Climatic implications of hydrologic changes in two lake catchments on the central Tibetan Plateau since the last glacial
The numerous and widespread lakes of the Tibetan Plateau (TP) constitute the largest group of alpine lakes on Earth. Some of the lakes are fed mainly by glacier meltwater and others by precipitation and groundwater. Past changes in the environments of these lakes differed because of differences in l...
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Veröffentlicht in: | Journal of paleolimnology 2017-08, Vol.58 (2), p.257-273 |
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