speleothems are scattered over most continen-tal areas and provide exceptional chronology. They will allow investigation of spatially vari-able changes as climate fronts move across continental regions, and enable direct compar-ison of climate in distant regions, as recently demonstrated in a study...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.2427 http://science.sciencemag.org/content/sci/313/5787/622.full.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1029.2427 2023-05-15T16:38:52+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.2427 http://science.sciencemag.org/content/sci/313/5787/622.full.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.2427 http://science.sciencemag.org/content/sci/313/5787/622.full.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://science.sciencemag.org/content/sci/313/5787/622.full.pdf text ftciteseerx 2016-10-30T00:07:49Z speleothems are scattered over most continen-tal areas and provide exceptional chronology. They will allow investigation of spatially vari-able changes as climate fronts move across continental regions, and enable direct compar-ison of climate in distant regions, as recently demonstrated in a study of rainfall in the south-ern and northern Tropics (9). For paleoclimate, the past two decades have been the age of the ice core. The next two may be the age of the speleothem. Text ice core Unknown |
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Open Polar |
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ftciteseerx |
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English |
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speleothems are scattered over most continen-tal areas and provide exceptional chronology. They will allow investigation of spatially vari-able changes as climate fronts move across continental regions, and enable direct compar-ison of climate in distant regions, as recently demonstrated in a study of rainfall in the south-ern and northern Tropics (9). For paleoclimate, the past two decades have been the age of the ice core. The next two may be the age of the speleothem. |
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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=10.1.1.1029.2427 http://science.sciencemag.org/content/sci/313/5787/622.full.pdf |
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ice core |
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ice core |
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http://science.sciencemag.org/content/sci/313/5787/622.full.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1029.2427 http://science.sciencemag.org/content/sci/313/5787/622.full.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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