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作为现代海洋旅游的重要组成部分,游艇旅游正随着人们收入水平的不断增长而得到蓬勃发展,引起了旅游管理者和学术界的高度关注。本文通过对国内外游艇旅游文献资料的全面检索和分析,发现国外学者对游艇旅游的研究时间较早,研究内容更加广泛和深入,主要包括游艇旅游基础概念探讨,游艇旅游需求与供给研究,游艇旅游对经济、社会文化和环境影响的研究,以及游艇旅游政府管理和协同治理研究等5个方面。而在研究方法上,国外主要采用多学科研究方法,注重实地调研和数据库的建立,通过模型构建与数理统计支撑定性描述。我国未来应不断拓展研究领域,完善游艇旅游理论和实践治理体系,借鉴国际经验探索游艇旅游本土化发展范式,并加强定量研究方法使用,以期为中国游艇旅游发展实践提供参考。 相似文献
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南极旅游是近些年的热点研究问题,日益引起国外学术界和有关国家南极战略决策者的重视。文章在搜集分析相关文献的基础上,比较分析了南极旅游概念与内涵,对主要研究领域进行梳理,发现国外研究内容主要集中在下述领域：南极游客行为分析,包括南极旅游分布特征及其原因、核心吸引力的构成和环保意识等;南极旅游环境影响研究,包括旅游开发与环保两者关系的代表观点、环境影响的具体形式与评估;南极旅游全球治理机制分析,覆盖《南极条约》框架下的治理特征与困境、国际南极旅游组织协会主导的行业自治特征与挑战,以及实施全面旅游管理的探讨。最后探讨了国外研究对国内研究的启示,以期为国内相关研究提供些许参考。 相似文献
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旅游中心城市在旅游业中的地位和功能研究 总被引：10，自引：0，他引：10
从中国旅游业发展实际出发,深入分析了旅游中心城市在旅游业发展中的地位和作用.通过探讨旅游资源开发与旅游城市建设的关系,确立旅游中心城市的主导地位,阐述旅游中心城市的主要功能,分析区域旅游发展的时空演化规律,并对发展旅游中心城市提出3点建议. 相似文献
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为促进粤东地区发挥区域优势、提升海岸带生态功能和促进可持续发展,文章概述粤东海岸带生态系统的类型及其分布,分析其面临的问题,并结合已开展的海岸带生态保护修复项目提出建议。研究结果表明：粤东具有砂质海岸生态系统、重要河口生态系统、红树林生态系统、珊瑚礁生态系统和海湾生态系统等海岸带生态系统,海洋资源十分丰富;但面临海岸侵蚀、环境污染和过度开发利用等问题,不利于发挥海岸带生态和减灾功能;在已开展的中央海域使用金支持项目、“蓝色海湾”整治行动、围填海项目生态保护修复和海岸带保护修复工程等的基础上,未来应开展海岸带生态系统现状调查和评估、加强滨海湿地保护、建立海岸带生态系统动态监视监测平台以及加快海岸带生态保护修复标准体系建设。 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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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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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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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