中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The seasonal variation of the North Pacific Meridional Overturning Circulation heat transport

文献类型:CNKI期刊论文

作者LIU Hongwei; ZHANG Qilong; PANG Chongguang; DUAN Yongliang; PXU Jianping
发表日期2019-03-15
出处Journal of Oceanology and Limnology
关键词meridional overturning circulation heat transport North Pacific seasonal variation
英文摘要Based on the 50-year Simple Ocean Data Assimilation(SODA) reanalysis data, we investigated the basic characteristics and seasonal changes of the meridional heat transport carried by the North Pacific Meridional Overturning Circulation. And we also examined the dynamical and thermodynamic mechanisms responsible for these heat transport variability at the seasonal time scale. Among four cells, the tropical cell(TC) is strongest with a northward heat transport(NHT) of(1.75±0.30) PW(1 PW=1.0×10 15 W) and a southward heat transport(SHT) of(-1.69±0.55) PW, the subtropical cell(STC) is second with a NHT of(0.71±0.65) PW and SHT of(-0.63±0.53) PW, the deep tropical cell(DTC) is third with a NHT of(0.18±0.03) PW and SHT of(-0.18±0.11) PW, while the subpolar cell(SPC) is weakest with a NHT of(0.09±0.05) PW and SHT of(-0.07±0.09) PW. These four cells all have dif ferent seasonal changes in their NHT and SHT. Of all, the TC has stronger change in its SHT than in its NHT, so do both the DTC and SPC,but the seasonal change in the STC SHT is weaker than that in its NHT. Therefore, their dynamical and thermodynamic mechanisms are dif ferent each other. The local zonal wind stress and net surface heat flux are mainly responsible for the seasonal changes in the TC and STC NHTs and SPC SHT, while the local thermocline circulations and sea temperature are primarily responsible for the seasonal changes of the TC,STC and DTC SHTs and SPC NHT.
文献子类CNKI期刊论文
资助机构Supported by the National Natural Science Foundation of China(Nos.41406012,41576060) ; the Open Fund of State Key Laboratory of Satellite Ocean Environment Dynamics(Second Institute of Oceanography)(No.SOED1613) ; the Open Fund of Key Laboratory of Global Change and Marine-Atmospheric Chemistry,State Oceanic Administration,China(No.GCMAC1501) ; the NSFC-Shandong Joint Fund for Marine Science Research Centers(No.U1406401)
v.37期:02页:51-61
语种英文;
分类号P731.27;P732.6
ISSN号2096-5508
源URL[http://ir.qdio.ac.cn/handle/337002/188613]  
专题中国科学院海洋研究所
作者单位1.KeyLaboratoryofOceanCirculationandWaves,InstituteofOceanology,ChineseAcademyofSciencesandQingdaoNationalLaboratoryforMarineScienceandTechnology
2.StateKeyLaboratoryofSatelliteOceanEnvironmentDynamics,MNR
3.CenterforOceanMega-Science,ChineseAcademyofSciences
4.CenterforOceanandClimateResearch,FirstInstituteofOceanography,MNR
5.LaboratoryforRegionalOceanographyandNumericalModeling,QingdaoNationalLaboratoryforMarineScienceandTechnology
推荐引用方式
GB/T 7714
LIU Hongwei,ZHANG Qilong,PANG Chongguang,et al. The seasonal variation of the North Pacific Meridional Overturning Circulation heat transport. 2019.

入库方式: OAI收割

来源:海洋研究所

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