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论我国的海洋产业结构及其优化 总被引：19，自引：0，他引：19
海洋产业结构是指各海洋产业部门之间的比例构成以及它们之间相互依存、相互制约的关系。海洋产业结构是否合理，对一个国家的海洋经济发展至关重要。分析了海洋产业的划分方法以及我国海洋产业结构的现状及存在的问题，论述了我国海洋产业结构优化的目标、原则和具体措施，为海洋经济协调、稳定、快速发展提供参考依据。 相似文献
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刘明 《海洋与海岸带开发》2008,(12):9-14
从海洋安全角度分析影响我国海洋经济发展面临的国内国际方面的问题。首先从探讨海洋经济安全的内涵入手，分析世界主要沿海国家及我国周边国家海洋经济发展状况，研究当前我国海洋经济安全形势，在此基础上，提出为维护我国海洋经济安全应强调的主要对策。 相似文献
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加强海洋综合管理，提高海监执法水平，对于维护海洋开发秩序和海洋权益，促进海洋经济、社会、生态效益和谐共进，保障海洋经济又好又快发展，都具有极其重要的作用。目前我国海洋经济发展速度明显加快，全社会依法用海意识明显增强，海洋法制建设日趋完善，海监执法队伍日益壮大。但在海洋执法管理中仍存在不容忽视的问题。主要结合海洋执法管理中存在的问题．对加强海洋监察执法工作．促进海洋经济又好又快发展提出了建设性的建议和措施。 相似文献
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解决海洋经济发展中资金短缺问题的思路徐质斌（山东省海洋经济研究中心副主任）资金投放问题是海洋经济发展中一个关键问题。无论是海洋经济的全面启动，还是海洋科技项目的研究，都需要大量的资金。我国作为一个发展中国家，资金短缺是一个普遍现象，资金短缺已成为海洋... 相似文献
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从山东海洋产业发展现状出发，通过对资源与产业及科技等问题的具体分析，用辩证的观点，阐述了影响山东海洋经济发展的深层矛盾和制约因素，指出了以往认识中的盲区，同时提出了改善与修补的基本思路。 相似文献
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开发海洋资源，加快海洋经济发展，是我国的一项重要发展战略。贯彻和落实科学发展观就要统筹海洋经济的发展和海洋资源及海洋环境之间的关系，以法律为基础，以行政管理和执法监察为手段，通过科学的决策，协调海洋产业的发展步骤，为综合开发利用海洋、保护海洋，搭建良好的经济发展平台，促进海洋与人类的和谐发展。 相似文献
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威海在发展海洋经济方面有着天然优势和巨大潜力,如何更好地挖掘、利用传统优势,更好地转型、再造新优势,推动海洋经济发展走在前,是威海面临的一项重大课题。文章从大海洋概念入手,系统、科学地分析了威海在海洋空间与资源开发利用、海洋科技创新驱动、海洋经济发展机制模式等方面的历史和现状,提出了推进海洋经济高质量发展的过程中面临的过程性、结构性问题,并深入地剖析了问题出现的原因。文章立足于海洋发展的全过程,创新性地从宏观和微观两个层面,提出符合威海实际、切实可行地巩固传统优势、塑造新优势和打造海洋经济发展新格局的对策建议。 相似文献
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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
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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
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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
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V. A. Ivanov S. P. Lyubartseva N. Mikhailova N. B. Shapiro 《Physical Oceanography》2001,11(6):509-524
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
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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
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Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east 总被引：2，自引：0，他引：2
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
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I. E. Timchenko A. A. Primalenny V. D. Yarin E. F. Vasechkina E. M. Igumnova 《Physical Oceanography》2001,11(4):367-378
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
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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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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
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E. L. Vinogradova 《Oceanology》2008,48(4):483-492
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