Interannual variability of transport and bifurcation of the North Equatorial Current in the tropical North Pacific Ocean

The relationship of the interannual variability of the transport and bifurcation latitude of the North Equatorial Current (NEC) to the El Niño-Southern Oscillation (ENSO) is investigated. This is done through composite analysis of sea surface height (SSH) observed by satellite altimeter during Octob...

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Published inChinese journal of oceanology and limnology Vol. 30; no. 1; pp. 177 - 185
Main Author 翟方国 胡敦欣
Format Journal Article
LanguageEnglish
Published Heidelberg Springer-Verlag 2012
SP Science Press
Springer Nature B.V
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ISSN0254-4059
2096-5508
1993-5005
2523-3521
DOI10.1007/s00343-012-1194-8

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Summary:The relationship of the interannual variability of the transport and bifurcation latitude of the North Equatorial Current (NEC) to the El Niño-Southern Oscillation (ENSO) is investigated. This is done through composite analysis of sea surface height (SSH) observed by satellite altimeter during October 1992–July 2009, and correspondingly derived sea surface geostrophic currents. During El Niño/La Niña years, the SSH in the tropical North Pacific Ocean falls/rises, with maximum changes in the region 0–15°N, 130°E–160°E. The decrease/increase in SSH induces a cyclonic/anticyclonic anomaly in the western tropical gyre. The cyclonic/anticyclonic anomaly in the gyre results in an increase/decrease of NEC transport, and a northward/southward shift of the NEC bifurcation latitude near the Philippine coast. The variations are mainly in response to anomalous wind forcing in the west-central tropical North Pacific Ocean, related to ENSO events.
Bibliography:North Equatorial Current; interannual variability; NEC bifurcation; E1 Nifio-Southern Oscillation
The relationship of the interannual variability of the transport and bifurcation latitude of the North Equatorial Current (NEC) to the E1 Nifio-Southern Oscillation (ENSO) is investigated. This is done through composite analysis of sea surface height (SSH) observed by satellite altimeter during October 1992-July 2009, and correspondingly derived sea surface geostrophic currents. During E1 Nifio/La Nifia years, the SSH in the tropical North Pacific Ocean falls/rises, with maximum changes in the region 0-15~N, 130~E-160~E. The decrease/increase in SSH induces a cyclonic/anticyclonic anomaly in the western tropical gyre. The cyclonic/anticyclonic anomaly in the gyre results in an increase/decrease of NEC transport, and a northward/southward shift of the NEC bifurcation latitude near the Philippine coast. The variations are mainly in response to anomalous wind forcing in the west-central tropical North Pacific Ocean, related to ENSO events.
ZHAI Fangguo , HU Dunxin 1Key Laboratory of Ocean Circulation and Waves, Chinese Academy of Sciences, Qingdao 266071, China 2 Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China 3 Graduate University of Chinese Academy of Sciences, Beijing 100049, China
37-1150/P
http://dx.doi.org/10.1007/s00343-012-1194-8
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ISSN:0254-4059
2096-5508
1993-5005
2523-3521
DOI:10.1007/s00343-012-1194-8