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Sea Surface Temperatures in the Eastern Equatorial Pacific and Surface Temperatures in the Eastern Cordillera of Colombia During El Niño: Implications for Pliocene Conditions
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2017
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Source: Paleoceanography, 32(11), 1309-1314
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Journal Title:Paleoceanography
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Description:Regressions of surface temperatures in the Eastern Cordillera of Colombia with sea surface temperatures (SSTs) in the equatorial Paci fic, and speci fically with Niño1+2 and Niño3 temperature anomalies, show that the Eastern Cordillera warms or cools by approximately half of the amplitude of thevariation of SSTs in the eastern tropical Paci fic. Because Pliocene SSTs in the eastern tropical Paci fic resemble those during major El Niño events, when SSTs warm by ~4°C, these regressions suggest that the Pliocene Eastern Cordillera was warmer by ~2°C at both high and low elevations. Such post-Pliocene cooling is smallerthan the ~9 –12°C inferred from fossil pollen assemblages, but comparable to recent estimates of Anderson et al. of 3 ± 1°C (1 σ) since ~8 Ma. This change in surface temperature could be explained by a change in regional climate associated with a different tropical Paci fic SST distribution and therefore would require
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Source:Paleoceanography, 32(11), 1309-1314
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ISSN:0883-8305
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Rights Information:Other
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