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1.
本文收集了1960~1990年间的水文气象资料进行累年统计,并参考有关航海资料和海洋图集,详细地对大隅海峡进行了分析研究,阐明了该海峡气候及水文特征的变化规律。  相似文献   

2.
混合坐标模式HYCOM模拟COADS强迫下的南海平均环流   总被引:1,自引:0,他引:1  
采用混合坐标模式(HYCOM)模拟南海环流,同时利用海表温度卫星资料和吕宋海峡Sb-ADCP观测海流数据来评估模式结果.地形敏感性实验表明,吕宋海峡地形数据对模拟黑潮入侵方式影响较大,在地形误差较大的情况下,模拟的黑潮可能以反气旋流套方式入侵.和Pathfinder海表温度卫星资料比较,模式输出的月平均温度在海盆区域误差较小.ERA-15资料强迫所模拟的吕宋海峡上层环流和Sb-ADCP观测一致,而COADS结果低估了吕宋海峡的体积输送.  相似文献   

3.
福建海坛海峡是闽江和浙闽沿岸流南下物质向兴化湾及福建中南部沿海输运的重要通道。本文运用GIS手段对海坛海峡近50a来的地形资料进行了分析研究, 研究结果表明: 1964—1975年, 闽江流域性洪水导致海坛海峡表现为较强的淤积; 1975—1990年受闽江上游水土保持和大量水库建设的影响, 海峡经历了较强的冲刷过程, 此后冲刷速率逐渐降低, 以轻微冲刷为主; 2007年以后由于大规模人工采砂影响, 海坛海峡北部出现大范围侵蚀。2007年以前, 闽江来沙量是海坛海峡地貌演变的主要控制因素, 其流域洪水、采砂和水库修建等都对海峡内的地貌演变产生直接影响; 而2007年以后, 海峡内大范围的人为采砂活动和围填海工程逐渐成为影响其地貌演变的主要因素。  相似文献   

4.
利用1977-1991年日本“KuroshioExploitationandUtilizationResearch”(KER)资料和日本气象厅海洋观测资料计算吐噶喇海峡的黑潮流速和流量。结果表明,海峡处黑潮主轴的平均核心流速为92.0cm/s,平均流量为周.1×106m3/s;揭示了吐噶喇海峡黑潮流速的多核结构和多股流动的突出特征。探讨了海峡中流量分布状况和季节变化。  相似文献   

5.
吕宋海峡两侧中尺度涡统计   总被引:4,自引:0,他引:4  
利用1993-2000年间的T/P卫星高度计轨道资料的时间序列和MODAS同化产品中的卫星高度计最优插值资料对南海东北部海区中尺度涡旋进行动态追踪。按照给定的标准从2种资料中提取了涡旋信息并对其特征量进行统计分析。结果表明,南海东北部海区中尺度涡旋十分活跃,平均每年6个,其中暖涡4个,尺度一般为200~250 km,平均地转流速为44 cm/s;冷涡每年平均2个,尺度一般为150~200 km,平均地转流速为-37 cm/s。吕宋海峡两侧涡旋的比较分析表明,南海东北部海区仍属于西北太平洋副热带海区的涡旋带,冷、暖涡旋处于不断的形成—西移—消散过程中。南海东北部中尺度冷涡大多是南海内部产生的,而暖涡与吕宋海峡外侧暖涡有一定的联系又具有相对的独立性。分析认为西北太平洋的西行暖涡在到达吕宋海峡时,受到黑潮东翼东向下倾的等密度面的抑制和岛链的阻碍,涡旋停滞于吕宋海峡外侧并逐渐消弱,被阻挡于吕宋海峡东侧涡旋释放的能量,形成一支横穿吕宋海峡(同时横穿过黑潮)的高速急流,把能量传递给吕宋海峡西侧的涡旋,使其得到强化,这是吕宋海峡两侧涡旋联系的一种重要机制。  相似文献   

6.
利用我国第九次南极考察队获得的德雷克海峡地区水温资料,并结合国外锚碇浮标和测流资料,分析和研究了德雷克海峡绕极流和锋面的时间变化和空间变化.研究表明,德雷克海峡绕极流的流速共有3个强流区,就德雷克海峡上层海流的空间变化而言,以亚南极锋附近的海流最强,流向和流速也最稳定少变.德雷克海峡深层海流的空间分布特点与上层海流的空间分布特点不同,深层流速明显减弱,且稳定性差.德雷克海峡绕极流有着明显的时间变化,但是这种时间变化因地而异.极锋附近在冬春季节是稳定的深层北向流,它与南半球高纬度的冬、春季节的Ventilation过程有着密切的关系,德雷克海峡上层水温的空间分布具有明显的锋面分布特征.水温在德雷克海峡的高纬度区更加稳定少变,而极锋附近深层海水温度随时间的变化最大.  相似文献   

7.
通过对Argos浮标资料的分析,针对黑潮能否在吕宋海峡入侵南海的问题进行了研究,结果表明:黑潮由吕宋海峡入侵南海主要发生在秋、冬两季,春、夏季基本上不发生。而入侵主要是以流的形式传入,秋季少量的入侵水会有分支沿台湾海峡北上,冬季黑潮自吕宋海峡入侵南海后向西进入南海腹部。并对其季节变化原因作了初步讨论,该区域风应力和黑潮流量的季节性变化可能是重要原因。  相似文献   

8.
利用1990—2014年的ICOADS观测资料,从空间分布、季节变化和不同风速风向特征等角度,对3种海面风场资料(ERA-I、CCMP、CFSR)在吕宋海峡处的风速和风向质量进行了较为全面详细的对比和评估。主要结论如下:(1)3种风场资料在吕宋海峡处风速整体偏小,海峡中部误差较小,南北两端误差较大;均方根误差季节变化显著,6月最小,12月最大;(2)风速误差随不同风速、不同风向而不同,整体呈现高风速时风速较观测偏大,低风速时风速偏小的特点,且低风速段误差较小,高风速段误差随风速增大而增大;(3)3种风场资料在吕宋海峡处风向整体偏右,海峡中部误差较小,南北两端误差较大;季节变化显著,12月最小,5月最大;(4)风向误差随不同风速、不同风向而不同,偏北方向,风向偏右;偏东方向,低风速段风向偏右,高风速段风向偏左;偏南方向,低风速段风向偏左,高风速段风向偏右;偏西方向,风向呈偏左状态。风向误差整体随风速的增大而减小;(5)综合比较,CCMP的风速、风向资料质量均好于其他两种资料。  相似文献   

9.
本文概括了近几十年来,关于德里克海峡附近绕极流研究的进展,这些研究主要以实际观测资料为基础,说明了德里克海峡附近海洋锋面分布和绕极流的体积输运,其中,主要的海洋锋面有:亚南极锋,极锋和陆缘水边界;而德里克海峡绕极流的体积输运则代表了太平洋和大西洋两大洋之间通过德里克海峡的水量交换,读者可通过本文加深关于德里克海峡锋面成因和绕极流机制的理解。  相似文献   

10.
台湾海峡1998年夏季温盐场的分布特征   总被引:2,自引:0,他引:2  
根据1998年夏季台湾海峡调查所得到的温盐观测资料,分析了该海区的温盐场特征。结果表明:(1)海峡西部主要为低温高盐水分布,而在海峡东部则是受高温低盐水控制。(2)海峡西部表层水体的低温高盐特征反映出深层在台湾海峡不同区域沿陆坡爬升的动力特  相似文献   

11.
双功能潜水器是目前国际上比较新型的可用于深海水下观察和作业的装备。既可有缆载人/无人,又可无缆载人。该潜水器最大工作深度450m,其结构材料和结构形式与以往类似的装备不同。文章对双功能潜水器耐压壳结构和载体框架设计中的一些问题进行了探讨,提出的设计思想和计算方法,这对获得一个具有最轻结构重量的实用的双功能潜水器结构具有指导意义。  相似文献   

12.
ArcSDE在数字海底系统中的应用   总被引:5,自引:0,他引:5  
在数字海底系统中的开发中,应用了ArcSDE对渤海工程地质空间数据和属性数据在Oracle中进行了统一存储和管理,并以此数据库为基础,实现了渤海工程地质空间数据的查询显示、虚拟现实等应用。文章重点讨论了ArcSDE的原理及其在数字海底系统中的应用。  相似文献   

13.
Abstract. Sediment characteristics determining macrofauna communities were investigated on the continental shelf of Crete. The sedimentary environment of the outer continental shelf of Crete is characterized by a silty substrate with significant decrease in chlorophyll a and organic carbon concentration with depth. Redox potential values indicated an ample supply of oxygen at all depths. Values of most production-related parameters TOC, chlorophyll a , ATP were found at the low end of the range reported from the literature even though the sampling stations were very close to the coastline. Organic carbon to chlorophyll ratios in the sediments indicated that most of the organic material is of phytoplankton origin; the quality of the organic material in the outer shelf, however, seems to be of lower bioavailability.  相似文献   

14.
15.
At the time of writing, the EU has just finished appointing a new cohort of senior representatives for the period 2014–2019. This includes appointing a Commissioner with a newly defined remit for Environment, Maritime Affairs and Fisheries and the members of the various Committees of the European Parliament with competences related to maritime affairs. These individuals will invariably spend at least part of their first months in office identifying their respective priorities for the coming years. This commentary seeks to contribute to these deliberations by making concrete suggestions for priorities that might be considered as regards the future of the EU’s Integrated Maritime Policy (IMP). Seven years since its launch, the IMP remains very much a work in progress. Drawing on recent academic studies of the EU’s various ocean related policies this commentary argues that two of the greatest weaknesses of the IMP are the sectoral nature of priority-setting and strategy-making as well as the lack of a funding tool to implement its aims. Two concrete proposals are made, specifically aimed at the incoming EU leadership, which seek to address these weaknesses and to realize the aims articulated in the IMP.  相似文献   

16.
文中介绍陆地影像图与港口航道图镶嵌的制图工艺,影像图与港口航道图镶嵌后的成图质量评价。简单阐述了作者在绘制该图种过程中的一些体会,以及影像图取代现有港口航道图上陆地地形的可行性。  相似文献   

17.
Development of ocean community systems relating to the Taiwan Strait Tunnel (TST) project, with regionalization and multistage approach is proposed. The purposes of these systems are to assist the development of coastal marine lands and harbor facilities and to develop connecting isolated islands into an organized community by means of embankment roadways, tunnels, bridges, ferryboats, and so on. The major aim of such an approach is to develop the isolated abandoned islands into useful land improvement, expand the forest, agriculture, and fishing industries and other resources to generate additional revenue to subsidize some of the cost for building the TST. This article points out the systems' importance, outlines the general procedures, and discusses a possible transportation network connecting islands with land; and the outlines development of the knowledge-based expert system computer program to be applied to the ocean community systems relating to the TST project.  相似文献   

18.
Development of ocean community systems relating to the Taiwan Strait Tunnel (TST) project, with regionalization and multistage approach is proposed. The purposes of these systems are to assist the development of coastal marine lands and harbor facilities and to develop connecting isolated islands into an organized community by means of embankment roadways, tunnels, bridges, ferryboats, and so on. The major aim of such an approach is to develop the isolated abandoned islands into useful land improvement, expand the forest, agriculture, and fishing industries and other resources to generate additional revenue to subsidize some of the cost for building the TST. This article points out the systems' importance, outlines the general procedures, and discusses a possible transportation network connecting islands with land; and the outlines development of the knowledge-based expert system computer program to be applied to the ocean community systems relating to the TST project.  相似文献   

19.
In an article published in Marine Policy a year ago, (Lynne and Brian Chatterton, ‘How much political compromise can fisheries management stand’, Vol 5, No 1, April 1981), it was argued that management of South Australian coastal fisheries reflected the political ideology of the government in power, rather than the biological and socioeconomic imperatives of the resource. In the first article below, A.M. Olsen, former Director of Fisheries, criticizes the Chattertons' conclusions, maintaining that fisheries should be managed by professionals not politicians and that many of Brian Chatterton's problems during his tenure as Minister of Fisheries were of his own making. In the Chattertons' response, they point out that by allocating management of the resource between various vested interests (including government bureaucracy) a minister is making a political decision. In the third article, R.D. Walkerden, a former Permanent Secretary to Fisheries Ministers in South Australia, offers an administrator's view of the controversy. Detailed and parochial as some of the points at issue appear, the debate provides an illuminating view of some of the ideological and organizational conflicts that can hinder the effective management of a coastal resource.  相似文献   

20.
Seven dives in the submersible ALVIN and four deep-towed (ANGUS) camera lowerings have been made at the eastern ridge-transform intersection of the Oceanographer Transform with the axis of the Mid-Atlantic Ridge. These data constrain our understanding of the processes that create and shape the distinctive morphology that is characteristic of slowly-slipping ridge-transform-ridge plate boundaries. Although the geological relationships observed in the rift valley floor in the study area are similar to those reported for the FAMOUS area, we observe a distinct change in the character of the rift valley floor with increasing proximity to the transform. Over a distance of approximately ten kilometers the volcanic constructional terrain becomes increasingly more disrupted by faulting and degraded by mass wasting. Moreover, proximal to the transform boundary, faults with orientations oblique to the trend of the rift valley are recognized. The morphology of the eastern rift valley wall is characterized by inward-facing scarps that are ridge-axis parallel, but the western rift valley wall, adjacent to the active transform zone, is characterized by a complex fault pattern defined by faults exhibiting a wide range of orientations. However, even for transform parallel faults no evidence for strike-slip displacement is observed throughout the study area and evidence for normal (dip-slip) displacement is ubiquitous. Basalts, semi-consolidated sediments (chalks, debris slide deposits) and serpentinized ultramafic rocks are recovered from localities within or proximal to the rift valley. The axis of accretion-principal transform displacement zone intersection is not clearly established, but appears to be located along the E-W trending, southern flank of the deep nodal basin that defines the intersection of the transform valley with the rift floor.  相似文献   

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