Observations of the countercurrent on the inshore side of the Kuroshio northeast of Taiwan   总被引：4，自引：0，他引：4  

Wen-Ssn Chuang  Hsien-Wen Li  T. Y. Tang  Chong-Kung Wu 《Journal of Oceanography》1993,49(5):581-592

Intensive current measurements in the area northeast of Taiwan indicate subsurface, southwestward flow existed between the inshore edge of the Kuroshio and the East China Sea continental slope. At 70 km away from Taiwan, this countercurrent has a mean speed about 30 cm s^–1 at mid-depth. Closer to Taiwan, the flow turns along with the topography, and subjects to sidewall and bottom friction. Both the magnitude and the vertical shear of this countercurrent are comparable with that inferred from hydrographic survey. The wind field features short-period (a few days) fluctuations associated with the cold front passages, however, this is not reflected on the current records. It appears that the countercurrent is fairly steady. Together with similar reversing flow found at places much further to the north, the overall pattern seems to be a general quasi-steady feature along most part of the shelf edge of the East China Sea.  相似文献   

Further evidence for non-reemergence of winter SST anomalies in the North Pacific eastern subtropical mode water area     

Shusaku Sugimoto  Kimio Hanawa 《Journal of Oceanography》2007,63(4):625-635

Following our previous study (Sugimoto and Hanawa, 2005b), we further investigate the reason why reemergence of winter sea surface temperature anomalies does not occur in the North Pacific eastern subtropical mode water (NPESTMW) area, despite its occurrence in the North Pacific subtropical mode water and North Pacific central mode water areas. We use vertical temperature and salinity profiles of the World Ocean Circulation Experiment Hydrographic Program and Argo floats with high vertical and temporal resolution, together with heat flux data through the sea surface. We point out first that one of the causes for non-occurrence of reemergence is that the thickness of NPESTMW is very thin. In addition to this basic cause, two major reasons are found: a vigorous mixing in the lower portion of NPESTMW and less heat input from the atmosphere in the warming season. Since, in the lower portion of NPESTMW and deeper, the stratification is favorable for salt-finger type convection to occur compared with the other mode water areas, vigorous mixing takes place. This is confirmed by both a large Turner Angle there and the existence of staircase structures in vertical temperature and salinity profiles. From the viewpoint of heat input, the NPESTMW area gradually gains heat in the warming season compared with other mode water areas. As a result, NPESTMW cannot be capped so quickly by the shallow summer mixed layer, and water properties of NPESTMW are to be gradually modified, even in the upper portion.  相似文献   

Geomorphological evidence for upslope canyon-forming processes on the northern KwaZulu-Natal shelf,SW Indian Ocean,South Africa     

Andrew N. Green  John A. Goff  Ron Uken 《Geo-Marine Letters》2007,27(6):399-409

A geomorphological and statistical analysis of slope canyons from the northern KwaZulu-Natal continental margin is documented and compared with submarine canyons from the Atlantic margin of the USA. The northern KwaZulu-Natal margin is characterized by increasing upslope relief, concave slope-gradient profiles and features related to upslope growth of the canyon forms. Discounting slope-gradient profile, this morphology is strikingly similar to canyon systems of the New Jersey slope. Several phases of canyon incision indicate that downslope erosion is also an important factor in the evolution of the northern KwaZulu-Natal canyon systems. Despite the strong similarities between the northern KwaZulu-Natal and New Jersey slope-canyon systems, key differences are evident: (1) the concavity of the northern KwaZulu-Natal slope, contrasting with the ∼linear New Jersey slope; (2) the relative isolation of the northern KwaZulu-Natal canyons, rather than the dense clustering of the New Jersey canyons; and (3) the absence of strongly shelf-breaching canyons along the northern KwaZulu-Natal margin. In comparison with the New Jersey margin, we surmise a more youthful stage of canyon evolution, a result of either the canyons themselves being younger or the formative processes being less active. Less complicated patterns of erosion resulting from reduced sediment availability have developed in northern KwaZulu-Natal. The reduction in slope concavity on the New Jersey margin may be the result of grading of the upper slope by intensive headward erosion, a process more subdued—or less evident—on the KwaZulu-Natal margin.  相似文献   

Study on genetic diversity of cultivated populations in 4 species of shrimps   总被引：2，自引：0，他引：2  

Li Zhongbao  Wu Zhongqing 《海洋学报(英文版)》2003,22(1):97-101

Genetic diversity of cultivated populations was investigated using assay of vertical slabpolyacrylamide gel electrophoresis in 4 species of shrimps, which were Penaeus japonicus, Penaeus monodon , Penaeus vannamei and Metapenaeus ensis, The results showed that the mean number of alle-les per locus (A) is 1.3±0.2, 1.3±0.1, 1.3±0.1 and 1.3 ±0.1 respectively; the percentage of polymorphic loci (P0.95) is 12.5, 6.7, 20 and 23.5 respectively; the expected heterozygosity (He) is 0.042±0.034,0.042±0.031, 0.094±0.042 and 0.097±0.047 respectively; and the observed heterozygosity (H0)is 0.029±0.024, 0.028±0.023,0.154±0.082 and 0.150±0.084 respectively. The difference of genetic diversity is obvious in 4 species of shrimps. The degree of genetic diversity is M. ensis > P. vannamei > P. japonicus > P. monodon. In short, the lower level of genetic diversity is estimated in 4 species of shrimps.  相似文献   

加州鲈鱼的繁殖习性,早期胚胎发育以及孵化与水温的关系   总被引：2，自引：0，他引：2  

吴庆龙 《海洋湖沼通报》1993,(1):64-70

作者对加州鲈鱼繁殖习性及早期胚胎发育进行了阐述,对受精卵孵化与水温的关系进行了研究。结果表明:加州鲈鱼2龄即达性成熟,3—6月繁殖产卵,水温20℃—24℃时达产卵盛期;雄鱼具有筑巢护卵及护苗等生殖习性;水温17.4℃—19.5℃,平均18.3℃时,受精卵孵化时数为74小时25分钟;在实验温度范围内,孵化时数与水温负相关,而与有效积温正相关。有效积温与平均水温负相关。  相似文献   

中国东南沿海潮灾与防潮对策研究   总被引：2，自引：0，他引：2  

吴培木 《台湾海峡》1994,13(3):308-315

中国东南沿海是中风暴潮灾害的最严得岸段，本文针对闽，粤，海南三省台风暴潮灾害概况，防潮现状及其存在问题，提出防潮减灾的对策和见解，以祈提醒人们居安思危，防患未然。  相似文献   

Fluctuations of peak energy and peak frequency of local wavelet energy spectrum for wind waves     

Wu Kejianl  Lou Shunli 《海洋学报(英文版)》1997,16(4):429-439

Ｆｌｕｃｔｕａｔｉｏｎｓ　ｏｆ　ｐｅａｋ　ｅｎｅｒｇｙ　ａｎｄ　ｐｅａｋ　ｆｒｅｑｕｅｎｃｙ　ｏ　ｌｏｃａｌ　ｗａｖｅｌｅｔ　ｅｎｅｒｇｙ　ｓｐｅｃｔｒｕｍ　ｆｏｒ　ｗｉｎｄ　ｗａｖｅｓTXＦｌｕｃｔｕａｔｉｏｎｓｏｆｐｅａｋｅｎｅｒｇｙａｎｄｐｅａｋ...  相似文献   

青海钩虾配合饲料对罗非鱼两品系生长效果的研究     

武云飞  韩凤进  江涛  孔晓瑜 《中国海洋大学学报(自然科学版)》2003,33(2):199-205

研究青海钩虾对罗非鱼两品系吉富罗非鱼和彩虹鲷生长的促进作用。实验用青海钩虾与面粉、麸皮和豆饼制成 5组 ( ～ )配合饲料及良种场原用饲料 ( 组 )饲育吉富罗非鱼和彩虹鲷 ,经2 5 d试验结果表明 :( 1)彩虹鲷增重效果以 组饲料最高 ,平均增重为 4 4 .9g,较大于 组的 4 3.1g;( 2 )所有钩虾饲料对彩虹鲷的增色效果都高于良种场的原用饲料 组 ,其中以饲料 组最高 ;( 3)饲料 I组饲育吉富罗非鱼平均增重为 4 4 g,高于 组的 4 0 .1g;( 4 )吉富罗非鱼和彩虹鲷比较则显示出吉富罗非鱼的增重率明显高于彩虹鲷而饵料系数又较低的结果。  相似文献   

海水中Cr（Ⅲ）的氧化作用     

吴国琳 《海洋技术学报》1994,13(3):47-51

本文以人工海水和天然海水为介质，研究了Ｃｒ（Ⅲ）被Ｈ２Ｏ２的氧化作用，结果表明，Ｃｒ（Ⅲ）的氧化速率为介质ｐＨ和温度的函数；海水中溶解有机质的存在也将影响Ｃｒ（Ⅲ）的氧化速率，随着海水中腐殖质浓度的增加其氧化速率呈现下降趋势。其原因可解释为腐殖质对Ｃｒ（Ⅲ）的配合作用和对Ｃｒ（Ⅵ）的还原－催化作用。  相似文献   

浙江近海大黄鱼 Pseudosciaena crocea( Richardson )的性成熟特性   总被引：2，自引：0，他引：2  

徐恭昭  吴鹤洲 《海洋科学集刊》1962,(2):50-58

鱼类性成熟的开始是鱼类生命周期中转入繁衍后代的一个重要阶段。同一世代的个体开始性成熟的年龄、大小,以及延续期限与速度,是种和种内种群对水域生活条件的适应属性之一。 研究鱼类性成熟过程的特点,不仅在解决鱼类种群数量的预测与控制问题中,对补充过程的了解具有重大的意义,而且也为制订合理的渔业经营管理措施提供必要的生物学依据。 本文主要在于探讨浙江近海大黄鱼种群的性成熟特点及其影响因子;其次,讨论该特点在这一种群数量上的意义;并对捕捞规格(法定许可捕捞的鱼体大小和年龄等生物学指标)问题提出初步意见。 在这项工作中,单才根、滕文法和蓝志满等同志曾协助搜集资料、耳石制片和计算工作。在资料的收集中,得到洞头公社和温州地方水产部同的大力支持;本文承张孝威教授热情指导,井承成庆泰副教授等提出宝贵意见,均此谨表谢忱。  相似文献