长江口深水航道治理一期工程实施对北槽拦门沙的影响   总被引：8，自引：3，他引：8  

刘杰乐嘉海  胡志峰丁光明 《海洋工程》2003,21(2):58-64

介绍了长江口拦门沙发育及其特点和北槽航道拦门沙形成机理，利用长江口深水航道治理一期工程实施后的地形资料分析治理工程对北槽航道拦门沙影响。结果表明：治理工程建成后，增加了主槽流速，减少了航道回淤，打通北槽航道拦门沙，增加了航道水深，治理工程效果明显。  相似文献   

南海鱼类生物多样性与区系分布   总被引：7，自引：0，他引：7  

马彩华  游奎  李凤岐  张美昭 《中国海洋大学学报(自然科学版)》2006,36(4):665-670

分析了南海鱼类生物多样性与区系分布的生态地理条件,鱼类生物多样性特征。校核整理了南海鱼类2 321种,分属于六鳃鲨等35目,以鲈形目占绝对优势(979种),并以珊瑚礁栖,典型暖水种的隆头鱼科为优势科(占117种),而蝴蝶鱼和石斑鱼分别达到34种、31种,列为优势属,从而构成南海富有潜势的群落结构。文中进一步论述了南海鱼类区系属于以印度-西太平洋为主体的区系特征。  相似文献   

南海北部海区水团的判别分析   总被引：1，自引：0，他引：1  

李凤岐  苏育嵩  范立群 《中国海洋大学学报(自然科学版)》1989,(Z1)

将判别分析应用于南海北部海区的水团分析。划分为八个水团:沿岸冲淡水团(F),近岸混合水团(M),暖表层水团(WS),表层水团(S),表—次层混合水团(SU),次层水团(U),次—中层混合水团(UI)和中层水团(I)。给出了各水团在四季代表月的Bayes多组判别的系数和参数。用资料检验判别的成效.冬季和春季可达95.90％以上,夏季为94.80％,秋季是全年最低值,为92.72％。讨论了造成错判的原因,并与Fisher判别作了比较。当测值维数较低时,建议选用Bayes判别。对八个水团以及各水团两两之间差异的显著性进行了检验,证实在每个季节中各水团之间的差异,都在高度置信水平(α=0.01)上具有显著性。因而,划分为八个水团是有实际意义的,其判别式的系数和参数,可用于实际的判别和预报。  相似文献   

渤海海域的上第三系油气研究   总被引：4，自引：0，他引：4  

肖国林  陈建文 《海洋地质前沿》2003,19(8):1-6

综述了渤海湾盆地沉积与构造活动在时间与空间上的迁移与演化、烃源岩与储盖层的空间分布规律，结合盆地内的勘探现状分析了渤海湾海域上第三系的油气远景。认为盆地内凸起、低凸起以上第三系为主体，伴有东营组和前第三系油气藏的复式油气聚集带是目前渤海油气勘探最现实的有利目标。  相似文献   

杰氏风暴潮预报方法在珠海及粤西海域的应用     

魏晓宇  窦金来  黄根华  周求赞  陈强  王欣睿 《台湾海峡》2007,26(2):197-203

本文通过杰氏风暴潮预报方法对历史上给珠海和粤西海域造成较大影响的台风增水事件进行后报试验,并通过统计分析方法对原有的预报公式进行订正,总结出适合珠海及粤西海域的风暴潮预报公式.利用5a的时间对珠海及粤西海域的台风增水进行试报,结果表明预报准确率分别达95.0%和87.6%,尤其对一些增水较大、影响较严重的台风增水预报相对更加准确,预报准确率均达90.0%以上.这说明订正后的公式对珠海及粤西海域的风暴潮预报能得到较好的预报效果.  相似文献   

Estimating the geostrophic velocity obtained by HF radar observations in the upstream area of the Kuroshio     

Ryoko Tokeshi  Kaoru Ichikawa  Satoshi Fujii  Kenji Sato  Shoichiro Kojima 《Journal of Oceanography》2007,63(4):711-720

A method to extract geostrophic current in the daily mean HF radar data in the Kuroshio upstream region is established by comparison with geostrophic velocity determined from the along-track altimetry data. The estimated Ekman current in the HF velocity is 1.2% (1.5%) and 48° (38°)-clockwise rotated with respect to the daily mean wind in (outside) the Kuroshio. Furthermore, additional temporal smoothing is found necessary to remove residual ageostrophic currents such as the inertial oscillation. After removal of the ageostrophic components, the HF geostrophic velocity agrees well with that from the altimetry data with rms difference 0.14 (0.12) m/s in (outside) the Kuroshio.  相似文献   

两个同源地不同路径热带气旋的大尺度场对比分析     

舒锋敏  林良勋 《海洋预报》2007,24(4):102-108

本文利用NCEP/NCAR再分析格点资料,着重对8903号"BRENDA"和0601号"珍珠"两个同源地进入南海后不同路径的典型热带气旋的大尺度环境场进行对比分析。结果表明:西风槽的强弱和东移的快慢、西太平洋副高的形状变化和东退西进、冷空气的强弱和南下路径及热带气旋内部的不对称结构是造成二者移动路经差异的主要原因。另,印缅槽的变化也对其路径差异有一定的作用。  相似文献   

东营北部凸起带古冲沟储层分布规律研究     

张维冈  刘怀山 《中国海洋大学学报(自然科学版)》2002,32(4):603-607

在油田勘探与开发中 ,充分认识古冲沟油气藏的勘探与开发是十分重要和有意义的。本文利用东营北部凸起带的地质、钻井、航磁和地震等资料 ,对古冲沟在地震剖面上的特征和古冲沟储层预测方法等进行了研究与探讨  相似文献   

Responses of CO₂ in surface water in subtropical West Pacific to El Niño event     

Xing Runan  Ma Liming  Qiao Ran  Wang Zhanggui 《海洋学报(英文版)》2001,20(1):39-50

In order to investigate the relationships between the change of TCO2, △PCO2 and SST, current, upwelling and biological activities during El Nin(～)o event in the subtropical Pacific, the responses of TCO2 and △PCO2 in surface water in the subtropical Pacific during El Nin(～)o and La Nina have been simulated using a three-dimension carbon cycle model with biota pump. The results of numerical simulations show that TCO2 in sea water increases with reducing of SST during mature phase of El Nin(～)o in the subtropical West Pacific . At the same period , the Kuroshio in this region was weakened , the zonal currents were divergence , the upwelling carried the water with high concentrations of CO2 to the sea surface , so both of TCO2 and △PCO2 in surface water were increased . But TCO2 and △pCO2 were decreased during La Nina period. These simulated results confirmed the observations in 1982/1983 , 1986/1987 ,1991/1995 and 1997/1998 El Nin(～)o events .  相似文献   

Freshening of the Intermediate Waters in the Northern South China Sea over the PastSix Decades     

陈栩洋  王东晓  舒业强  成里京  范双双 《热带气象学报(英文版)》2024,30(1):42-50

The properties of salinity in the South China Sea (SCS), a significant marginal sea connecting the Pacific andIndian Oceans, are greatly influenced by the transport of fresh water flux between the two oceans. However, the long-termchanges in the intermediate water in the SCS have not been thoroughly studied due to limited data, particularly in relationto its thermodynamic variations. This study utilized reanalysis data products to identify a 60-year trend of freshening in theintermediate waters of the northern South China Sea (NSCS), accompanied by an expansion of low-salinity water. Thestudy also constructed salinity budget terms, including advection and entrainment processes, and conducted an analysis ofthe salinity budget to understand the impacts of external and internal dynamic processes on the freshening trend of theintermediate water in the NSCS. The analysis revealed that the freshening in the northwest Pacific Ocean and theintensification of intrusion through the Luzon Strait at intermediate levels are the primary drivers of the salinity changes inthe NSCS. Additionally, a weakened trend in the intensity of vertical entrainment also contributes to the freshening in theNSCS. This study offers new insights into the understanding of regional deep sea changes in response to variations in boththermodynamics and oceanic dynamic processes.  相似文献