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DC Field | Value | Language |
---|---|---|
dc.contributor.author | McGregor, HV | - |
dc.contributor.author | Fischer, MJ | - |
dc.contributor.author | Gagan, MK | - |
dc.contributor.author | Fink, D | - |
dc.contributor.author | Phipps, SJ | - |
dc.contributor.author | Wong, HKY | - |
dc.contributor.author | Woodroffe, CD | - |
dc.date.accessioned | 2014-09-17T05:30:01Z | - |
dc.date.available | 2014-09-17T05:30:01Z | - |
dc.date.issued | 2013-09-05 | - |
dc.identifier.citation | McGregor, H.V., Fischer, M.J., Gagan, M.K., Fink, D., Phipps, S.J., Wong, H., & Woodroffe, C.D. (2013). A weak El Niño/Southern Oscillation with delayed seasonal growth around 4,300 years ago. Nature Geoscience, 6(11), 949-953. doi:10.1038/ngeo1936 | en_AU |
dc.identifier.govdoc | 5226 | - |
dc.identifier.issn | 1752-0894 | - |
dc.identifier.uri | http://dx.doi.org/doi:10.1038/ngeo1936 | en_AU |
dc.identifier.uri | http://apo.ansto.gov.au/dspace/handle/10238/5868 | - |
dc.description.abstract | Palaeoclimate records indicate lower El Niño/Southern Oscillation (ENSO) variance during the middle Holocene compared with today, but the mechanisms leading to this muted variability are not clear. A 175-year oxygen isotope record from a Porites coral microatoll in the NINO3.4 region records persistently reduced ENSO variance about 4,300 years ago, and season-specific analyses of the record suggest that insolation played an important role in this change.© 2013, Nature Publishing Group. | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Nature Publishing Group | en_AU |
dc.subject | Southern Oscillation | en_AU |
dc.subject | Seasonal variations | en_AU |
dc.subject | Growth | en_AU |
dc.subject | Climates | en_AU |
dc.subject | Variations | en_AU |
dc.subject | Isotopes | en_AU |
dc.title | A weak El Niño/Southern Oscillation with delayed seasonal growth around 4,300 years ago | en_AU |
dc.type | Journal Article | en_AU |
dc.date.statistics | 2013-09-17 | - |
Appears in Collections: | Journal Articles |
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