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随着全球海洋经济的飞速发展,海洋产业结构的优化升级问题引起各国的普遍关注。本文在借鉴国际经验的基础上,针对青岛市的具体情况,通过海洋产业的部门分析法,对目前的海洋各产业产值进行排序,分析目前青岛市海洋产业结构存在的问题,提出相应的对策建议。 相似文献
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青岛市的海洋产业发展战略是在保持第一产业稳定增长的条件下,大力发展第二产业,依靠科技进步提高第二产业的比重,稳定第三产业,优化海洋产业结构。建立东北亚航运中心、修造船和临海工业基地、海洋药物基地、海水淡化基地、海水增养殖基地和海洋科技产业城和滨海旅游城。 相似文献
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产业结构变动对经济增长影响已经得到了现代经济增长理论的肯定,但是产业结构变动对经济增长效率的影响一直是学术界没有解决的问题。目前中国已经进入了中等收入国家,粗放式增长逐渐结束,集约式增长越来越受到重视。文章基于海洋产业,研究了海洋产业结构变动对经济增长效率的影响,将海洋产业结构变动具体量化,分为海洋产业结构高级化和合理化;其次运用海洋产业全要素生产率来衡量海洋经济增长效率,通过从海洋生产函数中剔除初级要素带来的海洋经济增长效率得出海洋产业全要素生产率;同时计算出海洋产业劳动和资本的生产效率;最后收集了1996—2015年全国沿海11个省、市、自治区的数据,运用混合面板数据模型来研究海洋产业结构高级化和合理化对海洋经济增长效率的影响。研究发现海洋产业结构合理化和高级化对海洋经济增长具有正面影响,对于未来发展海洋经济提出了提高海洋产业技术来提高海洋产业结构优化,从而使得海洋经济发展走上集约式增长之路。 相似文献
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为促进我国海洋产业结构的优化升级和海洋经济的可持续发展,文章概述我国海洋产业结构现状,选取相关数据和普通最小二乘法模型,计算2005—2014年我国海洋产业结构偏离度,并分析其对海洋经济的影响。研究结果表明:目前我国海洋经济的增长动力主要来源于海洋第二、第三产业,海洋产业结构较合理;产业结构偏离度与劳动生产率成反比,海洋第一产业结构偏离度较高,海洋第二、第三产业结构偏离度较低,这与我国海洋经济发展历程密切相关;产业结构偏离度对海洋经济的影响由大到小依次为海洋第二产业、海洋第三产业和海洋第一产业。在此基础上,提出3点建议,即现代化模式完善海洋第一产业、政府助力完善海洋第二产业和发展多种产业完善海洋第三产业。 相似文献
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地球上的海洋面积为３．６７亿km２，占整个地球５．１６亿km２表面积的７１％；而人类居住的大陆面积仅仅为１．４９亿km２，只占地球表面积的２９％。随着经济的不断发展，海洋正成为人类第二生存空间。目前，我国海洋产业年收入５０００亿元，远远低于发达国家的水平，而海洋产业发展的相关问题也产业发展的整体出发，提出了制约目前我国海洋产业发展的五大因素，并据此提出相应的对策，强调海洋产业结构的调整。也有学者从区域经济的角度强调了海洋产业结构调整的必要性和重要性。本文在进行海洋三产分类的基础上，从产业关联性的角度出… 相似文献
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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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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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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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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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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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I. G. Ostrovskaya 《Physical Oceanography》1992,3(5):397-403
Three mathematical models are considered: a two-dimensional model for calculating the concentration fields of the ecosystem components on the shelf of the Republic of Guinea, a pointwise model for the annual variation of the components, and a two predators-prey model. These models are used to study the effect of hydrodynamic conditions on the state of the shelf ecosystem and for research into the causes which distort the balance between marketable and unmarketable fish.Translated by Mikhail M. Trufanov. 相似文献
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Al. A. Shreider 《Oceanology》2007,47(1):91-103
The first data on the temporal evolution of the slope of the buried depression of the Black Sea are obtained. The sharp change in the rate of the decrease in the slope steepness that occurred in the Late Miocene-Pliocene time reflects a reorientation of the vector of mutual movement and a related intensification of the collision between the Arabian and Eurasian lithospheric plates. 相似文献