Reconstructing ENSO:the influence of method, proxy data, climate forcing and teleconnections

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...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Wilson, Rob, Cook, Edward, D'Arrigo, Rosanne, Riedwyl, Nadja, Evans, Michael N., Tudhope, Alexander, Allan, Rob
Format: Article in Journal/Newspaper
Language:English
Published: 2010
Subjects:
ENSO
reconstruction
corals
tree rings
teleconnection
SEA-SURFACE TEMPERATURE
CORAL-BASED RECONSTRUCTION
CONTINENTAL UNITED-STATES
TREE-RING CHRONOLOGIES
CARBON ISOTOPIC RECORD
PAST 4 CENTURIES
EL-NINO
SOUTHERN-OSCILLATION
TROPICAL PACIFIC
STABLE OXYGEN
Pacific
ice core
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/reconstructing-enso(110c4a74-6046-4a40-bbf2-b51e2727c90d).html
https://doi.org/10.1002/jqs.1297
http://www.scopus.com/inward/record.url?scp=71149118787&partnerID=8YFLogxK
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Summary: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. Copyright (C) 2009 John Wiley & Sons, Ltd. and Crown Copyright 2009.

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