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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Systems with Spontaneous Symmetry Breakingegative trends in southern South America are due to mostly changes in summer (December to February) temperatures. Changes in the Pacific Decadal Oscillation (PDO) around 1976 are felt in summer temperatures at most stations in the Pacific domain, starting a period with increased temperature across t

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Systems with Spontaneous Symmetry Breakingnologies in the different ranges, consistent with their containing a growing season temperature signal on decadal time scales. The four upper forest border chronologies all show an anomalous increase in growth since the late 19th century, and an apparent change in climate control of ring growth.

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https://doi.org/10.1007/978-0-8176-4779-7he previous two centuries. With the exception of the 1930s, streamflow during the 20th century exceeded average flows during the previous 200 years. The drought of the 1930s resulted in the lowest flows during the last three centuries, however, this probably does not represent a worst-case scenario

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Climate Variability and Change in High Elevation Regions: Past, Present & Future

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1574-0919 s 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 interpret978-90-481-6322-9978-94-015-1252-7Series ISSN 1574-0919 Series E-ISSN 2215-1621

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Climatic Change in Mountain Regions: A Review of Possible Impacts,th issues, and tourism. A portfolio of research and policy options are discussed in the concluding section, as a summary of what the IYM and other concerned international networks consider to be the priority for mountain environmental protection, capacity building, and response strategies in the fac