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Titlebook: Climate Variability and Change in High Elevation Regions: Past, Present & Future; Henry F. Diaz Book 2003 Springer Science+Business Media

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发表于 2025-3-21 18:43:49 | 显示全部楼层 |阅读模式
书目名称Climate Variability and Change in High Elevation Regions: Past, Present & Future
编辑Henry F. Diaz
视频videohttp://file.papertrans.cn/228/227654/227654.mp4
丛书名称Advances in Global Change Research
图书封面Titlebook: Climate Variability and Change in High Elevation Regions: Past, Present & Future;  Henry F. Diaz Book 2003 Springer Science+Business Media
描述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 interpret
出版日期Book 2003
关键词Precipitation; Scale; Snow; climate change; development; ecosystem; environmental change
版次1
doihttps://doi.org/10.1007/978-94-015-1252-7
isbn_softcover978-90-481-6322-9
isbn_ebook978-94-015-1252-7Series ISSN 1574-0919 Series E-ISSN 2215-1621
issn_series 1574-0919
copyrightSpringer Science+Business Media Dordrecht 2003
The information of publication is updating

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发表于 2025-3-21 21:58:59 | 显示全部楼层
1574-0919 t 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
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Systems with Spontaneous Symmetry-Breakingand glaciers in western North America correlate with the Southern Oscillation and Northern Hemisphere air temperature. The degree of synchronization for distant glaciers relates to changes in time of atmospheric circulation patterns as well as differing dynamic responses.
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Climate Variability and Change in High Elevation Regions: Past, Present & Future978-94-015-1252-7Series ISSN 1574-0919 Series E-ISSN 2215-1621
发表于 2025-3-23 02:58:33 | 显示全部楼层
https://doi.org/10.1007/978-1-4684-9930-8 Davos, Switzerland on 25–28 June 2001. The workshop was titled ‘Climate Change at High Elevation Sites: Emerging Impacts’, and was convened to reprise an earlier conference on the same subject that was held in Wengen, Switzerland in 1995 (Diaz et al., 1997). The Davos meeting had as its main goals,
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https://doi.org/10.1007/978-1-4684-9930-8 on the ‘Mountain Regions’ Chapter 13 of Agenda 21, a basis document presented at the 1992 United Nations Conference on Environment and Development (UNCED) in Rio de Janeiro, and the International Year of the Mountains (IYM) 2002. The awareness that mountain regions are an important component of the
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