《热带海洋学报》征稿简则

<正>《热带海洋学报》是由中国科学院南海海洋研究所主办、科学出版社出版、国内外公开发行的海洋学综合学术刊物,是我国自然科学核心期刊之一,是《中国学术期刊综合评价数据库》、《中国科学引文数据库》、《万方数据——数字化期刊群》来源期刊,已为《中国学术期刊(光盘版)》和《中国期刊网》全文收录,并已入选中国期刊方阵;同时还被联合国《水科学与渔业文摘》、美国《化学文摘》、俄罗斯《文摘杂志》及英国《动物学记录》收录为源期刊。主要刊载     

毁灭就在后天？

看繁华如伺毁于一旦电影《后天》英文原名为《The Day AfterTomorrow》,也译为《明日之后》、《末日浩劫》和《劫世惊魂》,是二十世纪福克斯公司今年投放市场的科幻灾难巨片,5月28日全球同步上映。该片投资达1.25亿美元,由曾经执导《独立日》、《爱国者》等片的著名导演罗兰德·埃米里奇执导,由丹尼斯·奎德、杰克·吉伦哈尔、艾米·罗森、沙拉·沃德等大牌明星主演。     

《海洋测绘》被日本《日本科学技术振兴机构数据库》收录

<正>日前,根据国际检索系统网站公告和中国科学技术期刊编辑学会国际交流工作委员会通知,《海洋测绘》期刊已被日本《日本科学技术振兴机构数据库》收录。本刊自1981年创刊以来,先后被国内的《中国学术期刊综合评价数据库》、《中国核心期刊(遴选)数据库》、《中国科学引文数据库》、《中国期刊全文数据库》、《中文科技期刊数据库》、《全国测绘科技信息网》、《中国科技论文在线》和国际的俄罗斯《文摘杂志》、美国《艾博思科数据库》、《乌利希期刊指南》等收录。由于     

《海洋测绘》被日本《日本科学技术振兴机构数据库》收录

<正>日前,根据国际检索系统网站公告和中国科学技术期刊编辑学会国际交流工作委员会通知,《海洋测绘》期刊已被日本《日本科学技术振兴机构数据库》收录。本刊自1981年创刊以来,先后被国内的《中国学术期刊综合评价数据库》、《中国核心期刊(遴选)数据库》、《中国科学引文数据库》、《中国期刊全文数据库》、《中文科技期刊数据库》、《全国测绘科技信息网》、《中国科技论文在线》和国际的俄罗斯《文摘杂志》、美国《艾博思科数据库》、《乌利希期刊指南》等收录。由于     

《热带海洋学报》征稿简则

<正>《热带海洋学报》是由中国科学院南海海洋研究所主办、科学出版社出版、国内外公开发行的海洋学综合学术刊物,是我国自然科学核心期刊之一,是《中国学术期刊综合评价数据库》、《中国科学引文数据库》、《万方数据——数字化期刊群》来源期刊,已为《中国学术期刊(光盘版)》和《中国期刊网》全文收录,并已入选中国期刊方阵;同时还被     

依法开展海岛保护 认真履行管理职责

<正>一、提高对实施《海岛保护法》重大意义的认识《中华人民共和国海岛保护法》(以下简称《海岛保护法》)是继《中华人民共和国海域使用管理法》之后我国出台的有关海洋管理的又一部重要法律,《海岛     

《海洋测绘》被日本《日本科学技术振兴机构数据库》收录

<正>日前,根据国际检索系统网站公告和中国科学技术期刊编辑学会国际交流工作委员会通知,《海洋测绘》期刊已被日本《日本科学技术振兴机构数据库》收录。本刊自1981年创刊以来,先后被国内的《中国学术期刊综合评价数据库》、《中国核心期刊(遴选)数据库》、《中国科学引文数据库》、《中国期刊全文数据库》、《中文科技期刊数据库》、《全国测绘科技信息网》、《中国科技论文在线》和国际的俄罗斯《文摘杂志》、美国《艾博思科数据库》以及美国《乌利希期刊指南》等收录。由于本刊论文质量的逐步提升,不     

海洋之歌——我国首张海洋歌曲专辑录制侧记

从小喜欢鱼的林萍高歌起《重返海洋》;生长在青岛的江涛呼唤《大海,永远的朋友》;从《黄河源头》走来的张迈这次《走进蔚蓝》;屠梅华愿意与大家《共享大海》;《楼兰姑娘》俞静则憧憬着《迎接海洋世纪》……近日在北京百花录音棚,一批词曲作家和歌星汇集在这里,为建国以来首张海洋歌曲专辑紧张录制。这张专辑汇集了刚刚结束的“南麂杯”全国海洋歌曲征集的一、二、三等奖和特别奖的作品12首。这12首歌是从2000多首参评作品中脱颖而出的。     

《海洋测绘》被美国《斯蒂芬斯全文数据库》收录

<正>2015年8月8日,《海洋测绘》编辑部接到美国《斯蒂芬斯全文数据库》(EBSCO)文献库通知,《海洋测绘》通过美国EBSCO业务部门的遴选和评审,被全文收录于EBSCO大型文献库系统,并将在短时间内通过该系统发行至世界各国。这是《海洋测绘》继被俄罗斯《文摘杂志》和美国《乌利希期刊指南》等收录之后,再一次被国际著名检索系统收录,标志着《海洋测绘》的学术质量和影响力     

16项测绘地理信息标准通过审查

<正>7月2日,国家测绘地理信息局标准化工作委员会在西安组织召开标准审查会,由国家测绘标准化研究所承担的16项测绘地理信息标准通过审查。这些标准包括强制性国家标准《国家基本比例尺地图测绘基本技术规定》,推荐性国家标准《国家基本比例尺地图图示地形图图式》、《国家基本比例尺地图正射影像地图》、《国家基本比例尺地图地形图》、《数字城市地理信息公共平台运行服务质量规范》,行业标准《数字表面模型航天摄影测量生产技术规范》、《基础地理信息数字产品1∶50000数字表面模型》等。     

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.