Reconstruction of sea surface temperature and salinity of the Arabian Sea
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2001
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| author | Kudrass, Hermann-Rudolph Hofmann, Annette Doose, Heidi Emeis, Kay-Christian Erlenkeuser, Helmut |
| author_facet | Kudrass, Hermann-Rudolph Hofmann, Annette Doose, Heidi Emeis, Kay-Christian Erlenkeuser, Helmut |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | High-frequency suborbital variations (Dansgaard-Oeschger cycles) characterize the climatic history of the Northern Hemisphere as observed in Greenland ice cores, deep-sea sediments of the North Atlantic, the Californian borderland, the Arabian Sea, the South China Sea, and the Chinese loess area. Paleoceanographic data from core KL126 from the Bay of Bengal in combination with data from the other Asian monsoonal areas indicate that the feedback processes involving snow and dust of the Tibetan Plateau vary the summer monsoon capacity to transport moisture into central South Asia and into the atmosphere. We postulate that the summer monsoon initiates, amplifies, and terminates these cycles in the Northern Hemisphere. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_735053 |
| institution | PANGAEA |
| language | en |
| publishDate | 2001 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Reconstruction of sea surface temperature and salinity of the Arabian Sea Kudrass, Hermann-Rudolph Hofmann, Annette Doose, Heidi Emeis, Kay-Christian Erlenkeuser, Helmut Bay of Bengal; BENGAL FAN; KL; Piston corer (BGR type); SO93/3; SO93/3_126KL; Sonne High-frequency suborbital variations (Dansgaard-Oeschger cycles) characterize the climatic history of the Northern Hemisphere as observed in Greenland ice cores, deep-sea sediments of the North Atlantic, the Californian borderland, the Arabian Sea, the South China Sea, and the Chinese loess area. Paleoceanographic data from core KL126 from the Bay of Bengal in combination with data from the other Asian monsoonal areas indicate that the feedback processes involving snow and dust of the Tibetan Plateau vary the summer monsoon capacity to transport moisture into central South Asia and into the atmosphere. We postulate that the summer monsoon initiates, amplifies, and terminates these cycles in the Northern Hemisphere. |
| title | Reconstruction of sea surface temperature and salinity of the Arabian Sea |
| topic | Bay of Bengal; BENGAL FAN; KL; Piston corer (BGR type); SO93/3; SO93/3_126KL; Sonne |
| url | https://doi.org/10.1594/PANGAEA.735053 |