广西科学
廣西科學
엄서과학
GUANGXI SCIENCES
2014年
4期
313-324
,共12页
北部湾%琼州海峡%环流%上升流
北部灣%瓊州海峽%環流%上升流
북부만%경주해협%배류%상승류
Beibu Gulf%Qiongzhou Strait%circulation%upwelling
针对北部湾环流的季节变化和琼州海峡水体输送的传统观念,根据近20多年的海流、底质、浮游生物的实地调查资料,对众多的研究结果进行对比和评述。认为:从平均态来说,琼州海峡水体输送全年都是从东向西,冬季多于夏季;冬季北部湾环流是气旋式,夏季,北部湾北部环流是气旋式,南部是反气旋式,其中分界线大致在19°30′N处。北部湾存在多处上升流区域,不计越南沿岸,仅靠近我国大陆,就有广西沿海铁山港和北海的上升流区;海南省西部,从八所-莺歌海的上升流区;海南省南部上升流区。虽然,北部湾环流研究已取得长足进步,但是,还存在许多不足之处,如潮汐余流的研究:未能在充分考虑水体边界、实际风场、真实地形、潮汐余流、密度流等诸多要素情况下,计算出北部湾真实环流。
針對北部灣環流的季節變化和瓊州海峽水體輸送的傳統觀唸,根據近20多年的海流、底質、浮遊生物的實地調查資料,對衆多的研究結果進行對比和評述。認為:從平均態來說,瓊州海峽水體輸送全年都是從東嚮西,鼕季多于夏季;鼕季北部灣環流是氣鏇式,夏季,北部灣北部環流是氣鏇式,南部是反氣鏇式,其中分界線大緻在19°30′N處。北部灣存在多處上升流區域,不計越南沿岸,僅靠近我國大陸,就有廣西沿海鐵山港和北海的上升流區;海南省西部,從八所-鶯歌海的上升流區;海南省南部上升流區。雖然,北部灣環流研究已取得長足進步,但是,還存在許多不足之處,如潮汐餘流的研究:未能在充分攷慮水體邊界、實際風場、真實地形、潮汐餘流、密度流等諸多要素情況下,計算齣北部灣真實環流。
침대북부만배류적계절변화화경주해협수체수송적전통관념,근거근20다년적해류、저질、부유생물적실지조사자료,대음다적연구결과진행대비화평술。인위:종평균태래설,경주해협수체수송전년도시종동향서,동계다우하계;동계북부만배류시기선식,하계,북부만북부배류시기선식,남부시반기선식,기중분계선대치재19°30′N처。북부만존재다처상승류구역,불계월남연안,부고근아국대륙,취유엄서연해철산항화북해적상승류구;해남성서부,종팔소-앵가해적상승류구;해남성남부상승류구。수연,북부만배류연구이취득장족진보,단시,환존재허다불족지처,여조석여류적연구:미능재충분고필수체변계、실제풍장、진실지형、조석여류、밀도류등제다요소정황하,계산출북부만진실배류。
According to nearly 20 years of field survey data of marine currents,bottom sub-strate,plankton,this paper compared numerous research results and commented on them a-gainst the traditional concept of the seasonal variation of circulation in Beibu Gulf and Qiong-zhou Strait water conveying.It points out that from the mean state,Qiongzhou Strait water conveying goes from east to west all year round,and is more in winter than in summer.Beibu Gulf circulation is cyclonic in winter;in summer,north circulation in Beibu Gulf is cyclonic, while south one is anticyclonic,and the demarcation line is approximately at 19°30′N.There are many upwelling regions in Tonkin Gulf,regardless of the coast of Vietnam.Only near main-land China,there are Guangxi coastal upwelling regions near Tieshan Port and Beihai,the up-welling region from Basuo to Yinggehai in the west of Hainan Province,and the southern Hainan upwelling area.Although great progress has been achieved on circulation study,howev-er,there are still many deficiencies,for example,there are still lack of the evaluation of the tid-al residual current,and the calculation of real circulation in Beibu Gulf in the cases of fully con-sidering factors such as the water boundary,the actual wind field,the real terrain,the tidal re-sidual current and density current.