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PALEOLIMNOLOGY

Decadal-scale autumn temperature reconstruction back to AD 1580 inferred from the varved sediments of Lake Silvaplana (southeastern Swiss Alps).
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Blass, A.,Bigler, C.,Grosjean, M.,Sturm, M. 2007 Decadal-scale autumn temperature reconstruction back to AD 1580 inferred from the varved sediments of Lake Silvaplana (southeastern Swiss Alps). Quaternary Research Vol. 68, pp. 184-195.
Data Coverage North: 46.45 * South: 46.45
West: 9.8 * East: 9.8
Altitude: 1800 m

Start Year: 373 cal yr BP * End Year: 1 cal yr BP

Data:     Please Cite Data Contributors!
  Text: europe/switzerland/silvaplana2007.txt
  Excel: europe/switzerland/silvaplana2007.xls

Summary:

A quantitative high-resolution autumn (September¿November) temperature reconstruction for the southeastern Swiss Alps back to AD 1580 is presented here. We used the annually resolved biogenic silica (diatoms) flux derived from the accurately dated and annually sampled sediments of Lake Silvaplana (46°27'N, 9°48'E, 1800 m a.s.l.). The biogenic silica flux smoothed by means of a 9-yr running mean was calibrated (r=0.70, pb0.01) against local instrumental temperature data (AD 1864¿1949). The resulting reconstruction (±2 standard errors=±0.7°C) indicates that autumns during the late Little Ice Age were generally cooler than they were during the 20th century. During the cold anomaly around AD 1600 and during the Maunder Minimum, however, the reconstructed autumn temperatures did not experience strong negative departures from the 20th century mean. The warmest autumns prior to 1900 occurred around AD 1770 and 1820 (0.75 °C above the 20th-century mean). Our data agree closely with two other autumn temperature reconstructions for the Alps and for Europe that are based on documentary evidence and are completely unrelated to our data, revealing a very consistent picture over the centuries.
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noaa-lake-6059  (Last Revised: 2009-02-11 )

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