Rapid 20th century warming in the Caribbean and impact of remote forcing on climate in the northern tropical Atlantic as recorded in a Guadeloupe coral

Hetzinger, Steffen, Pfeiffer, Miriam, Dullo, Wolf-Christian, Garbe-Schönberg, Dieter and Halfar, Jochen (2010) Rapid 20th century warming in the Caribbean and impact of remote forcing on climate in the northern tropical Atlantic as recorded in a Guadeloupe coral Palaeogeography Palaeoclimatology Palaeoecology, 296 (1/2). pp. 111-124. DOI 10.1016/j.palaeo.2010.06.019.

[img] Text
Hetzinger_et_al._2010_PPP_GUAcoral_authors_copy.pdf - Published Version
Restricted to Registered users only

Download (2242Kb) | Contact

Supplementary data:

Abstract

We have generated 104-year long (1895–1999) monthly δ18O and Sr/Ca time series from a fast-growing
Diploria strigosa coral core drilled off Guadeloupe Island, Lesser Antilles. Coral Sr/Ca reliably records
interannual to decadal surface air temperature (SAT) variations in the region and shows a pronounced
warming of approximately 1.5 °C since 1950, with the strongest warming (1.2 °C) occurring since 1975. This
warming is also evident in SAT measured at Guadeloupe, which ends in 1951. Thus, our Sr/Ca series extends
the air temperature record by 56 years. We find that the past few decades are the warmest years over the
entire period of record. The accelerated warming since 1950 is accompanied by a pronounced decrease in
regional precipitation. This dampens the warming signal indicated by coral δ18O, which is too low (only 0.7–
0.8 °C since 1951). Consistently, δ18Osw estimated from the coral proxies also shows a strong decrease since
1950. Our data suggest an inverse relationship between SAT and precipitation (i.e. warmer and drier) for the
latter half of the 20th century with the strongest trends since the mid-1970s. This is consistent with recent
observational and model data, which report that while over the tropical oceans rainfall has increased due to
an increase in sea surface temperatures, precipitation over land regions is reduced. A continuation of this
warming and drying trend over Caribbean land regions would have severe societal consequences, especially
in the context of anthropogenic warming.
The El Niño Southern-Oscillation (ENSO) and the North Atlantic Oscillation (NAO) are the two major climate
modes affecting large-scale SST variability in the northern tropical Atlantic. Both Sr/Ca and δ18O show a close
relationship to ENSO and the NAO. A quantitative comparison between extremes in mean March–May coral
δ18O and the Nino3 and NAO indices imply that climate variability in the northern tropical Atlantic is mainly
forced by tropical Pacific and North Atlantic variability. Spectral analysis suggests that the relative
importance of ENSO and the NAO is frequency dependent, with ENSO dominating at interannual, and the
NAO dominating at interdecadal time scales.

Document Type: Article
Keywords: Corals; Climatology; Coral Sr/Ca; Coral δ18O; Diploria strigosa; North Atlantic Oscillation; El Niño Southern-Oscillation
Research affiliation: Kiel University
OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
OceanRep > The Future Ocean - Cluster of Excellence
Refereed: Yes
DOI etc.: 10.1016/j.palaeo.2010.06.019
ISSN: 0031-0182
Projects: Future Ocean
Date Deposited: 02 Sep 2010 08:49
Last Modified: 23 Jan 2017 13:52
URI: http://eprints.uni-kiel.de/id/eprint/8840

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...