共查询到20条相似文献，搜索用时 125 毫秒
1.
市级海岛保护规划是沿海市管辖范围内海岛保护的专项规划,内容较省级海岛保护规划更为详尽,实践性与可操作性也更强;较单岛规划覆盖的范围更广,更有利于沿海市海岛保护与利用工作的全面开展,可有效衔接省级规划与单岛规划。文章分析了市级海岛保护规划在海岛保护规划体系中的定位,探讨了市级海岛保护规划的编制要点,以钦州市为例,从规划范围、期限与原则、分类分区与重点工程、区域海岛规划等方面,提出了市级海岛保护规划的编制框架,可为市级海岛保护规划的科学编制提供参考。今后应进一步开展无居民海岛功能分类研究、区域海岛规划的实施情况评估和利益相关者参与机制的探索,为市级海岛保护规划的编制提供支撑。 相似文献
2.
文章从分析厦门无居民海岛资源分布特征与生态问题入手,阐述了无居民海岛保护规划编制的总体框架、基本思路、基本要求与基本内容。强调了无居民海岛保护规划应体现强制性、导向性、针对性和可操作性。论述了海岛功能定位与利用方向的确定对于海岛资源环境保护的重要性,认为分类保护是有效保护海岛资源的重要方法。从方法学上,总结并介绍了厦门海岛保护规划编制的实践经验。 相似文献
3.
4.
无居民海岛保护和利用规划是我国海岛保护规划体系的最后一级规划,是政府引导无居民海岛保护和利用最直接的调控工具。文章在分析无居民海岛保护和利用规划利益相关者概念与内涵的基础上,对无居民海岛保护和利用规划利益相关者进行识别与界定,并根据利益相关者的影响力、利益属性,将利益相关者分为高影响力、高利益性,高影响力、低利益性,低影响力、高利益性和低影响力、低利益性4类,进而根据分类提出了“紧密管理”“使其满意”“保证信息获取”以及“最小程度关注”等管理策略。只有通过对无居民海岛保护和利用规划利益相关者进行界定、分类和管理,才能厘清各方复杂的利益关系,让利益相关者参与规划编制,达成规划共识,使无居民海岛保护和利用规划更具科学性和实用性。 相似文献
5.
我国是世界上海岛最多的国家之一,而海岛的无度无序开发却是我国海岛管理所面临的严峻问题,在《中华人民共和国海岛保护法》颁布前我国尚无一套完整的规划体系是针对海岛而设立的,海岛的开发利用问题都是各个部门交叉处理。文章通过对海岛保护规划体系进行梳理分析,认真研究规划编制的程序和规划的编制内容,为今后海岛保护规划的编制提供理论基础。 相似文献
6.
7.
8.
9.
省域海岛保护规划是全国海岛保护规划的重要体现和具体落实,通过对海岛进行分类登记,合理划分省级管辖区域内海岛的功能分区,科学设置重点工程,是指导各省海岛保护与开发的指导性文件。规划成果及时、完整备案,对加强规划落实、促进海岛管理、实施规划监督、支撑规划评估等具有重要意义。目前,省域海岛保护规划备案工作尚未形成一套较为完备的备案体系,造成备案工作可操作性不强。文章在对规划编制及成果充分研究的基础上,梳理了规划备案现状、阐述了规划备案的必要性、分析了规划备案存在的问题,明确了备案管理体系的构成,初步形成规划备案管理体系。在此基础上,基于海岛管理信息系统,实现海岛保护规划备案及可视化分析。 相似文献
10.
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.
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
17.
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
18.
The study of the sedimentary body of the Bransfield Strait has made it possible to identify several sedimentary complexes, to construct the first electronic charts for the acoustic basement, and to establish four stages of the evolution of its floor, which updates the previous knowledge about the formation of the strait. At the first stage, there was an increase in tension stresses that were accompanied by the local splits of the continental crust at the periphery of the Antarctic Peninsula. At the second stage, a graben-like structure filled with the Lower stratigraphic complex was formed northward of the Antarctic Peninsula. At the third stage, the continuing processes of extension led to intensive explosive activity of the growing volcanic structures and filling of the graben with sediments of the Middle seismostratigraphic complex. The fourth stage, which has continued until recently, is characterized by quasi-linear localization of the major centers of volcanic activity in the band closer to the South-Shetland Islands and the formation of the Upper seismostratigraphic sedimentary complex. The evolution of the floor of the Bransfield Strait reflects the process of penetration of the American-Antarctic ridge to the continental lithosphere of the Antarctic Peninsula for the last million years. 相似文献
19.
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
20.
A. G. Zatsepin N. N. Golenko A. O. Korzh V. V. Kremenetskii V. T. Paka S. G. Poyarkov P. A. Stunzhas 《Oceanology》2007,47(3):301-312
An analysis of the data of measurements of the fine structure and microstructure fluctuations of hydrophysical fields in the upper 200-m layer of the Black Sea carried out using CTD profilers and a Baklan free falling microstructure and turbulence profiler revealed the existence of a positive correlation between the intensity of the fine structure and microstructure fluctuations and the dynamics of the currents. On the other hand, the level of the fine structure and microstructure fluctuations reflects the rate of the vertical turbulent exchange. It was shown that, in the case of the absence of the Black Sea Rim Current (BSRC) jet or clearly manifested mesoscale eddy structures, the vertical turbulent exchange in the pycnocline is weak, while, in the opposite case, it is stronger. The results obtained support the supposition that the interbasin dynamics play an important role in the maintenance of the rate of small-scale mixing in the pycnocline and halocline and provide the vertical transport of dissolved oxygen from the cold intermediate layer into the deeper layers of the sea. 相似文献