| 410 | 57 | 40 |
| 下载次数 | 被引频次 | 阅读次数 |
<正> 本调查于1981年6月至1982年4月按季度共进行四次,调查海区在23°45′—35°N,122°30′—128°30E的范围内。这一研究区域正处于黑潮、台湾暖流、对马暧流、黄海沿岸流、东海沿岸流、长江冲淡水以及黄海冷水团的综合作用区域,水文条件十分复杂。在研究地理环境及环流系统时,不能仅限于调查海域范围内,需要扩展到整个黄东海区,因此将引入其它文献的有关资料和结论,并结合调查资料的分析,对若干问题提出初步见解。
Abstract：A survey of geographical environment in the Huanghai Sea and East China Sea is simply introduced. We'll emphatically analyse the circulation systems in this investigated area. Some Preliminary opinions and conclusions were obtained as follows;The forward mixed water of Taiwan warm Current in summer may pass through the Changjiang River Diluted Water from the bottom layer to influence the nearshore area of Northern Jiangsu to the north of 32*N. The water in the west side of Duima Warm Current is a mixed water of East China Sea and the water in its east side is a branch water coming from the Kuroshio. The current direction of Huanghai Sea Warm Current has a regularity with circulation movement for the seasons. The Huanghai Sea Bottom Cold Water Mass;belongs to a seasonal water mass and its waxing and waning are identical with the formation and elimination of thermocline. The Huanghai S.ea Bottom Cold water Mass are not independent each other every yearjand their general characters are even more outstanding than their different characters. The East China Sea Deep Cold Water can not well up with the aid of climbing to intrude into the inside of Huanghai Sea Bottom Cold water Mass in summer. In the southern area of Che judo Island, the ^inversion phenomena of temperature and solinity in median layer are formed by two reasons of the diffusion effect of Huanghai Sea Density Circulation and the climbing of East China Sea Deep Cold Water along the boundary of Huanghai Sea Bottom Cold Water Mass.In this paper, the relation between the marine environment and the central fishing grounds is analysed and some useful regular patterns are obtained.
[1] 孙湘平等,《中国沿岸海洋水文气象概况》,科学出版社,1981。
[2] 山东海洋学院海洋热学位研室,《海洋学》,第2章,第5节;第15章,第9节,1982。
[3] 中国科学院《中国自然地理》编委会,中国自然地理-海洋地理,1-224,科学出版社,1979。
[4] Nakao, T., Oceanic variablity in relation to fisheries in the East China Sea and Yellow Sea. Jour. of the Faculty of Marine Science and Technology Tokai University. Special Number: 199-367． 1977．
[5] 苏育嵩,划分变性水团边界的温盐点聚对照法与东海西部海区变性水团的分析,海洋学报2(1) :1-16． 1980．
[6] 苏育嵩等,聚类分析法在浅海水团分析中的应用及黄东海变性水团的分析,海洋与湖沼,14(1) :1-13,1983。
[7] 管秉贤,东海黑潮变异研究和若干结果,海洋与湖沼,10(4) ;290-306,1979。
[8] 毛汉礼,应用T-S关系定量地分析浅海水团的初步研究,海泽洋与湖沼,6(1) :1-22,1964。
[9] 郑执中等,黄海和东海浮游有孔虫生态的研究,海洋与湖沼,4(1-2) :60-86,1962。
[10] 井上尚夫,東海大陆棚上海底流动,海洋科学,7(1) :12-18,1974。
[11] 字田道隆,東支那海水温变化(其),東海黄海海况,1950,
[12] 近藤正人等,東海流况,海洋科学,7(1) :27-32,1975。
[13] 深濑茂。封话“東海”,海洋科学.7(1) :6-11,1975。
[14] 藤原伊佐美,東海海况,海洋科学,13(4) :264-270,1981。.
[15] Asaoka. O. and S. Morlyasn, On the circulation in the East China Sea and the Yellow Sea in winter(Preliminary Report), Oceanogr, Mag. 18(1-2) 3-81, 1966．
[16] Ninomiya, K. J. Meteor, Soc. Japan, 54: 334-337, 1976。
[17] 管秉贤,我国台湾及其附近海底地形对黑潮途径的影响,海洋科学集刊,14:1-22,1978。
[18] 翁学传等,台湾暖流水(团)夏季T-S特征和来源的初步分析,海洋科学集刊,21:113-132,1984。
[19] 苏育嵩,台湾海区海水环流及黄东海水平衡的初步探讨,太平洋西部渔业研究委员会第四次全体会议论文集,科学出版社,17-33,1963。
[20] 翁学传等,台湾暖流深层水变化特征分析,海洋与湖沼,14(4) :357-366,1983。
[21] 毛汉礼等,南黄海和东海北部(28-37) 夏季的水文特征以及海水类型(水系)的初步分析,海洋科学集刊,01:1-77,1964。
[22] 田峙美,東支那海及对马海峡渔业海洋学,西海区水产研究所研究报告,13:1-12,1957。
[23] 佐原勉等,東海水系分布,海空,54(4) :135-148,1979。
[24] Lim,D.B.J.Oceanogr.Soc.Korea,6:85-91,1971。
[25] 袁耀初等,东中国海陆架环流的单层模式;海洋学报,4(1) :1-11,1982。
[26] 毛汉礼,长江冲淡水及其混合问题的初步控讨,海洋与湖沼,5(3) ;183-205,1963。
[27] 乐肯堂,长江冲淡水路径问题的初步研究(Ⅰ)模式,海洋与湖沼,15(2) :157-166,1984。
[28] 浦永修,夏季长江冲淡水扩展机制的初析,东海海洋,1:43-51,1983。
[29] 浦永修等,从径流、水位和海区盐度的变化看长江水的扩展,海洋通报,2(3) :1-6,1983。
[30] 顾玉荷,长江冲淡水转向原因的探讨,海洋与湖沼,16(5) :354-363,1985。
[31] 赫崇本等,黄海冷水团的形成及其性质的初步探讨,海洋与湖沼,2(1) :11-15,1959。
[32] 管秉贤,黄海冷水团的水温变化以及环流特征的初步分析,海洋与湖沼,5(4) :255-283,1963。
[33] 邱道立,应用聚类分析法划分黄海水团的初步分析,海洋学报6(3) :281-292,1984。
[34] 兰淑芳,东海北部陆架区底层冷水的初步分析,海洋科学集刊,21:75-85,1984。
[35] 胡敦欣等,东海北部一个气旋型涡旋的初步分析,科学通报,1:29-31,1980。
[36] Sawarh. T., On the sea surface temperature in the East China Sea for the years 1953-1972, The Oceanographical Magazine, 26(1) , 17-26． 1974。
[37] 袁业立,黄海冷水团环流,海洋与湖沼,10(3) :187-199,1979。
[38] 竹下克一,黑潮离岸变动,(3) ,黑潮开发利用调查研究成果查报告,334-335,1981。
[39] 喻祖祥等,长江口及济州岛附近海域变性水团的初步分析,山东海洋学院学报,14(3) :1-12． 1984。
基本信息:
DOI：10.16441/j.cnki.hdxb.1986.s1.003
引用信息:
[1]苏育嵩.黄东海地理环境概况、环流系统与中心渔场[J].山东海洋学院学报,1986(S1):12-27.DOI:10.16441/j.cnki.hdxb.1986.s1.003.
1986-12-31
1986-12-31