基于调制不稳定性的吕宋海峡内孤立波生成机理探讨     

王晶  孙美玲  张旭东  孙丽娜  孟俊敏 《海洋学报(英文版)》2015,34(7):38-43

The South China Sea (SCS) is a hot spot for oceanic internal solitary waves due to many factors, such as the complexity of the terrain environment. The internal solitary waves in the northern SCS mainl...  相似文献   

Vessels,risks, and rules: Planning for safe shipping in Bering Strait     

《Marine Policy》2015

Commercial vessel traffic through the Bering Strait is increasing. This region has high biological and cultural significance, to which commercial shipping poses several risks. For this environment, these risks include ship strikes of whales, noise disturbance, chronic pollution, and oil spills. Indigenous Chukchi, Iñupiaq, St. Lawrence Island Yupik, Siberian Yupik, and Yup’ik peoples may be affected by proximity between small hunting boats and large commercial vessels leading to swamping or collisions, through displacement of animals or impacts to food security from contaminants, and through loss of cultural heritage if archeological sites and other important places are disturbed by wakes or an increase in people spending time on shore. Several measures are available to govern shipping through the region, including shipping lanes, Areas to Be Avoided (ATBAs), speed restrictions, communications measures, reporting systems, emissions controls, oil spill prevention and preparedness and salvage, rescue tug capability, voyage and contingency planning, and improved charting. These measures can be implemented in various ways, unilaterally by the U.S. or Russia, bilaterally, or internationally through the International Maritime Organization (IMO). Regulatory measures can be established as voluntary measures or as mandatory measures. No single measure will address all risks, but the framework presented herein may serve as a means of identifying what needs to be done and evaluating whether the goal of safe shipping has been achieved.  相似文献   

强台风纳沙 (1117) 近地层风特性观测分析          下载免费PDF全文

王志春  植石群  丁凌云 《应用气象学报》2013,24(5):595-605

根据琼州海峡两岸2个梯度塔和1部车载风廓线雷达共同获取的强台风纳沙 (1117) 实测风速资料,分析强台风纳沙影响期间大风特性,发现以下观测事实和变化规律:位于台风移动路径右侧的测风站,其风向呈顺时针方向旋转,台风眼区经过的测风站,其最大风速接近35 m·s-1,且风向旋转超过180°,台风外围大风区经过的测风站其最大风速达到30 m·s-1,风向旋转73°;大风风切变过程可用对数函数和指数函数拟合,对数函数和指数函数对光滑下垫面的拟合效果更好,且对数函数拟合效果要略优于指数函数;阵风系数随风速增大而减小,但风速达到6级以后,阵风系数不随风速大小产生趋势变化,阵风系数与下垫面粗糙度有关,在粗糙下垫面上阵风系数会偏大;大风阵风系数随高度变化可用指数函数来描述,且对来自光滑下垫面的近地层大风阵风系数拟合效果更好。该观测个例的大风风切变指数与GB/T 18710—2002的推荐值存在差异——粗糙下垫面的大风风切变指数大于标准推荐值,而来自光滑下垫面的大风风切变指数则小于GB/T 18710—2002的推荐值。  相似文献   

Seasonal variation of the double diffusion processes at the Strait of Hormuz     

AZIZPOUR Jafar  CHEGINI Vahi  SIADATMOUSAVI Seyed Mostafa 《海洋学报(英文版)》2017,36(1):26-34

Profiles of salinity and temperature were measured in the strait of Hormuz (SH) during the winter of 2012, spring and summer of 2013. To investigate the double diffusion (DD) processes, Turner (TU) angle values are calculated in all the stations in the SH. Different TU angle values correspond to salt fingering (SF), diffusive convection (DC) and stable stratification. The distributions of the two forms of DD were plotted vertically along transects in the eastern, central and western part of the SH, and corresponding DD processes were described. The results show that both SF and DC occurred in most part of the study area. Two different water masses (the Indian Ocean surface water and the Persian Gulf water) were evident at the SH, and SF and DC were evident at the interface of two water masses. Due to evaporation, SF occurred in the surface layer of most Stations throughout the year. In the eastern part of the SH, occurrences of DC were more feasible in wintertime. SF was the main phenomenon at the end of hot season. For central part, SF occurred throughout the year in water column. In the western part, water column was stable in summer and DC happened in most part of water column in winter.  相似文献   

台湾海峡中、北部海域春、夏季水团分析   总被引：13，自引：2，他引：13  

翁学传  张启龙  颜廷壮  王从敏  梁红星 《海洋与湖沼》1992,23(3):235-244

本文依据1983,1984,1987,1988几年的有关资料,利用“对应分析法”对台湾海峡中、北部海域春、夏季(5—8月)的水团及有关问题进行了分析。结果表明:(1)5—8月间该海域存在两种水团分布类型,其中5月属冬季型,全海域存在浙闽沿岸水和海峡暖流水两个水团;6—8月属夏季型,全海域均为海峡暖流水盘踞,按温度不同,它又分为上层水和深层水两部分。(2)浙闽沿岸水具低温、低盐、高溶解氧特征,均一性较差,年际变异较大;海峡暖流水以高盐为主要特征,温、盐度和溶解氧分布较均匀,且诸特征相对稳定。(3)海峡东、西两侧均存在上升流现象,西侧的上升流出现于6—8月,中心在海潭岛附近;东侧的上升流7月见于澎湖群岛北方海区。(4)6—8月间,海峡暖流深层水(核心)主要沿海峡偏西一侧北上,而不是紧靠东侧径直向北。  相似文献