Mineralogy-based quantitative precipitation and temperature reconstructions from annually laminated lake sediments (Swiss Alps) since AD 1580
We present quantitative autumn, summer and annual precipitation and summer temperature reconstructions from proglacial annually laminated Lake Silvaplana, eastern Swiss Alps back to AD 1580. We used X‐ray diffraction peak intensity ratios of minerals in the sediment layers (quartz qz, plagioclase pl...
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Veröffentlicht in: | Geophysical research letters 2008-07, Vol.35 (13), p.n/a |
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