Heat Budget of the Upper Ocean in the South-Central Equatorial Pacific

被引:26
作者
Liu, Hailong [1 ]
Lin, Wuyin [2 ]
Zhang, Minghua [2 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Sci & Geophys Fluid Dynam, Beijing, Peoples R China
[2] SUNY Stony Brook, Inst Terr & Planetary Atmospheres, Stony Brook, NY 11794 USA
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
AIR-SEA FLUXES; BULK PARAMETERIZATION; DOUBLE-ITCZ; WARM POOL; CLOUDS; CLIMATOLOGY; CIRCULATION; REANALYSIS; RADIATION; ICOADS;
D O I
10.1175/2009JCLI3135.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The double intertropical convergence zone (ITCZ) over the tropical Pacific, with a spurious band of maximum annual sea surface temperature (SST) south of the equator between 5 degrees S and 10 degrees S, is a chronic bias in coupled ocean-atmosphere models. This study focuses on a region of the double ITCZ in the central Pacific from 5 degrees S to 10 degrees S and 170 degrees E to 150 degrees W, where coupled models display the largest biases in precipitation, by deriving a best estimate of the mixed layer heat budget for the region. Seven global datasets of objectively analyzed surface energy fluxes and four ocean assimilation products are first compared and then evaluated against field measurements in adjacent regions. It was shown that the global datasets differ greatly in their net downward surface energy flux in this region, but they fall broadly into two categories: one with net downward heat flux of about 30 W m(-2) and the other around 10 W m (2). Measurements from the adjacent Manus and Nauru sites of the Atmospheric Radiation Measurement Program (ARM), the Tropical Atmosphere Ocean (TAO) buoys, and the Tropical Ocean and Global Atmosphere Coupled Ocean-Atmosphere Response Experiment (TOGA COARE) are then used to show that the smaller value is more realistic. An energy balance of the mixed layer is finally presented for the region as primarily between warming from surface heat flux of 7 W m(-2) and horizontal advective cooling in the zonal direction of about 5 W m(-2), with secondary contributions from meridional and vertical advections, heat storage, and subgrid-scale mixing. The 7 W m(-2) net surface heat flux consists of warming of 210 W m(-2) from solar radiation and cooling of 53, 141, and 8 W m(-2). respectively, from longwave radiation, latent heat flux, and sensible heat flux. These values provide an observational basis to further study the initial development of excessive precipitation in coupled climate models in the central Pacific.
引用
收藏
页码:1779 / 1792
页数:14
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