Journal of Tropical Oceanography ›› 2019, Vol. 38 ›› Issue (1): 1-10.doi: 10.11978/2018046CSTR: 32234.14.2018046

• Orginal Article •     Next Articles

Diagnostic analysis of upper-ocean heat content change in the equatorial Pacific and related mechanism

Ning LI1,2(), Xiaochun WANG1,2   

  1. 1. School of Marine Science, Nanjing University of Information Science & Technology, Nanjing 210044, China;
    2. Jiangsu Engineering Technology Research Center of Marine Environment Detection, Nanjing 210044, China
  • Received:2018-04-21 Revised:2018-07-04 Online:2019-01-16 Published:2019-01-16
  • Supported by:
    National Natural Science Foundation of China (41630423);National Key Research and Development Project (2016YFC1401601);2015 Program for Innovation Research and Entrepreneurship Team in Jiangsu Province

Abstract:

The ECCO v4 outputs from 1992 to 2015 is used to diagnose the heat content change in the equatorial Pacific box (118°E-75°W, 5°S-5°N, 0-300 m) and the Niño 3.4 box (170°-120°W, 5°S-5°N, 0-80 m). In the interannual time scale after removing the seasonal cycle, the temperature tendency term is driven by meridional heat transport and balanced by the surface heat flux term in the equatorial Pacific box. The transport across 5°N plays a dominant role in determining the magnitude and sign of temperature tendency term. For the Niño 3.4 box, the temperature tendency term of heat content is driven by the heat transport term and balanced by the surface heat flux term, with vertical transport playing an important role. The meridional heat transport of the equatorial Pacific box leads the vertical heat transport of the Niño 3.4 box on the interannual time scale, which explains why the heat content change of the equatorial Pacific leads the Niño 3.4 SST change by several months during the ENSO (El Nino-Southern Oscillation). Though there are subtle differences between the eastern Pacific and central Pacific ENSO events, two types of ENSO bear similarities in terms of heat content change mechanism. For the equatorial Pacific box, meridional heat transport plays a major role in determining its heat content change. For the Niño 3.4 box, vertical transport is the dominant term driving the heat content change in both developing and decaying stages of ENSO events.

Key words: upper-ocean heat content, change mechanism, El Niño, ECCO v4, equatorial Pacific