Ranges of moisture-source temperature estimated from Antarctic ice cores stable isotope records over glacial–interglacial cycles
A single isotope ratio (&delta;D or &delta;<sup>18</sup>O) of water is widely used as an air-temperature proxy in Antarctic ice core records. These isotope ratios, however, do not solely depend on air-temperature but also on the extent of distillation of heavy isotopes out of atm...
Αποθηκεύτηκε σε:
| Κύριοι συγγραφείς: | , , , , , |
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| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Copernicus Publications
2012-06-01
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| Σειρά: | Climate of the Past |
| Διαθέσιμο Online: | http://www.clim-past.net/8/1109/2012/cp-8-1109-2012.pdf |
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