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- W2016548 abstract "Pollen analysis, 14C and lichenometric dating of moraines, former elevations of the upper tree limit, and dendroclimatological and limnological data are some of the most relevant proxies for the reconstruction of climate variability and glacier behavior during the last millennium. A considerable number of paleoclimate reconstructions exist for the mountains of the Former Soviet Union. In this paper, we provide a regional overview of these datasets. Only regions with chronologically controlled and, preferably, high-resolution reconstructions will be considered here, namely, the Khibiny, the Urals, the Cherskogo Range, the Putorana Plateau, the Birranga Mountains, the Suntar-Khayata, the Kamchatka, the Caucasus, the Pamir-Alay, the Tien Shan, and the Altay Mountains (Fig. 1). This paper is a brief summary of the glacier and climate history of the last millennium and identifies achievements as well as gaps in our knowledge of paleoclimate in these regions. Ultimately, the identification of regional patterns of past climate changes will allow us to gain a better understanding of the causes behind climate variability on inter-annual to centennial timescales." @default.
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- W2016548 date "2005-01-01" @default.
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- W2016548 title "Glacier and Climate Variability in the Mountains of the Former Soviet Union during the last 1000 Years" @default.
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- W2016548 doi "https://doi.org/10.1007/1-4020-3508-x_7" @default.
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