Stenni et al.’s calculations result in two time series of relative temperature change, one for the Antarctic plateau and the other for the moisture source for East Antarctic precipitation. General circulation models and isotopic tracer studies show that this moisture source is the area between 30º a...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.693.7614 2023-05-15T13:49:54+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.693.7614 http://www.mantleplumes.org/WebDocuments/TopDown.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.693.7614 http://www.mantleplumes.org/WebDocuments/TopDown.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mantleplumes.org/WebDocuments/TopDown.pdf text ftciteseerx 2016-01-08T18:31:59Z Stenni et al.’s calculations result in two time series of relative temperature change, one for the Antarctic plateau and the other for the moisture source for East Antarctic precipitation. General circulation models and isotopic tracer studies show that this moisture source is the area between 30º and 50ºS in the Indian Ocean. A potential problem remains. The deu-terium excess proxy for SST can only tell us about the evaporation temperature of the average moisture reaching Dome C. The SST variations reported by Stenni et al. may thus merely reflect changes in the rela-tive contribution of moisture from different Text Antarc* Antarctic Unknown Antarctic The Antarctic Indian Tive ENVELOPE(12.480,12.480,65.107,65.107) |
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Open Polar |
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Unknown |
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English |
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Stenni et al.’s calculations result in two time series of relative temperature change, one for the Antarctic plateau and the other for the moisture source for East Antarctic precipitation. General circulation models and isotopic tracer studies show that this moisture source is the area between 30º and 50ºS in the Indian Ocean. A potential problem remains. The deu-terium excess proxy for SST can only tell us about the evaporation temperature of the average moisture reaching Dome C. The SST variations reported by Stenni et al. may thus merely reflect changes in the rela-tive contribution of moisture from different |
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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=10.1.1.693.7614 http://www.mantleplumes.org/WebDocuments/TopDown.pdf |
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ENVELOPE(12.480,12.480,65.107,65.107) |
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Antarctic The Antarctic Indian Tive |
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Antarctic The Antarctic Indian Tive |
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Antarc* Antarctic |
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Antarc* Antarctic |
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http://www.mantleplumes.org/WebDocuments/TopDown.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.693.7614 http://www.mantleplumes.org/WebDocuments/TopDown.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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1766252492150013952 |