Abstract
Using the high-resolution Hybrid Coordinate Ocean Model and the Navy Coupled Ocean Data Assimilation Global 1/12° Analysis (GLBa0.08), and the Objectively Analyzed Air–Sea Fluxes and the International Satellite Climatology Cloud Project products, we investigated the seasonal and interannual evolutions of heat budget, including the pseudo-heat content change, the net air–sea heat flux and the eddy heat transport (EHT), based on the time-dependent heat budget analysis in the western Pacific warm pool (WPWP). The results show that the pseudo-heat content change has significant semi-annual variation, which peaks in April–May and September. There is strong positive feedback between EHT and the net air–sea heat flux. EHT is important in balancing the sea surface heat flux into the WPWP. The seasonal EHT variability is dominated by its meridional component. On the interannual time scale, the zonal and vertical components of EHT show comparable amplitudes with the meridional one. The observed net air–sea heat flux in the WPWP is highly correlated with EHT and the pseudo-heat content change on the interannual time scale. The net air–sea heat flux leads the pseudo-heat content change by about half a month and leads EHT by about one month. The variations of the air–sea heat flux and EHT are connected to the El Niño Southern Oscillation events: during the development of El Niño (La Niña) events, the warm pool expanded eastward (retreated westward), the net air–sea surface flux into the WPWP increased (decreased) and EHT enhanced (weakened) significantly.
Similar content being viewed by others
References
Bjerknes J (1969) Atmospheric teleconnections from the equatorial Pacific. Mon Weather Rev 97:163–172
Cane MA, Zebiak SE (1985) A theory for El Ni~no and the Southern Oscillation. Science 228:1085–1087
Chen YL, Hu GX (2003) Influence of heat content anonialy in the Tropical Western Pacific warm pool region on onset of South China Sea summer monsoon. Acta Meteorol Sin 17:213–225
Chen JN, Wang HN (2009) The variation of heat status in the west Pacific warm pool and its eastward propagation. Oceanologia et Limnologia Sinca 40:669–673
Chen JN, Wang HN, Liu XY (2008) Spatial and temporal distribution of the western Pacific warm pool and the relationship with ENSO cycle. Acta Oceanol Sin 20:10–19
Chen X, Qiu B, Chen S, Qi Y, Du Y (2015) Seasonal eddy kinetic energy modulations along the North Equatorial Countercurrent in the western Pacific. J Geophys Res Oceans 120(9):635–6362
Cravatte S, Delcroix T, Zhang DX, Michael M, Julie L (2009) Observed freshening and warming of the western Pacific warm pool. Clim Dyn 33:565–589
Enfield DB, Lee S (2005) The heat balance of the Western Hemisphere warm pool. J Clim 18:2662–2681
Graham NE, Barnett TP (1987) Sea surface temperature, surface wind divergence, and convection over tropical oceans. Science 238:657–659
Gent PR (1991) The heat budget of the TOGA-COARE domain in an ocean model. J Geophys Res 96(S01):3323
Ho CR, Yan XH, Zhang Q (1995) Satellite observations of upperlayer variabilities in the western Pacific warm pool. Bull Am Meteorol Soc 76:669–679
Hoerling M, Kumar A (2003) The perfect ocean for drought. Science 299:691–694
Jayne SR, Marotzke J (2002) The oceanic eddy heat transport. J Phys Oceanogr 32:3328–3345
Levitus S (1983) Climatological atlas of the World Ocean. Eos Trans Am Geophys Union 64:962–963
Lin CY, Ho CR, Lee YH (2013) Thermal variability of the Indo-Pacific warm pool. Glob Planet Change 100:234–244
Meinen CS, McPhaden MJ (2001) Interannual variability in warm water volume transports in the equatorial Pacific during 1993–99. J Phys Oceanogr 31:1324–1345
Niiler PP, Stevenson J (1982) On the heat budget of tropical warm water pools. J Mar Res 40(Suppl):465–480
Palmer T, Mansfield D (1984) Response of two atmospheric general circulation models to sea surface temperature anomalies in the tropical East and West Pacific. Nature 310:483–485
Paulson CA, Simpson JJ (1977) Irradiance measurements in the upper ocean. J Phys Oceanogr 7:952–956
Picaut J, Delcroix T (1995) Equatorial wave sequence associated with warm pool displacements during the 1986–1989 El Niño-La Niña. J Geophys Res 100:18393–18408
Qiu B, Chen S (2005) Eddy-induced heat transport in the subtropical North Pacific from Argo, TMI, and altimetry measurements. J Phys Oceanogr 35:458–473
Rasmussen EM, Carpenter TH (1982) Variations in tropical sea surface temperature and surface wind fields associated with the Southern Oscillation/El Niño. Mon Weather Rev 110:354–384
Roemmich D, Gilson J (2009) The 2004–2008 mean and annual cycle of temperature, salinity, and steric height in the global ocean from the Argo program. Prog Oceanogr 82:81–100
Schneider N, Barnett T, Latif M, Stockdale T (1996) Warm pool physics in a coupled GCM. J Clim 9:219–239
Song X, Yu L (2013) How much net surface heat flux should go into the Western Pacific Warm Pool? J Geophys Res Oceans 118:3569–3585
Stammer D (1998) On eddy characteristics, eddy transports, and mean flow properties. J Phys Oceanogr 28:727–739
Toole JM, Zhang HM, Caruso MJ (2004) Time-dependent internal energy budgets of the tropical warm water pools. J Clim 17:1398–1410
Trenberth KE, Branstator GW, Karoly D, Kumar A, Lau NC, Ropelewski C (1998) Progress during TOGA in understanding and modeling global teleconnections associated with tropical sea surface temperatures. J Geophys Res 103:14291–14324
Volkov DL, Lee T, Fu LL (2008) Eddy-induced meridional heat transport in the ocean. Geophys Res Lett 35:L20601
Walin G (1982) On the relation between sea-surface heat flow and thermal circulation in the ocean. Tellus 34:187–195
Wyrtik K (1985) Water displacement in the Pacific and the genesis of El Niño cycles. J Geophys Res 90:7129–7132
Yim BY, Noh Y, Qiu B, Yoon JH (2010) The vertical structure of eddy heat transport simulated by an eddy-resolving ogcm. J Phys Oceanogr 40:340–353
Yu L, Jin X, Weller RA (2008) Multidecade global flux datasets from the objectively analyzed air-sea fluxes (OAFlux) project: latent and sensible heat fluxes, ocean evaporation, and related surface meteorological variables, OAFlux Project Tech. Rep. OA-2008-01
Zhang QL, Weng XC, Cheng MH (2003) Variations of heat content field in the western Pacific warm pool area and their impact. Oceanologia et Limnologia Sinca 34:389–396
Acknowledgments
This work is supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (XDA11010103), the National Science Foundation of China (41525019, 41522601, 41521005), the State Oceanic Administration of China (GASI-IPOVAI-02), and the Open Project Program of the State Key Laboratory of Tropical Oceanography (grant LTOZZ1501). The OAFlux product was provided by the WHOI OAFlux Project (http://oaflux.whoi.edu/). The Argo product was provided by the International Argo Program (http://www.argo.ucsd.edu). The HYCOM product was obtained from the National Ocean Partnership Program (NOPP) (http://HYCOM.org). We would like to think Yan Li for providing HYCOM daily products.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Chi, J., Shi, P., Zhuang, W. et al. Heat budget of the western Pacific warm pool and the contribution of eddy heat transport diagnosed from HYCOM assimilation. J Oceanogr 73, 193–203 (2017). https://doi.org/10.1007/s10872-016-0396-7
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10872-016-0396-7