When possible, a multi-proxy approach is preferable for inferring robust information on past climate evolution. A good example was given for southeastern Brazil (B. Turcq), where lake-level reconstructions, speleothemes (e.g., stalagmites), and pollen fossils allow the documentation of a continuous...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.185.1281 2023-05-15T15:03:05+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.185.1281 http://www.climateaudit.info/pdf/news/crowley.2005.EOS.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.185.1281 http://www.climateaudit.info/pdf/news/crowley.2005.EOS.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.climateaudit.info/pdf/news/crowley.2005.EOS.pdf for PMIP Experiments text ftciteseerx 2016-01-07T16:38:34Z When possible, a multi-proxy approach is preferable for inferring robust information on past climate evolution. A good example was given for southeastern Brazil (B. Turcq), where lake-level reconstructions, speleothemes (e.g., stalagmites), and pollen fossils allow the documentation of a continuous increase in precipitation since the Last Glacial Maximum. Progress has also been made about the knowledge of past ice sheets. Geophysical constraints on the history of the Laurentide Ice Sheet (W. R. Peltier) allow the inferring of the existence of large freshwater meltwater runoff flow into the Arctic during the Younger Dryas (12,700–11,700 years ago). There are also an increasing number of attempts to extract indices of past climate variability from high-resolution paleoclimatic records, although it has not been possible so far to infer information on interannual variability that is spatially consistent (S. Brewer). Finally, detailed analysis of modern climate and pollen data remains essential, as illustrated by an extensive survey of modern bioclimatic relationships presented by B. Thompson. Text Arctic Ice Sheet Unknown Arctic Peltier ENVELOPE(-63.495,-63.495,-64.854,-64.854) |
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When possible, a multi-proxy approach is preferable for inferring robust information on past climate evolution. A good example was given for southeastern Brazil (B. Turcq), where lake-level reconstructions, speleothemes (e.g., stalagmites), and pollen fossils allow the documentation of a continuous increase in precipitation since the Last Glacial Maximum. Progress has also been made about the knowledge of past ice sheets. Geophysical constraints on the history of the Laurentide Ice Sheet (W. R. Peltier) allow the inferring of the existence of large freshwater meltwater runoff flow into the Arctic during the Younger Dryas (12,700–11,700 years ago). There are also an increasing number of attempts to extract indices of past climate variability from high-resolution paleoclimatic records, although it has not been possible so far to infer information on interannual variability that is spatially consistent (S. Brewer). Finally, detailed analysis of modern climate and pollen data remains essential, as illustrated by an extensive survey of modern bioclimatic relationships presented by B. Thompson. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.185.1281 http://www.climateaudit.info/pdf/news/crowley.2005.EOS.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.185.1281 http://www.climateaudit.info/pdf/news/crowley.2005.EOS.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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