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Climate Variability and Change in High Elevation Regions: Past, Present & Future (Hardcover, 2003 ed.)
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Climate Variability and Change in High Elevation Regions: Past, Present & Future (Hardcover, 2003 ed.)
Series: Advances in Global Change Research, 15
Expected to ship within 10 - 15 working days
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Glaciers in the Andes are particularly important natural archives
of present and past climatic and environmental changes, in
significant part because of the N-S trend of this topographic
barrier and its influence on the atmospheric circulation of the
southern hemisphere. Strong gradients in the seasonality and amount
of precipitation exist between the equator and 30 Degrees S. Large
differences in amount east and west of the Andean divide also
occur, as well as a change from tropical summer precipitation
(additionally modified by the seasonal shift of the circulation
belts) to winter precipitation in the west wind belt (e. g. ,
Yuille, 1999; Garraud and Aceituno, 2001). The so-called 'dry axis'
lies between the tropical and extra tropical precipitation regimes
(Figure 1). The high mountain desert within this axis responds most
sensitively to the smallest changes in effective moisture. An
important hydro-meteorological feature on a seasonal to
inter-annual time-scale is the occurrence of EN SO events, which
strongly control the mass balance of glaciers in this area (e. g. ,
Wagnon et ai. , 2001; Francou et ai. , in press). The precipitation
pattern is an important factor for the interpretation of climatic
and environmental records extracted from ice cores, because much of
this information is related to conditions at the actual time of
precipitation, and this is especially so for stable isotope
records. Several ice cores have recently been drilled to bedrock in
this area. From Huascanin (Thompson et ai. , 1995), Sajama
(Thompson et ai.
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