Titlebook: Climatic Change at High Elevation Sites; Henry F. Diaz,Martin Beniston,Raymond S. Bradley Book 1997 Springer Science+Business Media Dordre

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Climatic Change and Debris Flows in High Mountain Regions: The Case Study of the Ritigraben Torrentof permafrost may also play a role in the response of slope stability to extreme precipitation. At the foot of the Ritigraben, warming trends of both minimum and maximum temperatures have been particularly marked in the last two decades.

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Glacial Varve Thickness and 127 Years of Instrumental Climate Data: A Comparison,iently explained without considering summer precipitation and the number of days with snow per year. The wide range of observed correlation coefficients reveals the sensitivity of the archive to temporal variability of the climatic forcing factors and makes the development of transfer functions ambi

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Recent Trends in Tree-Ring Records from High Elevation Sites in the Andes of Northern Patagonia, reconstructed changes in snow cover duration in late spring and variations in mean annual temperature since A.D. 1750. Abrupt interannual changes in the mean annual temperature reconstruction are associated with strong to very strong El Ni?o-Southern Oscillation events. At upper treeline, tree grow

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A Changing Temperature Response with Elevation for , in Tasmania, Australia, temperature, precipitation and cloudiness, and their combined influence on photosynthesis, particularly at higher-elevation sites..A rotated Principal Component Analysis reveals a clear grouping of the high and low-elevation chronologies, represented by the first and second eigenvectors, respective

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G. Esser,M. Laucht,M. H. Schmidtmore distant past documented by a variety of climate-sensitive environmental indicators, such as tree-rings and alpine glaciers, that serve as a measure of the natural variability of climate in mountains over longer time scales..Detailed studies such as those found in this special issue of ., as wel

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G. Esser,M. Laucht,M. H. Schmidten heightened interest in this subject recently due to the finding that high-elevation tropical glaciers have been retreating and that significant melting from even the highest alpine regions has occurred in some areas during the past 20 years or so, as recorded in ice core records, which do not rev