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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Frequency-Dependent Climate Signal in Upper and Lower Forest Border Tree Rings in the Mountains of ountain ranges in and near to the semiarid Great Basin. We confirm LaMarche’s (1974a) finding, based on a single mountain range in this same region, and a much shorter period of comparison, that climate responses are frequency dependent. In particular, upper and lower forest border chronologies in e

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Upper Yellowstone River Flow and Teleconnections with Pacific Basin Climate Variability during the ee-ring reconstructions of stream flow that extend the observational record by several centuries provide critical information on the short-term variability and multi-decadal trends in water resources. In this study, precipitation sensitive Douglas- fir (.) tree ring records are used to reconstruct a

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https://doi.org/10.1007/978-1-4684-9930-8th 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

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Complex Manifolds and Vector Bundles,evel heights tend to decrease with increasing latitude, although maximum heights are found well north of the equator, over the Tibetan Plateau. Correlations of interannual anomalies of temperature between paired high and low elevation sites are relatively high at 1 or 2 km above the mountain station

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https://doi.org/10.1007/BFb0081273sea surface temperatures (SST) realistically reproduce the observed warming trend as well as the spatial trend pattern. Model results further suggest that a significant fraction of the observed warming can be traced to a concurrent rise in SST in the equatorial Pacific and that the markedly differen