中国对虾池浮游生物与对虾养殖的关系   总被引：9，自引：1，他引：9       下载免费PDF全文

张岩  王崇明  麻次松  赵法箴 《海洋科学》1993,17(6):6-9

为了进一步探讨繁殖浮游生物对改善养虾池水质和提高生产效益和作用,我们于1990～1992年在山东省牟平县宁海镇养虾场进行了连续的观察和实验,现将实验结果报告如下: 1 材料和方法  相似文献   

世界大洋中的锋面   总被引：2，自引：0，他引：2  

蒲书箴 《海洋湖沼通报》1985,(1)

众所周知,挪威气象学家很早就提出了表征气团运动的锋面概念。这就是著名的“极锋学说”。他们通过对锋面移行的观察和预报,在天气学的历史上,成功地开创了预报天气的新纪元。与此相比,海洋学家对海洋锋面的研究不仅开始的晚,而且进展也慢。这多半是因为海洋观测比气象观测受更多条件的制约,所使用的海洋仪器,以及所必需的海洋调查,都需要更多投资的缘故。  相似文献   

Variability of the Continental Water Boundary near the Pryda Bay     

蒲书箴  董兆乾等 《海洋通报(英文版)》2002,4(1):1-10

Based on the data obtained during the 15th Antarctic Expedition of China between November 1998 and February 1999,the paper discusses the water masses distributed on both sides of the Continental Water Boundary(CWB) as well as the spacial variability of the physical characteristics of the central location,the frontal width,the frontal strength,the vertical depth,and the vertical thickness for CWB,The above results are compared with the results from the data obtained during the 9th Antarctic Expedition of China between December 1992 and February 1993,and the temporal variabiltiy of those characteristics is discussed.In addition,the inhomogeneity of the kinematic characteristics and the patterms of the dynamic heights for those water masses located on both sides of CWB are illustrated.As it is pointed out in the paper,the trough in the dynamic height field is identified with the frontal location of CWB and the oceanic current shear.Furthermore,the dynamic reason for the upwelling of the circumpolar deep water can be understood by the explanation described in the paper.  相似文献   

巴士海峡和南海东北部黑潮分支     

蒲书箴  于惠苓  蒋松年 《热带海洋学报》1992,(2)

本文根据多个航次声学多晋勒海流剖面议(ADCP)的资料并结合历史文献说明:确有黑潮分支经过巴士海峡进入南海东北部。其流向多为NW向,但强度有比较明显的时间变化。该分支进入南海后可能进一步分为两支:台湾西海岸附近的N向流和南海东北部的W向流;后者的强度也有明显的时间变化。测流结果还表明:南海东北部W向流的南侧可能存在着一个涡状结构,而其北面向岸一侧,则有偏E方向的流动。  相似文献   

赤道太平洋西部的上层环流     

蒲书箴  蒋松年 《热带海洋学报》1994,(1)

讨论了赤道太平洋西部的上层海洋环流、结果表明：（１）棉兰老涡气旋式环流随着深度的增加而减小。由于埃克曼抽吸作用，它是一个低盐冷涡；（２）对棉兰老岛—巴布亚新几内亚岛之间穿越流的观测表明：该断而北部（５°—６°Ｎ）的Ｓ向流是棉兰老海流的Ｓ向延伸；Ｗ向的巴布亚新几内亚沿岸潜流可达该断而的东南部门（２°Ｎ一２°Ｓ）；北赤道逆流则在两者之间沿表层的盐度锋作Ｅ向流动。据此，赤道太平洋西部次表层盐度分布状况可得到圆满解释。关键词：  相似文献   

漂浮式防波堤消波在水库防汛中应用的探讨     

李陆平  蒲书箴 《海岸工程》1995,14(2):9-13

基于青岛地区水库资料，探讨风浪对水库防汛的影响，指出风浪对水库大坝的破坏及在坝体斜坡上，由于风浪破碎所致的平均水位升高和波浪爬高是威胁水库大坝安全的主要因素，风浪的作用降低了水库的蓄水能力和防洪标准，强调在库区，采用消波技术，合理运用漂浮式防波堤消波，消除风浪的影响是保障大坝安全，提高现有水为蓄水能力和防洪标准的科学而有效的方法，提出了水库漂浮式防波堤消波试验研究方案和设计依据。  相似文献   

会议简讯——“热带海洋和全球大气” 科学计划会议在巴黎召开     

蒲书箴 《海洋科学进展》1984,(2)

一九八四年九月十七日至廿一日在巴黎教科文总部召开了热带海洋和全球大气(TOGA)科学计划会议.这次会议是由政府间海洋学委员会(IOC)、世界气象组织(WMO)、海洋研究科委(SCOR)和国际科联理事会(ICSU)联合举办的.据不完全统计,来自世界各地的三十多个国家和地区的代表,9个国际组织的代表,计180余人出席了会议.我国代表汪兆椿等三人以观察员身份出席了会议.会议的主要目的是交流迄今为止的TOGA观测和模式研究的进展和现状,以便在现有的基础上提出TOGA的实施计划.  相似文献   

全美地震损失减轻研究与进展综述     

赵力箴  崔秋文 《地震科技情报》1998,(6):9-25

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Features and spatial distribution of circumpolar deep water in the southern Indian Ocean and the effects of Antarctic circum polar current     

蒲书箴  董兆乾  于卫东  卢燕  项宝强 《极地研究(英文版)》2007,18(2):100-109

The data from the Southern Ocean observations of World Ocean Circulation Experiment(WOCE) are used for analysis and illustration of the features and spatial distributions of Circumpolar Deep Water(CDW) in the southern Indian Ocean.It is learnt from the comparison among the vertical distributions of temperature/salinity/oxygen along the 30°E,90°E and 145°E sections respectively that some different features of CDW and the fronts can be found at those longitudes,and those differences can be attributed to the zonal transoceanic flow and the merizonal movement in the Circumpolar Deep Water.In fact,the zonal transoceanic flow is the main dynamic factor for the water exchange between the Pacific Ocean and the Indian Ocean or between the Atlantic Ocean and the Indian Ocean,and for the effects on the spatial distributions of the physical properties in CDW.  相似文献   

Thermohaline structure inhomogeneity associated with polynia at the northern margin of Emery Ice-shelf     

蒲书箴  葛人峰  董兆乾  于卫东  史久新  项宝强 《极地研究(英文版)》2007,18(1):18-26

Based on the hydrographic data in austral summer during the 22nd Antarctic Expedition of China(2005/2006),some features can be found about the northern margin of Emery ice shelf as follows.The heat content in the surface layer(0-50 m) at the eastern end and the western end of the ice-shelf margin is much higher than that at the middle.The upper mixing-layer depth and the seasonal thermocline depth at the middle of the ice-shelf northern margin are much shallower than those at the both ends.However there is much less difference between the middle and the ends in the bottom layer.The remote sensing photos show that the inhomogeneity in the surface-layer water is closely related to the spatial distribution of the floes and polynia in the area.  相似文献