Volcanic and Solar Forcing of the Tropical Pacific over the Past 1000 Years
The response of El Niño to natural radiative forcing changes over the past 1000 yr is investigated based on numerical experiments employing the Zebiak–Cane model of the tropical Pacific coupled ocean–atmosphere system. Previously published empirical results demonstrating a statistically significant...
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| Veröffentlicht in: | Journal of climate 2005-02, Vol.18 (3), p.447-456 |
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| container_end_page | 456 |
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| container_issue | 3 |
| container_start_page | 447 |
| container_title | Journal of climate |
| container_volume | 18 |
| creator | Mann, Michael E. Cane, Mark A. Zebiak, Stephen E. Clement, Amy |
| description | The response of El Niño to natural radiative forcing changes over the past 1000 yr is investigated based on numerical experiments employing the Zebiak–Cane model of the tropical Pacific coupled ocean–atmosphere system. Previously published empirical results demonstrating a statistically significant tendency toward El Niño conditions in response to past volcanic radiative forcing are reproduced in the model experiments. A combination of responses to past changes in volcanic and solar radiative forcing closely reproduces changes in the mean state and interannual variability in El Niño in past centuries recorded from fossil corals. The dynamics of El Niño thus appear to have played an important role in the response of the global climate to past changes in radiative forcing. |
| doi_str_mv | 10.1175/jcli-3276.1 |
| format | Article |
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Previously published empirical results demonstrating a statistically significant tendency toward El Niño conditions in response to past volcanic radiative forcing are reproduced in the model experiments. A combination of responses to past changes in volcanic and solar radiative forcing closely reproduces changes in the mean state and interannual variability in El Niño in past centuries recorded from fossil corals. The dynamics of El Niño thus appear to have played an important role in the response of the global climate to past changes in radiative forcing.</description><identifier>ISSN: 0894-8755</identifier><identifier>EISSN: 1520-0442</identifier><identifier>DOI: 10.1175/jcli-3276.1</identifier><language>eng</language><publisher>Boston, MA: American Meteorological Society</publisher><subject>Climate change ; Climate models ; Climatology. Bioclimatology. 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Previously published empirical results demonstrating a statistically significant tendency toward El Niño conditions in response to past volcanic radiative forcing are reproduced in the model experiments. A combination of responses to past changes in volcanic and solar radiative forcing closely reproduces changes in the mean state and interannual variability in El Niño in past centuries recorded from fossil corals. The dynamics of El Niño thus appear to have played an important role in the response of the global climate to past changes in radiative forcing.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/jcli-3276.1</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0894-8755 |
| ispartof | Journal of climate, 2005-02, Vol.18 (3), p.447-456 |
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| language | eng |
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| source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; JSTOR Archive Collection A-Z Listing |
| subjects | Climate change Climate models Climatology. Bioclimatology. Climate change Cooling Earth, ocean, space El Nino Exact sciences and technology Experiments External geophysics Global climate Global climate models Meteorology Modeling Ocean currents Ocean-atmosphere interaction Paleoclimatology Radiative forcing Tropical regions Volcanic eruptions |
| title | Volcanic and Solar Forcing of the Tropical Pacific over the Past 1000 Years |
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