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山东沿海旅游业可持续发展对策研究 总被引：4，自引：1，他引：4
滨海旅游是旅游活动的重要组成部分 ,在我国具有广阔的发展潜力。在讨论了山东沿海旅游业发展中存在的问题的基础上 ,指出发展滨海旅游与滨海和海洋环境之间的相关关系 ,探讨了使山东沿海旅游业可持续发展的主要对策 相似文献
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随着中国改革开放的不断深化，20世纪80年代以来，滨海旅游开始兴起并且不断发展，逐渐成为海洋经济乃至国民经济的重要组成部分。研究我国滨海旅游业的发展效率，对科学地制定滨海旅游业相关的政策具有重要的意义。文章选择劳动力和资本两大重要投入要素为依据，采用规模报酬可变的BCC-DEA模型，构建了一个滨海旅游业的发展效率评价指标体系，分析滨海旅游业2005—2016年的发展效率。研究结果表明，2005—2016年滨海旅游业的发展效率偏低，均值为0.658，期间各年度的发展效率呈现持续增长的趋势，同时规模效率的增长是发展效率持续攀升的主要原因。基于上述情况，提出完善滨海旅游资源开发及滨海旅游配套设施，避免滨海旅游项目同质化，开发特色滨海旅游产品，丰富滨海旅游产品体系，加大营销力度，提升滨海旅游品牌等相关建议。 相似文献
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任何旅游区都是通过旅游区划来实现其旅游价值的。山东省是海洋大省,也是滨海旅游的重要省份,而滨海旅游业又是经济发展的先导产业,作好滨海旅游区划对发展本地区的旅游业起着重要的决定性作用。 相似文献
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滨海旅游是我国新兴的海洋产业，由于我国拥有较多的旅游自然资源与人文资源，加之我国出台了一系列政策刺激消费，极大地促进滨海旅游业的发展。我国即将加入世贸组织，届时将对我国滨海旅游业产生巨大的影响，因此我们必须及早考虑应对措施，趋利而避害，掌握国际旅游市场的主动权。 一、我国滨海旅游业的发展现状与问题 １、滨海旅游业的发展现状 改革开放以来，我国沿海地区利用海洋资源优势和对外开放前沿的优势，大念“山海经”，吸引了大批的国内外游客同时，国家也在滨海旅游方面给予了许多政策，对外开放的地区也越来越多，我国主… 相似文献
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滨海旅游业是重要海洋产业之一。近十年我国滨海旅游业有了一定的发展。本文综合介绍了我国滨海旅游业开发现状,对目前我国滨海旅游业开发中存在的多种问题进行了论述。并提出了滨海旅游业开发的区域性布局和相应的对策。 相似文献
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近年来,休闲旅游逐渐成为人们享受生活、开拓视野的重要方式之一,其中滨海旅游吸引了众多国内外游客,威海市拥有丰富的滨海旅游资源,十分适合发展滨海旅游业。随着近年来旅游标准和需求的不断提高,旅游业的发展规划必须与时俱进,文章通过SWOT分析法对威海滨海旅游业现状进行分析,并根据分析结果提出威海滨海旅游业发展的对策。包括:开发独具特色的滨海旅游项目及相关产品;完善滨海旅游基础设施的建设;引进及培养高素质旅游人才;加强政府的引导和宣传力度。以此来提高威海市滨海旅游业的知名度和赞誉度,推动威海市的滨海旅游业走向更高层次。 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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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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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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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
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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. 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