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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Der lange Weg zur Erkenntnis: FCKW,Tasmania. The chronologies are analysed individually and collectively to explore Huon pine’s response to climate as a function of elevation. Three chronologies from greater than 700 metres in elevation exhibit a strong, direct response to temperature for most growing season months (.< 0.05), while t

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infringe

Studien zur Kommunikationswissenschaftrtance for paleoclimatic studies, as ahs been demonstrated by many recent publications based on the isotope records from polar ice cores. By means of direct comparison with instrumental data, this paper evaluates the potential of the deuterium and oxygen-18 records from two continental glaciers for

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Mammal

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Climatic Change at High Elevation Sites: An Overview,more 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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Panther

Variations of Snow Depth and Duration in the Swiss Alps Over the Last 50 Years: Links to Changes inr abundant or not. Periods with relative low snow amounts and duration are closely linked to the presence of persistent high surface pressure fields over the Alpine region during late Fall and in Winter. These high pressure episodes are accompanied by large positive temperature anomalies and low pre

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Decadal Variations in Climate Associated with the North Atlantic Oscillation,these changes have had a profound effect on regional distributions of surface temperature and precipitation. The changes over the North Pacific have been well documented and have contributed to increases in temperatures across Alaska and much of western North America and to decreases in sea surface

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20Th-Century Changes of Temperature in the Mountain Regions of Central Europe,ual variation of diurnal temperature range helps to distinguish unique climatic characteristics of high and low altitude stations. A comparison of the time series of extreme daily temperatures as well as mean temperature shows a good agreement between the low-lying stations and the mountain stations