| QIAO Lulu,WANG Xiaohua,WANG Yongzhi,WU Dexing,BAO Xianwen,MU Lin. 2011. Winter heat budget in the Huanghai Sea and the effect from Huanghai Warm Current (Yellow Sea Warm Current). Acta Oceanologica Sinica, (5):56－63 |
| Winter heat budget in the Huanghai Sea and the effect from Huanghai Warm Current (Yellow Sea Warm Current) |
| Winter heat budget in the Huanghai Sea and the effect from Huanghai Warm Current (Yellow Sea Warm Current) |
| Received:January 04, 2011 Revised:June 14, 2011 |
| DOI：10.1007/s13131-011-0147-y |
| Key words:heat budget Huanghai Sea and Bohai Sea surface heat flux Huanghai Warm Current (Yellow Sea Warm Current) |
| 中文关键词: heat budget Huanghai Sea and Bohai Sea surface heat flux Huanghai Warm Current (Yellow Sea Warm Current) |
| 基金项目:The National Natural Science Foundation Project "Sedimentary dynamic mechanism of the Huanghai Warm Current" of China under contract No.40906025; the State Basic Research Program of China under contract No. 2010CB428704; the National Natural Science Foundation of China "The process and mechanism of the increasing of surface temperature in the past 30 years in the adjacent seas of China" under contract No. 40930844; the Formation and development of the muddy deposition in the central southern Huanghai Sea, and its relation with climate and environmental change of Ocean University of China under contract No.41030856; the Scientific Research Fund of the Second Institute of Oceanography, State Oceanic Administration of China under contract No. JT1007; the Public Science and Technology Research Funds Projects of Ocean under contract Nos 200905001 and 201005019; the National Natural Science Foundation of China under contract No.41006002. |
| Author Name | Affiliation | E-mail | | QIAO Lulu | Key Laboratory of Seafloor Science and Exploration Technology, Ocean University of China, Qingdao 266100, China
Key Laboratory of Physical Oceanography, Ministry of Education, Ocean University of China, Qingdao 266100, China
School of Physical, Environmental and Mathematical Sciences, University of New South Wales at Australian Defence Force Academy, Canberra, Australia | qiaolulu126@sina.com | | WANG Xiaohua | School of Physical, Environmental and Mathematical Sciences, University of New South Wales at Australian Defence Force Academy, Canberra, Australia
State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute Oceanography, State Oceanic Administratim, Hangzhou 310012, China | | | WANG Yongzhi | The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China | | | WU Dexing | Key Laboratory of Physical Oceanography, Ministry of Education, Ocean University of China, Qingdao 266100, China | | | BAO Xianwen | Key Laboratory of Physical Oceanography, Ministry of Education, Ocean University of China, Qingdao 266100, China | | | MU Lin | National Marine Data and Information Service, State Oceanic Administration, Tianjin 300171, China | |
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| Abstract: |
| Four sources of surface heat flux (SHF) and the satellite remote sensing sea surface temperature (SST) data are combined to investigate the heat budget closure of the Huanghai Sea (HS) in winter. It is found that heat loss occurs all over the HS during winter and the area averaged heat content change decreases with a rate of -106 W/m2. Comparing with the area averaged SHF of -150 W/m-2 from the four SHF data sets, it can be concluded that the SHF plays a dominant role in the HS heat budget during winter. In contrast, the heat advection transported by the Huanghai Warm Current (Yellow Sea Warm Current, HWC) accounted for up to 29% of the HS heat content change. Close correlation, especially in February, between the storm events and the SST increase demonstrates that the HWC behaves strongly as a wind-driven compensation current. |
| 中文摘要: |
| Four sources of surface heat flux (SHF) and the satellite remote sensing sea surface temperature (SST) data are combined to investigate the heat budget closure of the Huanghai Sea (HS) in winter. It is found that heat loss occurs all over the HS during winter and the area averaged heat content change decreases with a rate of -106 W/m2. Comparing with the area averaged SHF of -150 W/m-2 from the four SHF data sets, it can be concluded that the SHF plays a dominant role in the HS heat budget during winter. In contrast, the heat advection transported by the Huanghai Warm Current (Yellow Sea Warm Current, HWC) accounted for up to 29% of the HS heat content change. Close correlation, especially in February, between the storm events and the SST increase demonstrates that the HWC behaves strongly as a wind-driven compensation current. |
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