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1.
海洋是高质量发展战略要地,推动海洋经济高质量发展是建设海洋强国的必然选择。文章从海洋经济高质量发展的内涵出发,以新发展理念为基础,运用熵权-TOPSIS模型评价沿海地区海洋经济发展质量的综合能力并分析其区域差异。实证结果显示：(1)五大准则层指标按权重从高到低排序依次为：海洋科技创新、对外开放、海洋经济结构、社会民生、海洋生态环境;(2)沿海地区的海洋经济高质量发展水平在考察期间为波动上升趋势,各省(自治区、直辖市)间海洋经济发展质量差距在逐渐变小;(3)影响海洋经济发展质量各子系统中,北部海洋经济圈在5个子系统评分中均处于较低水平。为此,提出促进海洋经济高质量发展的提升路径：海洋科技创新与海洋产业结构升级协同发展、完善海洋生态环境保护政策、打造对外开放新格局等。 相似文献
2.
海南陵水县区位和资源优势明显,在海洋经济发展和海洋生态文明建设中优势独特。文章在分析海南陵水建设海洋强县的优势条件的基础上,指出了建设海洋强县存在的问题,最后为加快实现海洋大县向海洋强县的跨越,从如下几个方面探讨了建设海洋强县的对策措施:陆海统筹,科学开发利用蓝色国土空间;发展壮大海洋渔业,构建现代渔业格局;充分利用独特的海洋资源环境,发展滨海旅游业;加强新村港整治,充分发挥国家级中心渔港的综合效益;加强海洋生态环境保护力度,推进海洋生态文明建设;加强海洋管理,提高海洋综合管控能力;实施科技兴海战略,提高海洋经济的质量和效益;加强海洋文化建设,提高海洋意识。 相似文献
3.
2011年国家发布的以海洋经济为主题的山东、浙江、广东3省的海洋经济发展规划重视对外开放、辐射连带、产业结构调整、生态文明建设和金融支持。山东省侧重从陆地依托、科技创新和发展海洋文化产业寻找突破口;浙江省强调加强港口建设、海岛开发与海洋清洁能源开发;广东省突出综合管理、区域合作和南海开发3个领域。为更好地促进海洋经济发展,探讨了3省的发展模式,为提升海洋综合管理水平,走绿色、低碳、高科技的蓝色经济发展之路提供了借鉴。 相似文献
4.
为促进我国海洋经济的高质量可持续发展,文章运用系统GMM实证检验海洋科技创新路径下环境规制对海洋经济发展的影响,并提出发展建议。研究结果表明：环境规制与海洋科技创新的联动显著促进海洋经济发展,且命令控制型环境规制的促进作用显著,而市场激励型环境规制的促进作用不显著;海洋劳动力投入对海洋经济发展起重要作用,对外开放程度对海洋经济发展的影响不显著;环境规制与海洋科技创新的联动显著促进东部和北部海洋经济圈的海洋经济发展且促进作用东部大于北部,但对南部海洋经济圈的促进作用不显著;未来应进一步完善环境规制政策、加快海洋科技创新、因地制宜发展、建设海洋人才队伍以及升级对外贸易结构。 相似文献
5.
21世纪海上丝绸之路是我国在新时期构建全方位对外开放新格局的重大举措。促进海洋产业结构升级、实现海洋经济提质增效、开展海上综合保障能力是海上丝绸之路建设的重点方向。海洋经济活动与海上综合保障都需要海洋科技的基础支撑,21世纪海上丝绸之路建设对海洋科技领域提出了新命题。文章围绕科技创新政策伙伴关系、推进海洋经济和产业发展、培育创新品牌等方面,深入分析发挥海洋科技领域在21世纪海上丝绸之路建设中支撑作用的思路和途径。 相似文献
6.
为加强海洋生态环境保护,大力提高海洋科技创新能力,推动海洋经济、海洋科技创新和海洋生态环境三者协调发展,文章以我国沿海11省（自治区、直辖市）为研究对象,选取22个评价指标,采用综合评价模型和耦合协调模型,评价2016年各沿海地区海洋经济、海洋科技创新和海洋生态环境的协调发展状况,并提出发展建议。研究结果表明:广东和山东处于中级耦合协调状态,上海和福建分别由于海洋生态环境和海洋科技创新的制约而处于初级耦合协调状态,天津等4个地区处于勉强耦合协调状态,河北处于轻度失调衰退状态,海南和广西处于中度失调衰退状态;各沿海地区在发展海洋经济的同时要提高海洋科技创新能力,守住海洋生态环境的底线,推动海洋经济系统、海洋科技创新系统和海洋生态环境系统的协调发展。 相似文献
7.
为科学合理评价区域海洋科技发展水平,进一步促进区域海洋经济增长,文章以东部海洋经济圈为例,采用主成分分析方法构建海洋科技发展水平综合指标,采用多元线性回归模型分析海洋科技发展等因素与海洋经济增长之间的关系,并提出建议。研究结果表明:海洋科技发展水平综合指标包括海洋科技支撑、海洋科技成果转化和海洋科技投入3个主要素及其11个指标,2006—2015年东部海洋经济圈各地海洋科技发展水平整体处于上升趋势,且差距较小;除政府支持力度外,海洋科技发展水平、海洋第三产业发展水平和工业污染程度等变量均与海洋生产总值存在显著相关关系,其中海洋科技发展水平为正相关;未来应促进海洋科技成果转化、减少区域壁垒制约以及加强海洋生态环境保护和治理。 相似文献
8.
海洋经济高质量发展是实现海洋强国目标的关键。文章在理论分析的基础上,基于2008—2019年我国沿海11省（自治区、直辖市）的面板数据,运用双重差分法和动态空间杜宾模型实证考察海洋经济发展试点政策对海洋经济高质量发展的影响。研究结果表明：我国海洋经济发展质量整体呈波动提高趋势,其中上海和广东位居前列,海南和广西相对落后;海洋经济发展试点政策显著提高海洋经济发展质量,且研究结论在经过一系列稳健性检验后依然成立;海洋经济发展试点政策通过科技创新促进海洋经济高质量发展;海洋经济发展试点政策对邻近地区的海洋经济高质量发展存在显著的正向空间溢出效应。 相似文献
9.
随着海洋强国战略的实施,探究海洋科技创新对于海洋经济的影响成为实现海洋强国目标的重要推动力。文章基于2008—2019年中国11个沿海地区的面板数据,构建面板模型,在金融发展视角下探讨海洋科技创新对于海洋经济高质量发展的调节效应以及门槛非线性作用。结果表明：海洋科技创新对于海洋经济高质量增长具有显著促进作用;在海洋科技创新对海洋经济高质量发展的影响过程中,金融发展规模和效率表现出正向调节效应,而金融发展结构的调节效应暂不显著;在海洋科技创新作用于海洋经济高质量发展的过程中,金融发展规模存在双门槛效应以及最佳金融发展水平区间,金融发展结构和效率均存在单门槛效应,即当金融发展结构大于单一门槛值时,海洋科技创新对海洋经济高质量增长表现显著正向作用,当金融发展效率大于单一门槛值时,海洋科技创新对海洋经济高质量增长的促进作用增大。 相似文献
10.
为深入揭示海洋科技创新与海洋经济发展的协调关系及其影响机理,促进我国海洋科技和海洋经济的高质量和可持续发展,文章构建海洋科技创新和海洋经济发展2个系统的评价指标体系,以辽宁为实例,利用协调度模型分析二者的协调度及其演化趋势,进一步利用结构方程模型构建海洋科技创新影响海洋经济发展的驱动路径,以此分析其影响因素和影响效应,并提出对策建议。研究结果表明:1997-2016年辽宁海洋科技创新与海洋经济发展的协调关系分为中度失调衰退、严重失调衰退、中度协调发展和良好协调发展4个主要阶段;海洋科技创新通过海洋资源水平、海洋经济规模和海洋经济结构对海洋经济发展产生直接效应,同时通过海洋经济规模对地区经济发展产生间接效应,即海洋科技创新对海洋经济发展和地区经济发展均产生显著的促进作用;未来应统筹海洋科技与海洋经济的协调发展,扩大海洋科技的投入和产出,积极培育海洋科研人才和新兴海洋产业,注重提高对外开放程度和发展港口经济。 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.
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
15.
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
16.
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
17.
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
18.
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
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.
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