Glacier change in western North America: influences on hydrology, geomorphic hazards and water quality
The glaciers of western Canada and the conterminous United States have dominantly retreated since the end of the Little Ice Age (LIA) in the nineteenth century, although average rates of retreat varied from strong in the first-half of the twentieth century, with glaciers stabilizing or even advancin...
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Veröffentlicht in: | Hydrological processes 2009, Vol.23 (1), p.42-61 |
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Sprache: | eng |
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