NOAA/WDS Paleoclimatology - Nino3.4 SST 460 Year Reconstructions
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title: NOAA/WDS Paleoclimatology - Nino3.4 SST 460 Year Reconstructions
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date: 2011-06-29
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Anchor: DOI doi:10.25921/17jb-fg08
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code: noaa-recon-11749
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code: NCEI DSI 1200_02
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individualName: Tudhope, A.W.
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abstract: This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Climate Reconstruction. The data include parameters of climate reconstructions|corals and sclerosponges with a geographic location of Eastern Pacific Ocean. The time period coverage is from 410 to -57 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.
purpose: Records of past temperature, precipitation, and other climate variables derived from paleoclimate proxies. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations.
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keyword: Earth Science > Climate Indicators > Paleoclimate Indicators > Paleoclimate Reconstructions
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keyword: earth science > paleoclimate > climate reconstructions|corals and sclerosponges
keyword: earth science > paleoclimate > climate reconstructions|corals and sclerosponges
keyword: earth science > paleoclimate > climate reconstructions|corals and sclerosponges
keyword: earth science > paleoclimate > climate reconstructions|corals and sclerosponges
keyword: earth science > paleoclimate > climate reconstructions
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keyword: earth science > paleoclimate > climate reconstructions|corals and sclerosponges
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keyword: earth science > paleoclimate > reconstructions > atmospheric circulation
keyword: earth science > paleoclimate > reconstructions > sea surface temperature
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keyword: Atmospheric and Oceanic Circulation Patterns Reconstruction
keyword: ENSO
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keyword: What: Niño 3.4 sea surface temperature index; Material: null
keyword: What: Niño 3.4 sea surface temperature index; Material: null
keyword: What: Niño 3.4 sea surface temperature index; Material: null
keyword: What: Niño 3.4 sea surface temperature index; Material: null
keyword: What: Niño 3.4 sea surface temperature index; Material: multiple proxies
keyword: What: Niño 3.4 sea surface temperature index; Material: null
keyword: What: Niño 3.4 sea surface temperature index; Material: multiple proxies
keyword: What: Niño 3.4 sea surface temperature index; Material: multiple proxies
keyword: What: age; Material: null
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keyword: Ocean > Pacific Ocean > Eastern Pacific Ocean > Nino3.4 > LATITUDE > LONGITUDE
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keyword: DOC/NOAA/NESDIS/NCEI > National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
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otherConstraints: Cite as: Wilson, R.J.S.; Cook, E.R.; D'Arrigo, R.D.; Riedwyl, N.; Evans, M.N.; Tudhope, A.W.; Allan, R.J. (2011-06-29): NOAA/WDS Paleoclimatology - Nino3.4 SST 460 Year Reconstructions. [indicate subset used]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/17jb-fg08. Accessed [date].
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otherConstraints: Distribution liability: NOAA and NCEI make no warranty, expressed or implied, regarding these data, nor does the fact of distribution constitute such a warranty. NOAA and NCEI cannot assume liability for any damages caused by any errors or omissions in these data. If appropriate, NCEI can only certify that the data it distributes are an authentic copy of the records that were accepted for inclusion in the NCEI archives.
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otherConstraints: Use liability: NOAA and NCEI cannot provide any warranty as to the accuracy, reliability, or completeness of furnished data. Users assume responsibility to determine the usability of these data. The user is responsible for the results of any application of this data for other than its intended purpose.
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otherConstraints: Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.
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title: Reconstructing ENSO: the influence of method, proxy data, climate forcing and teleconnections
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date: 2010
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individualName: Wilson, R., E. Cook, R. D'Arrigo, N. Riedwyl, M.N. Evans, A. Tudhope, and R. Allan
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organisationName: Journal of Quaternary Science
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description: Wilson, R., E. Cook, R. D'Arrigo, N. Riedwyl, M.N. Evans, A. Tudhope, and R. Allan, 2010: Reconstructing ENSO: the influence of method, proxy data, climate forcing and teleconnections. Journal of Quaternary Science, 25, 62–78, 10.1002/jqs.1297
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description: Date Range: 1540 CE to 2007 CE; Date Range: 410 cal yr BP to -57 cal yr BP;
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westBoundLongitude: -170
eastBoundLongitude: -120
southBoundLatitude: -5
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supplementalInformation: STUDY NOTES: Nino3.4 SST reconstructions based on a variety of proxy data, utilizing 3 reconstruction methodologies, for the core ENSO region in the central and eastern tropical Pacific, and for other tropical regions displaying teleconnected ENSO responses. The first region is labeled the 'centre of action' (COA), located in the central and eastern Pacific, where SSTs are positively correlated with NINO3.4 SSTs. The second region is the 'teleconnection' (TEL) region covering all other tropical areas where SSTs are either inversely (e.g. Indonesia to Tonga) or positively (e.g. Indian Ocean) correlated with NINO3.4 SSTs. Independent reconstructions of annual NINO3.4 SSTs were developed for the COA and TEL regions, using three approaches: (1) composite plus regression, (2) principal component regression, and (3) regularised expectation maximisation. ABSTRACT SUPPLIED BY ORIGINATOR: In this study we compare three newly developed independent NINO3.4 sea surface temperature (SST) reconstructions using data from (1) the central Pacific (corals), (2) the TexMex region of the USA (tree rings) and (3) other regions in the Tropics (corals and an ice core) which are teleconnected with central Pacific SSTs in the 20th century. Although these three reconstructions are strongly calibrated and well verified, inter-proxy comparison shows a significant weakening in interproxy coherence in the 19th century. This breakdown in common signal could be related to insufficient data, dating errors in some of the proxy records or a breakdown in El Nino–Southern Oscillation's (ENSO's) influence on other regions. However, spectral analysis indicates that each reconstruction portrays ENSO-like spectral properties. Superposed epoch analysis also shows that each reconstruction shows a generally consistent 'El Nino-like' response to major volcanic events in the following year, while during years T+4 to T+7 'La Nina-like' conditions prevail. These results suggest that each of the series expresses ENSO-like 'behaviour', but this 'behaviour' does not appear to be spatially or temporally consistent. This result may reflect published observations that there appear to be distinct 'types' of ENSO variability depending on location within the tropical Pacific. Future work must address potential dating issues within some proxies (i.e. sampling of multiple coral heads for one location) as well as assessing the time stability of local climate relationships with central Pacific SSTs. More emphasis is needed on sampling new and extending old coral proxy records from the crucial central and eastern tropical Pacific region.
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