| MODEL OF UPPER OCEANIC CIRCULATIONS IN THE SOUTH CHINA SEA DURING NORTHEAST MONSOON |
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| 引用本文： | 王东晓,秦曾灏,李永平. MODEL OF UPPER OCEANIC CIRCULATIONS IN THE SOUTH CHINA SEA DURING NORTHEAST MONSOON[J]. 中国海洋湖沼学报, 1997, 15(3): 242-251. DOI: 10.1007/BF02850880 |
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| 作者姓名： | 王东晓 秦曾灏 李永平 |
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| 作者单位： | WANG Dong-xiao(LASG Institute of Atmospheric Physics Academia Sinica Beijing，10082)QIN Zeng-hao; LI Yong-ping(Shanghai Institute of Typhoon，Shanghai，200030) |
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| 摘 要： | MODUrnONTheS0uthChinaSea(SCS)isabophalrnarginalbasinwhereEastAsiamonsoonsprevail.0bviousadjustInentSoftheupperocanoccurduetOthealtematingsurnxneandwintermonsoons.ThemostboohantaspchoflargeanlecurmtSintheSesaretheupperoonnicresponsetothemonsoons(Dale,l956).MostpreviousmrehesfocusedondiagnostiesandmodelingofsuffocecurmtS.Wwti(l96l)plotalsurfacentsbasedonshipdriflsintheNAGAReportNo.2anddescritaltheperiodicallysdri-annualreversingofwindsandrtinthisarea.Xuetal.(l982)calculatalthedy-naAn…
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| 收稿时间： | 1995-05-03 |
| 修稿时间： | 1996-10-18 |
Model of upper oceanic circulations in the South China Sea during northeast monsoon |
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| Wang Dong-xiao,Qin Zeng-hao,Li Yong-ping. Model of upper oceanic circulations in the South China Sea during northeast monsoon[J]. Chinese Journal of Oceanology and Limnology, 1997, 15(3): 242-251. DOI: 10.1007/BF02850880 |
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| Authors: | Wang Dong-xiao Qin Zeng-hao Li Yong-ping |
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| Affiliation: | (1) LASG, Institute of Atmospheric Physics, Academia Sinica, 100082 Beijing;(2) Shanghai Institute of Typhoon, 200030 Shanghai |
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| Abstract: | The large-scale upper oceanic circulation in the South China Sea (SCS) during the northeast monsoon was investigited using a 2 1/2-layer model inrolving entrainment and detraininent at the interface between the upper mixed layer and the seasonal thermocline. The model allows heat fluxes at the surface and at the interfaee with a reaxation scheme, the temperatures of the two active layers can vary. The model basin is idenical to the SCS lateral boundary with bottom topography of 50 m or more and is regarded as an enclosed basin by neglecting inflow and outflow through the straits, and is forced by the climetological wind stna of 12 calendar months. It was found tha the upper oceanic currents in winter were mainly wind-driven. Most aspects of streams reported by observations were simulated with eddyresolving. |
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| Keywords: | upper oceanic circulation South China Sea 2 1/2-layer model northeast monsoon |
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