On annual time scale energy fluxes are very similar in the ablation zone: turbulent heat fluxes compensate each other and net short-wave radiation dominates the SEB. Albedo is central in controlling the melting. Consequently solid precipitation occurrence manages the annual mass balance variability. In the outer tropics, the annual melting is directly related to the annual distribution of precipitation, the period December-February being crucial. However, in the inner tropics, liquid precipitation can occur on the ablation zone, and snowline altitude remains very sensitive to air temperature. Tropical glaciers react rapidly to El Niño events, mainly because of an induced precipitation deficit in the outer tropics and to a temperature increase in the inner tropics, both leading to a rise in snowline altitude.

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