全面推进海洋执法工作再上新的台阶

在全党深入开展学习实践科学发展观活动之际,2009年全国海监工作会议隆重召开.会议的主题是:认真学习贯彻党的十七大、十七届三中全会、中央经济工作会议和全国海洋厅局长会议精神,深入贯彻落实科学发展观,总结2008年工作,部署2009年任务,统一思想、转变观念,增强信心、扎实工作,全面推进海监执法工作再上新台阶.     

风雨兼程七年奋斗 励精图治示范建设

以"海监示范工作"作为有力的抓手,基层海监机构的执法工作从无到有、从弱到强,海监支队逐步成为海监执法实践的主体力量。2010年,中国海监总队对海监示范工作作出重大调整,特对七年来海监示范工作进行回顾,并以7个模范支队作为典型,总结他们2009年的各项工作,讲述事迹,展示风采,交流经验。     

落实科学发展观 强化创新意识 忠诚履行国家使命

8月初,中共中央政治局委员、国务院副总理曾培炎在“中国海监83船”上主持召开了“国务院渤海海洋环境工作会议”,观看了渤海巡航执法活动。会议期间,曾副总理亲切接见了中国海监执法队员,对海洋执法工作寄予殷切希望。目前,全国各级海监机构正在深入学习、贯彻落实曾副总理讲话精神,海监队伍一派蓬勃景象。值此契机,中国海监总队党委书记、常务副总队长张惠荣对海监执法工作进行了全新部署…     

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     

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。     

强化三种意识 做好海监执法工作

随着我国海洋工作地位和作用的日益提升,海监执法工作任务也越来越重。如何寓服务于管理,在建设生态海洋、和谐海洋工作中发挥好作用,笔者认为,至关重要的是要带着情感执法,将执法为民的思想根植于广大海监执法人员的头脑之中;带着责任执法,把依法行政贯穿于执法活动的每个环节;带着良知执法,把廉洁奉公落实到海监队伍建设的各个方面。     

浅谈海监执法船艇装备技术的管理

海监船艇建设是海洋执法工作的基础,也是海监装备体系建设的重点.2010年5月中国海监7002船正式列队,浙江省海监装备建设又迈出了新的步伐,至2010年底浙汀省海监专用执法船艇已经达到20余艘.海监执法船艇数最的逐年增多为海洋监察、海岛巡航、专项行动、维权执法提供了有力的保障,同时也对海监执法船艇装备技术管理工作也提出了新的要求.所谓海监执法船艇装备技术管理,就是对海监执法船艇的机电设备及其器材装备实行科学有效的管理,其根本目的在于科学地掌握和运用船艇使用、腐蚀、老化等规律,正确使用和精心保养船体及机电设备、电子仪器以及消防器材、附属设施等技术装备,使之经常处于良好状态,充分发挥技术性能,防止机械设备老化,有效地延长寿命,保证各项执法任务的完成.     

强化海洋标准化计量质量工作在海洋执法监察中的支撑保障作用

中国海监作为国家海洋局所属的综合性海洋执法队伍,履行着维护国家海洋权益、查处违法使用海域、损害海洋环境、破坏海洋设施、扰乱海洋开发秩序等非法活动的重要职能。随着海监执法工作的不断深入,海监执法工作对技术支撑,包括标准化计量质量管理工作的需求日益紧迫。执法工作的性质和特点,也决定了对标准化计量质量管理工作的高度依赖性。进一步加强海洋标准化计量质量工作在海监执法工     

海监技术装备保障支撑系统建设与管理

随着国家对海洋的重视,海洋权益维护日益严峻,中国海监维权执法任务越来越繁重,面临着严峻的挑战和复杂的形势。文章主要研究建立海监技术装备支撑系统,为海监维权执法提供技术保障与支撑,管理海监技术装备,更好地发挥高新技术装备,为海监维权执法与监察执法提供服务。     

在2006年中国海监总队长会议上的讲话

今天，我们在海南省三亚市召开中国海监总队长会议，研究讨论海监工作“十一五”规划以及今后一段时期的海监工作思路和安排。刚才大家畅所欲言，交流了各自有关“十一五”规划的设想和2006年的工作计划，并对海监工作提出了意见和建议。根据这些意见和建议，我们将进行认真的研究，修改和完善2006年中国海监工作要点和海监工作“十一五”规划。常言说“思路找出路，开局即结局”，正确的思路决定了良好的开局，从某种意义上也意味着成功的结局。在2006年初我们召开中国海监总队长会议研究年度工作计划，目的在于共谋思路，为2006年海监执法工作打好开局。今天的会议开得很成功，我们从大家的发言中得到了不少启发，也使得我们的思路更加清晰。下面我想利用这个机会，跟大家交流一些想法，希望对各地制定海监工作的“十一五”规划和2006年的工作计划，起到一点积极的作用。     

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.     

On the Relationship between the Characteristics of the Annual Variations of the Virtual Height of the Ionospheric Sporadic E Layer with the Seasonal Rearrangements of the Stratomesospheric Circulation

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...     

A model of the dynamics of the ecosystem of the Sea of Azov

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     

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.     

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.