Climate Variability and Change in High Elevation Regions: Past, Present & Future:
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 seas...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
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Dordrecht
Springer Netherlands
2003
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| Schriftenreihe: | Advances in Global Change Research
15 |
| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | 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 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 |
| Beschreibung: | 1 Online-Ressource (VI, 283 p. 122 illus., 10 illus. in color) |
| ISBN: | 9789401512527 |
| DOI: | 10.1007/978-94-015-1252-7 |
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| 520 | |a 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 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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| spelling | Climate Variability and Change in High Elevation Regions: Past, Present & Future edited by Henry F. Diaz Dordrecht Springer Netherlands 2003 1 Online-Ressource (VI, 283 p. 122 illus., 10 illus. in color) txt rdacontent c rdamedia cr rdacarrier Advances in Global Change Research 15 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 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 Earth Sciences Atmospheric Sciences Climate Change Environmental Management Earth sciences Atmospheric sciences Climate change Environmental management Klimaänderung (DE-588)4164199-1 gnd rswk-swf Hochgebirge (DE-588)4025207-3 gnd rswk-swf 1\p (DE-588)1071861417 Konferenzschrift 2001 Davos gnd-content Hochgebirge (DE-588)4025207-3 s Klimaänderung (DE-588)4164199-1 s 2\p DE-604 Diaz, Henry F. edt Erscheint auch als Druck-Ausgabe 9789048163229 https://doi.org/10.1007/978-94-015-1252-7 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Climate Variability and Change in High Elevation Regions: Past, Present & Future Earth Sciences Atmospheric Sciences Climate Change Environmental Management Earth sciences Atmospheric sciences Climate change Environmental management Klimaänderung (DE-588)4164199-1 gnd Hochgebirge (DE-588)4025207-3 gnd |
| subject_GND | (DE-588)4164199-1 (DE-588)4025207-3 (DE-588)1071861417 |
| title | Climate Variability and Change in High Elevation Regions: Past, Present & Future |
| title_auth | Climate Variability and Change in High Elevation Regions: Past, Present & Future |
| title_exact_search | Climate Variability and Change in High Elevation Regions: Past, Present & Future |
| title_full | Climate Variability and Change in High Elevation Regions: Past, Present & Future edited by Henry F. Diaz |
| title_fullStr | Climate Variability and Change in High Elevation Regions: Past, Present & Future edited by Henry F. Diaz |
| title_full_unstemmed | Climate Variability and Change in High Elevation Regions: Past, Present & Future edited by Henry F. Diaz |
| title_short | Climate Variability and Change in High Elevation Regions: Past, Present & Future |
| title_sort | climate variability and change in high elevation regions past present future |
| topic | Earth Sciences Atmospheric Sciences Climate Change Environmental Management Earth sciences Atmospheric sciences Climate change Environmental management Klimaänderung (DE-588)4164199-1 gnd Hochgebirge (DE-588)4025207-3 gnd |
| topic_facet | Earth Sciences Atmospheric Sciences Climate Change Environmental Management Earth sciences Atmospheric sciences Climate change Environmental management Klimaänderung Hochgebirge Konferenzschrift 2001 Davos |
| url | https://doi.org/10.1007/978-94-015-1252-7 |
| work_keys_str_mv | AT diazhenryf climatevariabilityandchangeinhighelevationregionspastpresentfuture |