Atlantic SST gradient and the influence of ENSO

The relationship between the boreal winter El Niño SST anomaly and boreal spring tropical Atlantic SST gradient (North Atlantic minus South Atlantic) is investigated using a long, detrended SST record. For both El Niño and La Niña, concordant cases (same sign for NINO3 index and Atlantic SST gradien...

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Bibliographic Details
Main Authors: Huang, Huei-Ping, Robertson, Andrew W., Kushnir, Yochanan
Format: Text
Language:unknown
Published: Columbia University 2005
Subjects:
Southern oscillation
Atmosphere
Climatic changes
North Atlantic
Online Access:https://dx.doi.org/10.7916/d8708b45
https://academiccommons.columbia.edu/doi/10.7916/D8708B45
Description
Summary:The relationship between the boreal winter El Niño SST anomaly and boreal spring tropical Atlantic SST gradient (North Atlantic minus South Atlantic) is investigated using a long, detrended SST record. For both El Niño and La Niña, concordant cases (same sign for NINO3 index and Atlantic SST gradient) slightly dominate over discordant ones, reflecting the fact that the NINO3 index correlates more strongly with the North Atlantic than the South Atlantic SST anomaly. The ratio of the numbers of concordant and discordant cases is 4:3 overall, indicating strong non-ENSO influences on the Atlantic SST gradient. The composite of the concordant cases shows an SST anomaly in the North Atlantic with the same sign as NINO3 and an opposite-signed anomaly off the southwest coast of Africa resembling "Benguela Niño". That of the discordant cases is dominated by a pre-existing SST anomaly with the same sign as NINO3 in the south-central South Atlantic.

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