Improving El Niño prediction using a space-time integration of Indo-Pacific winds and equatorial Pacific upper ocean heat content

2003 ◽  
Vol 30 (7) ◽  
Author(s):  
Allan J. Clarke ◽  
Stephen Van Gorder
Keyword(s):  
El Niño ◽  
El Nino ◽  
Time Integration ◽  
Heat Content ◽  
Space Time ◽  
Equatorial Pacific ◽  
Ocean Heat Content ◽  
Upper Ocean ◽  
Upper Ocean Heat Content

Quantifications of the Two “Flavours” of El Niño using Upper-Ocean Heat Content

2014 ◽  
Vol 52 (4) ◽  
pp. 351-362 ◽  
Author(s):  
Zhiwei Wu ◽  
Shengjie Chen ◽  
Jinhai He ◽  
Hua Chen
Keyword(s):  
El Niño ◽  
El Nino ◽  
Heat Content ◽  
Ocean Heat Content ◽  
Upper Ocean ◽  
Upper Ocean Heat Content

Dissimilarity among Ocean Reanalyses in Equatorial Pacific Upper-Ocean Heat Content and Its Relationship with ENSO

2022 ◽  
Vol 39 (1) ◽  
pp. 67-79
Author(s):  
Paxson K. Y. Cheung ◽  
Wen Zhou ◽  
Dongxiao Wang ◽  
Marco Y. T. Leung
Keyword(s):  
Heat Content ◽  
Equatorial Pacific ◽  
Ocean Heat Content ◽  
Upper Ocean ◽  
Upper Ocean Heat Content ◽  
Ocean Reanalyses

scholarly journals Can Tropical Pacific Winds Enhance the Footprint of the Interdecadal Pacific Oscillation on the Upper-Ocean Heat Content in the South China Sea?

2020 ◽  
Vol 33 (10) ◽  
pp. 4419-4437 ◽  
Author(s):  
Fuan Xiao ◽  
Dongxiao Wang ◽  
Lei Yang
Keyword(s):  
South China Sea ◽  
Wind Stress ◽  
South China ◽  
Heat Content ◽  
Equatorial Pacific ◽  
The South China Sea ◽  
Ocean Heat Content ◽  
Upper Ocean ◽  
Interdecadal Pacific Oscillation ◽  
Upper Ocean Heat Content

AbstractIn this study, an enhanced footprint of the interdecadal Pacific oscillation (IPO) on the upper-ocean heat content (OHC) in the South China Sea (SCS) since the 1990s is revealed. The negative OHC–IPO correlation is significant (r = −0.71) during 1990–2010 [period 2 (P2)], whereas it is statistically insignificant during 1960–80 [period 1 (P1)]. Analyses show that the scope of the equatorial Pacific wind anomalies is wider during P2 compared with that during P1 due to a larger east–west SST gradient and enhanced tropical warming in the Indian Ocean. When the IPO is negative during P2, a wider scope of the wind stress anomalies associated with the IPO could lead to 1) the southward migration of the North Equatorial Current bifurcation latitude (NECBL) by affecting the wind stress curl over the key region where it is near the climatological NECBL and 2) an increase in the interbasin pressure gradient (sea surface height difference) between the western Pacific and the SCS; these two processes strengthen the Kuroshio and weaken the Luzon Strait transport (LST) or SCS throughflow into the SCS. Also, 3) the equatorial Pacific wind anomalies are wide enough to directly weaken the LST in the SCS through the “island rule.” These three pathways finally change the oceanic gyre in the SCS and increase the OHC. Our results suggest that the scope of the tropical wind stress is the crucial factor when we consider the relationship between the upper ocean thermal conditions in the SCS and the Pacific variability.

Oceanic processes of upper ocean heat content associated with two types of ENSO

2017 ◽  
Vol 74 (2) ◽  
pp. 219-238 ◽  
Author(s):  
Junqiao Feng ◽  
Fei-fei Jin ◽  
Dunxin Hu ◽  
Shoude Guan
Keyword(s):  
Heat Content ◽  
Ocean Heat Content ◽  
Upper Ocean ◽  
Upper Ocean Heat Content
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