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海洋伏季休渔制度是一项重要的渔业资源养护管理制度。该制度自1995年实施以来取得了良好的效果,同时在国际上也产生了积极的影响。作为渔业管理领域中最为重要的制度之一,海洋伏季休渔制度目前只是一项渔业政策和措施,并没有上升到国家的法律和法规层面,该制度的效力远不能从根本上解决我国海洋渔业资源养护和可持续发展的问题。因此,文章对海洋伏季休渔制度的具体内容进行了深度分析,从法律与政策的关系出发,通过探讨国家立法、执法以及渔民守法等方面存在的问题,指出海洋伏季休渔制度作为一项渔业政策向法律和法规转变的必要性和条件,建议推动伏休政策的立法转变、加强渔业执法监督体制和加强政府对渔民的扶持政策。旨在进一步促进实施该制度,为海洋渔业资源的可持续发展服务。 相似文献
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总可捕量(Total Allowable Catch,TAC)制度是海洋渔业产出控制管理的一种有效措施,是与投入控制管理措施的耦合,对海洋渔业资源管理具有推进作用。韩国成功地导入并摸索出独自的TAC制度,其对象鱼种由1999年的5个品种演进并增至2009年的11个品种,海洋渔业资源管理已取得显著性成效。韩国在渔业科学数据收集、奠定TAC制度法律基础、培育和发展渔民协会组织、探讨TAC制度基本架构等方面的制度安排及其经验和做法,对中国具有借鉴与参考价值。 相似文献
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21世纪以来底拖网渔业的快速发展给脆弱海洋生态系统（VME）带来极大威胁,导致公海深海渔业发展不可持续以及海洋生物多样性降低。为更好地实现养护海洋渔业资源和保护海洋生物多样性的目标,同时为我国在保护VME以及管理公海深海渔业方面提供参考,文章分析八大区域渔业管理组织（RFMO）针对VME保护采取的系列措施及其保护VME的可行性,针对存在的问题提出对策建议,并对我国在RFMO中保护VME进行展望。研究结果表明：《公海深海渔业管理国际准则》在RFMO保护VME的实践中发挥重要的指导作用;RFMO采取的措施限制深海渔业活动,但为保护VME和养护海洋渔业资源提供重要基础和保障;未来RFMO应加强信息共享和技术合作,发展VME分布预测技术,同时在保护海洋生物多样性方面积极开展双边和多边合作;我国应进一步研究和实践基于生态系统的渔业管理方法,平衡保护与开发利用的关系,积极参与国际渔业管理和VME保护并促进合作,加强南极海域海洋保护区综合治理。 相似文献
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海洋渔业对海洋生态系统的影响越来越受到人们的重视,考虑生态系统的管理已经成为海洋渔业管理的发展趋势.作者分析了海洋渔业对海洋生态系统产生的影响,包括捕捞活动对目标和非目标种产生的危害、渔业资源栖息地和环境破坏、生物多样性降低等;分析了国际上考虑生态系统的海洋渔业管理的法律框架、国际组织和有关国家的实践及其具体措施,指出了中国在此方面存在的问题:海洋生态系统的基础科学研究缺乏系统性和全面性;基于生态系统的海洋渔业管理的理论研究比较缺乏;相关的法律框架不够完善等.讨论了应用生态系统方法的海洋渔业管理与传统的海洋渔业管理间的关系,指出生态系统方法在其实践中将存在各种问题,认为生态系统方法应有选择地应用.对中国海洋渔业管理如何应用生态系统方法,建议:(1)加强海洋生态系统的基础科学研究;(2)开展基于生态系统的海洋渔业管理理论和方法研究;(3)逐步建立相关的法律和制度框架;(4)开展广泛的多部门合作和国际合作. 相似文献
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海洋渔业是辽宁省海洋经济的重要组成部分,海洋功能区划是建设海洋渔业资源开发利用和保护机制的重要举措.在研究辽宁省海洋功能区划的基础上,分析了辽宁省海洋渔业的发展现状及面临的主要问题,提出了海洋渔业可持续发展的对策.即通过调整渔业产业结构、实施"科技兴渔战略"、发展渔业第三产业、优化远洋捕捞产业、加强渔业资源利用和养护区的建设等措施来促进海洋渔业的可持续发展. 相似文献
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基于Pocket PC 的海洋渔业调查数据采集 总被引：1，自引：0，他引：1
针对传统的主要依赖于纸质日志记录海洋渔业资源调查数据所存在的数据质量差、难以保存、作业效率低等弊端,结合Pocket PC移动终端的优越性,提出利用Pocket PC平台记录海洋渔业资源调查数据,并分别就近海调查和远洋调查数据采集提出了相应的基于 Pocket PC 平台的信息化数据采集解决方案。然后以大洋性鱿鱼资源调查为例,设计并开发了一个基于Pocket PC的海洋渔业调查数据采集系统。通过实践检验,该系统可较好地完成大洋性鱿鱼资源调查的数据采集任务,同时也表明了基于 Pocket PC的海洋渔业调查数据采集的可行性和优越性。讨论的数据采集解决方案和相关技术可为海洋渔业和海洋环境相关的调查数据采集提供信息化支持。 相似文献
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无论是经历半个世纪的江苏省海洋渔业指挥部还是年轻的"两沙"海域管理委员会办公室.无论是在海洋渔政执法还是在海监执法、资源养护等一系列的工作中,我们清楚地知道,鲜艳的党旗一直在高高飘扬. 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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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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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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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