Migration of the subtropical front as a modulator of glacial climate
Ice cores extracted from the Antarctic ice sheet suggest that glacial conditions, and the relationship between isotopically derived temperatures and atmospheric P<sub>CO₂</sub> have been constant over the last 800,000 years of the Late Pleistocene epoch. But independent lines of evidence...
| Päätekijät: | , |
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| Aineistotyyppi: | Journal article |
| Kieli: | English |
| Julkaistu: |
Macmillan Publishers Ltd.
2009
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| Aiheet: |