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1.
建设"海洋经济强市"要求福州借鉴发达国家或地区(如上海、宁波、大连、青岛、深圳等)先进的海洋经济实践,充分发挥福州自身海洋资源的比较优势和区位优势。此调查报告正是遵循这一思路,在对海洋经济进行充分理论分析基础上,探寻海洋经济发展规律,研究宁波发展海洋经济的先进经验,结合福州市自身的资源和社会情况。提出今后福州市加快海洋经济发展的战略思路。 相似文献
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上海傍江临海,具有丰富的滩涂、港口航道、滨海旅游、海洋可再生能源及海洋生物资源。随着上海聚焦“两个中心”战略的推进和长江隧桥工程的建成,海洋在上海可持续发展中的地位与作用日显突出,旨在查清上海资源家底的“上海市908专项”任务的开展正当其时,功在当代、利在千秋。 相似文献
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为充分展示我国改革开放以来海洋事业的发展,交流海洋科技及海洋经济所取得的巨大成就,深入了解国际海洋资源开发利用和技术设备发展状况,进一步拓展国际合作与交流,中国海洋学会与中国贸促会上海市分会,拟定于1999年11月28日在上海举办“99上海国际海洋开发展览会”。预计展览内容包括:海洋生物资源开发利用,海洋空间资源开发利用,海洋矿产资源开发利用,海水资源开发利用,滨海 相似文献
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海洋邮轮旅游产业在现代旅游业的发展中有极大的潜力。近些年来,邮轮旅游产业被誉为"漂浮在黄金水道上的黄金产业"。随着中国经济的发展,我国邮轮旅游业迅速兴起,使多级邮轮市场开始向中国倾斜,成为带动中国经济发展的新动力。文章首先对比了邮轮旅游业国内外的研究现状和理论分析方法,并介绍了上海海洋邮轮旅游业目前的发展现状;其次用"SWOT"分析法的角度讨论了上海邮轮旅游业面临的机会和威胁;最后针对上海海洋邮轮旅游产业,分别从改善环境、扩大宣传、丰富航线和完善港口设施等方面提出了邮轮旅游业的长期发展方向。 相似文献
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根据国家海洋局"数字海洋"的总体目标和总体框架,结合浙江省的实际情况,浙江省"数字海洋"建设的重点先期放在"数字海洋"信息基础框架建设上,基于国家"数字海洋"信息基础框架进行统筹规划和标准统一。充分利用"908专项"成果和浙江省在海域管理、环境保护、海岛和海岸带资源开发利用等各个领域积累的丰富信息资源,建立面向海洋经济、海洋开发管理和海洋决策支持的海洋信息基础平台和省级海洋综合管理信息系统,形成业务化海洋信息综合应用服务能力,为浙江省的海洋管理、海洋经济发展以及社会公众服务。 相似文献
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《中国海洋大学学报(自然科学版)》2010,40(5)
<正>第十届中国海洋药物学术研讨会2009年11月7日-9日在青岛召开,本届会议的主题为"海洋创新药物——人类健康的新希望"。科技部"863"计划海洋技术领域有关领导、国内海洋药物及相关研究领域的100余位专家学者应邀到会。与会代表围绕海洋药用生物资源及新资源开拓,海洋药物先导化合物的筛选,发现与结构优化,海洋多糖(寡糖)及 相似文献
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随着战略性资源短缺对经济社会发展的约束日益显现,海洋资源的开发利用已成为世界各国关注的焦点。上海是我国最大的滨海城市,也是资源最为紧缺的城市之一,在城市可持续发展中,面临土地、能源、环境容量有限等资源要素的制约。相对于上海陆域贫乏的自然资源,海域中却蕴藏着较为丰富的各类海洋资源,是上海国际“经济、金融、贸易、航运”中心建设的重要资源基础和保障。一、上海海洋资源现状及评价上海海域位于《全国海洋经济发展规划纲要》中的第七个经济发展区(长江口-杭州湾经济区),是我国海洋经济发展最具潜力的地区之一。目前,与上海海… 相似文献
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国家建设"海洋强国"战略与重建"海上丝绸之路"构想给浙江这一海洋资源丰富大省的经济发展注入了新的活力,海洋金融是发展海洋经济的核心动力,推进浙江海洋金融的发展有利于推动浙江经济的发展和国家政策的落实。浙江省海洋金融获得了初步的发展,但在抓住机遇的同时要关注所面临的问题,在全面掌握事实的基础上对浙江海洋金融的未来进行规划。并提出以下应对策略:提倡绿色海洋金融,注重海洋经济的可持续发展;从多方位、多角度、多领域考虑进行投融资;合理配置海洋金融资源,管控投融资风险;推进海洋金融创新,促进海洋产业结构合理化。 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
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.
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
18.
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
19.
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
20.
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