积极探索 勇于实践 全面推进海监先进示范支队建设

2007年以来,中国海监南通市支队在各级海洋行政主管部门及海监总队的正确领导和关心支持下,在南通市全体海监人员的共同努力下,以争创海区级模范支队和国家级模范支队为契机,以执法能力建设为核心,以履行海监职     

从“心里没底”到“颇具影响力”——记中国海监第九支队的成长

中国海监第九支队作为海监总队的一个基层支队，是2000年10月成立的。笔者作为其中的一员，亲身经历了支队从小变大，从弱变强的过程。刚成立时，支队一穷二自，只有一辆汽车，没有船。支队共有16名人员，执法工作主要由执法监察科4名同志负责，管辖的是海岸线长达1595千米的广西沿岸海域。执法监察科的4名同志多是从海洋监测、观测岗位转行而来，即使个别同志曾有少许的海洋执法经历，而那些在海监机构成立之前的执法活动却是不规范的。支队的执法工作就是在这个起点上启动的。     

加强海监执法管理 创建海监示范大队

中国海监启东市大队认真按照国家海洋局《关于开展2005年度中国海监执法示范工作的通知》和中国海监总队《关于开展养殖用海专项执法工作的意见》精神,紧紧围绕海监执法示范工作主题,以执法能力建设为核心,以履行海监职责为己任,以建一流队伍、树一流形象、创一流业绩为目标,锐意进取,开拓创新,大胆进     

着力打造国家级自然保护区海监中坚力量

根据国家海洋局在国家级海洋类型自然保护区成立海监支队的有关要求,2006年4月21日,昌黎黄金海岸国家级自然保护区上报成立海监支队的申请获得了批准.由此,保护区执法工作得到了明显改善,执法能力更强,保护成效更加显著.自成立以来,在中国海监总队和河北省海监总队的正确领导和大力支持下,中国海监昌黎黄金海岸国家级自然保护区支队(以下简称"保护区支队")不断完善能力建设,不断创新工作思路,不断提高执法人员素质,正在向着基础建设标准化、队伍建设目标化、装备设施现代化、查办案件规范化、执法监察科学化的目标大步迈进.     

热情饱满 脚踏实地 走在海监执法工作前列

<正>中国海监舟山市支队自2005年开展执法示范工作以来,在上级海监机构的关心和支持下,成绩斐然。2009年,舟山市支队根据中国海监总队《关于开展2009年中国海监执法示范工作的通知》和《东海区2009年度执法示范工作实施方案》要求,以保持模范支队称号为目标,组织开展2009年度     

加强我国海监队伍建设的几点建议

我国海上执法队伍建设是个庞大的课题，已有一些专家、学者对其进行了较为深入的研究并取得了一些成果。其中一些具有可操作性的建设方案已为国家相关部门所采纳，并已进入运作阶段。作为海上执法力量的海监队伍也有一个加强队伍建设的问题。改革我国海监队伍管理体制经中编办批准，中国海监总队于１９９８年１０月１９日正式成立。中国海监总队是国家海洋局领导下的，由中国海监各海区总队、各沿海省海监总队、市海监支队及县海监大队共同组成。中国海监各海区总队又下设直属支队（如中国海监第一支队）、航空支队（如中国海监北海航空支队…     

新时期海监执法人员应具备的基本素质

随着海洋开发活动的日益频繁和用海项目的大幅度增加,海监执法工作任务将越来越重,作用也将越来越大。要适应海监执法管理新的形势,确保海监执法职能的有效履行,海监执法人员必须具备以下三个方面的基本素质。     

浅议在海监执法工作中落实科学发展观

在全党开展深入学习实践科学发展观活动,是党的十七大作出的一项重大战略部署。日前,中国海监潍坊市支队组织开展了科学发展观专题学习活动,对海监执法历程进行了回顾总结,深刻分析了当前海监执法面临的形势,并对海监执法的前景与未来进行了探讨和展望。落实科学发展观,提高党的执政能力,体现在海监执法工作中,就是要求海监工作者以更加科学的态度和务实的精神,推进海监执法工作不断科学化、规范化。     

中国海监广东省总队 以政治强队为主线 以督察工作为重点

中国海监广东省总队共设21个海监支队、52个海监大队,共有人员2200人。根据国家有关法律授权,代表国家履行广东省近42万平方千米管辖海域的海洋执法监察职责,维护国家海洋权益、保护海洋环境、维持海洋开发秩序。     

加强领导 严格执法 使海监工作取得更大成果

<正>2008-2009年,中国海监第七支队继续以开展执法示范工作和贯彻落实国家海洋局"79号文"为行政执法工作重心,根据国家海洋局《关于规范中国海监海区总队行政执法工作的意见》、中国海监总队《关于开展2008年中国海监执法示范工作的通知》和中国海监南海总队《2008年度南海区海监执法示     

Model of the post-Cenozoic evolution of the cryolithozone of the shelf of the western part of the Laptev Sea

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.     

Investigation of the mechanism of the long-term evolution of the carbon cycle in the ecosystem of the Sevastopol bay

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.     

Contemporary state of the investigation of the influence of the discharge of rivers on the hydrologic structure of the Black Sea

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     

Modelling of the ecosystem of the Black-Sea shelf zone near the estuary of the Danube

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     

Dynamics of the ice cover and peculiarities of the ice transportation of the sediments at the tidal flats of the Kandalaksha Gulf of the White Sea

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.     

Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

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.     

Variability of the nutrient runoff of the rivers of the Arctic Basin

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.     

Parameters of the sediments of the deep-water basin of the Black Sea

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.     

Modelling of the ecosystem on the shelf of the Republic of Guinea

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.     

Evolution of the slope of the buried depression of the Black Sea

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.