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1.
随着我国海洋运输业的发展,产业集群特征愈发显现.文章探讨了我国海洋运输业集群的特点,运用主成分分析法对我国海洋运输业的集群状况进行了实证分析,得到了我国海洋运输业集聚程度的排序,提出了发挥我国海洋运输业集群优势的政策建议.  相似文献   

2.
海洋运输是人类利用海洋的一个重要内容,海洋运输在运输业中占有相当重要的地位。我省海域辽阔,海运业的开发利用历史悠久、贡献重大。现在我省在对外经济活动中实行“特殊政策、灵活措施”,搞活经济,因此,如何发展我省海洋运输业,以适应建立立足国内市场,面向国际市场的经济结构的要求,就成了我们研究的当务之急。下面就我省如何充分发挥海洋优势,大力发展海上运输,淡一些粗浅的意见。  相似文献   

3.
三、海洋管理体制国家实施海洋管理,必须设置相应的机构,形成科学的管理体制。不同的国家,海洋管理体制是不同的。决定设置什么样的海洋管理体制,主要因素有:①海洋的地理位置、自然环境、资源状况,以及海洋在国家发展中的地位。象日本这样的岛国,必须发展海洋运输业和海洋渔业,因此必须设立强  相似文献   

4.
发展临海产业实现辽宁海陆一体化建设   总被引:1,自引:0,他引:1       下载免费PDF全文
发展临海产业实现辽宁海陆一体化建设栾维新辽宁师范大学地理系辽宁省是全国重要的沿海省区之一,具备发展海洋经济的优越条件,经过多年开发,海洋水产业、海上运输业、海盐业、滨海旅游业和海洋油气开来业等海洋产业部门都已形成一定规模。但这些并不是海洋开发的全部,...  相似文献   

5.
随着海洋旅游业的高速发展,游客对海洋旅游产品的要求也越来越高,因此以市场为导向,调整优化海洋旅游产品结构就显得格外重要。文章以辽宁沿海旅游城市大连为例,重点分析了海洋旅游产品开发中存在的问题,并对优化海洋旅游产品结构提出几点建议。  相似文献   

6.
山东半岛蓝色经济区海洋主导产业发展实证分析   总被引:4,自引:0,他引:4  
秦宏  谷佃军 《海洋科学》2010,34(11):84-90
随着山东半岛蓝色经济区建设的提出,山东半岛海洋经济发展进入全新的阶段。文章综合运用相关性分析、贡献度分析以及趋势分析等方法对山东半岛主要海洋产业进行综合评价,对山东半岛蓝色经济区海洋主导产业进行了界定,进而对滨海旅游业、海洋运输业、海洋渔业、海洋修造船业、海洋油气化工业和海洋高新技术产业等主导产业的发展方向和重点进行了规划。  相似文献   

7.
海洋平台优化设计的研究进展   总被引:4,自引:0,他引:4  
结构优化是结构设计理论的重要发展,随着“十五”渤海大油田勘探开发战略的实施,结构优化技术将在新型抗冰振平台设计中发挥重要作用。从静力优化设计、动力优化设计、基于可靠度优化设计、全寿命优化设计四个方面论述了海洋平台结构优化设计的研究现状,并展望了海洋平台优化设计的研究前景。  相似文献   

8.
随着海洋运输业的与日俱增,以及深海石油钻探活动的日趋频繁,海洋噪声已成为环境科学家们愈来愈关注的问题。他们发出警告海洋噪声已危及海洋生物。  相似文献   

9.
文章基于1999—2020年我国沿海地区的面板数据,在建立面板向量自回归模型(PVAR)的基础上,运用脉冲响应函数和方差分解等方法,从金融发展规模、效率和结构3个方面,分析金融发展对沿海地区海洋经济增长的影响及其动态关系。研究结果表明:在短期内,金融发展规模会对海洋经济增长产生促进作用,但在长期内可能会制约海洋经济增长;金融发展效率会促进海洋经济增长,并在长期成为主要的影响因素;金融发展结构对海洋经济增长具有促进作用,但持续期较短。因此,海洋经济增长离不开金融有力的支持,应合理控制金融发展规模、提高金融发展效率和优化金融发展结构,为海洋经济增长提供长效支撑,推动海洋经济可持续增长。  相似文献   

10.
为加强海洋学科建设,提升海洋学科人才培养质量,更好地服务地方海洋经济发展,对天津市海洋经济发展和涉海高等教育事业现状进行深入分析,结合天津市高校涉海学科专业建设,提出地方高校对接地方海洋产业发展的路径选择:科学制定海洋教育发展规划,适当调整扩大涉海专业的招生规模;不断优化学科结构,调整专业设置,构建多层次的海洋教育体系;加强京、津、冀协同发展,努力推进协同创新;加强海洋师资队伍建设。  相似文献   

11.
The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ~200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ~380 km from the coast at a depth of ~250 m above the sea level.  相似文献   

12.
We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative abundances of organic and inorganic carbon as an index of the carbon cycle stability.  相似文献   

13.
We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic regime of the sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev  相似文献   

14.
We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the shelf zone and open sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev  相似文献   

15.
A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state.  相似文献   

16.
Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m3 from 1 km of coast in the wide tidal flats and <50 m3 on the steep coasts) are delivered to the water area.  相似文献   

17.
We use many-year archival observations of hydrologic and hydrobiologic state of the Sea of Azov for the identification of the structure of a model of its ecosystem. The ecosystem model, supplemented with expert estimates of bioresource consumption (fish reserve), contamination level, and possible ecologic fines for violation of the sea natural state, is formalized by the method of system dynamics. Hereat, the major part of influence functions is found in terms of observational data with application of self-organization algorithms. We also present the results of simulated experiments with the model of the ecosystem, which enable us to analyse scenarios of its behaviour under the influence of various external factors (wind, river discharge, water exchange with the Black Sea, etc.). Translated by Peter V. Malyshev and Dmitry V. Malyshev  相似文献   

18.
The spatiotemporal variability of the hydrochemical composition of the riverine runoff in nearmouth areas is presented using the example of selected rivers of the Arctic Basin. The temporal dynamics of the riverine nutrient runoff are mainly determined by the seasonal and interseasonal variations in the drainage basins. The spatial variations in the chemical composition of riverine waters in the near-mouth areas are mainly caused by the dynamics of the water flow and the river bed relief and, to a lesser degree, by biochemical processes. It is shown that the variations in the nutrient composition of the waters in near-mouth areas are comparable in magnitude to those at the river-sea geochemical barriers.  相似文献   

19.
The methodology and the first results of the computations of the volumes, masses, and growth rates of the sedimentary body of the buried Black Sea basin are presented. Their temporal evolution reflects the regional paleogeodynamics, in particular, the reorientation of the vector of the relative movement of the Arabian and Eurasian lithospheric plates and the related intensification of their collision in the late Miocene-Pliocene.  相似文献   

20.
Izvestiya, Atmospheric and Oceanic Physics - Analysis of the temporal variations of the virtual heights of the sporadic E layer (h?ES) determined from ionograms with increased accuracy (1...  相似文献   

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