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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The ,-Functor in Algebraic Geometry, processes affected by climatic variability. Paleoecological and contemporary ecological data in forest ecosystems provided model parameterization and validation at broad spatial and temporal scales for tree growth, tree regeneration and treeline movement. For subalpine tree species, winter precipit

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https://doi.org/10.1007/978-94-015-1252-7Precipitation; Scale; Snow; climate change; development; ecosystem; environmental change

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Climate Variability and Change in High Elevation Regions: Past, Present and Future, 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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Climatic Change in Mountain Regions: A Review of Possible Impacts, 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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20th Century Climate Change in the Tropical Andes: Observations and Model Results,otential mechanisms related to the observed glacier retreat in the tropical Andes between 1950 and 1998. Observational evidence indicates that changes in precipitation amount or cloud cover over the last decades are minor in most regions and are therefore rather unlikely to have caused the observed

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The Impact that Elevation has on the ENSO Signal in Precipitation Records from the Gulf of Alaska Recipitation records from the Gulf of Alaska region. A number of studies based on records from primarily coastal stations and the mass balance of low elevation glaciers suggest there is at best a weak relationship between ENSO and precipitation anomalies in the region. In contrast, an analysis of an

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The Health of Glaciers: Recent Changes in Glacier Regime,ciers are shrinking slightly, and arctic glaciers are warming. Net mass balances during the last 40 years are predominately negative and both winter and summer balances (accumulation and ablation) and mass turnover are increasing, especially after 1988. Two principal components of winter balance tim