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indonesian waters
相关语句
  印度尼西亚海域
     Analysis and Discussion on trawlnet used by fishing vessels of China in Indonesian waters
     对印度尼西亚海域中国渔船使用拖网渔具的分析和探讨
短句来源
     The calculation shows that the mean volume,heat and salt transports through the study area are 5.2Sv(1Sv=1×10 6m 3·s -1 ),0.57PW(1PW=1×10 15 W)and 184 Gg·s -1 ,respectively,with the flow being directed toward the Indonesian waters and eventually entering the Indian Ocean. These transports account for around 1/4 of the corresponding transports of the Indonesian Throughflow.
     计算得出 ,穿过研究海域流向印度尼西亚海域 ,最终流向印度洋的年平均体积、热量和盐量输运分别为 5 .2Sv( 1Sv =1× 1 0 6m3·s- 1 )、0 .5 7PW和 1 84Gg·s- 1 ,大约占印度尼西亚贯穿流相应输运量的 1 / 4。
短句来源
  “indonesian waters”译为未确定词的双语例句
     Once more discussion on trawlnet used by China's fishing vessels in Indonesian waters
     对印尼阿拉弗拉海中国底拖网的再讨论
短句来源
     A current flows through the Luzon Strait to enter the South China Sea to form a cyclonic circulation, and then flows into the Indonesian waters through the passages of the southern South China Sea.
     在吕宋海峡有海水进入南海,在南海形成一个气旋式流圈,进而通过南海南部水道流入印度尼西亚海。
短句来源
  相似匹配句对
     Waters.
     Waters二值最大覆盖算法的推广。
短句来源
     Analysis and Discussion on trawlnet used by fishing vessels of China in Indonesian waters
     对印度尼西亚海域中国渔船使用拖网渔具的分析和探讨
短句来源
     Once more discussion on trawlnet used by China's fishing vessels in Indonesian waters
     对印尼阿拉弗拉海中国底拖网的再讨论
短句来源
     Poets with hills and waters
     山光水色与诗人——谈中国山水及山水诗人
短句来源
     The Indonesian Film Status
     印度尼西亚电影现状
短句来源
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  indonesian waters
A detailed account of the second coelacanth specimen known to have been captured in Indonesian waters is provided.
      
An Account of the First Living Coelacanth known to Scientists from Indonesian Waters
      
Three new species of Pontella (Copepoda, Calanoida) from Indonesian waters, with notes on their species-groups
      
coggeri Kharin, 1984 were found in Fijian and Indonesian waters.
      
This was tested during a trial deployment in the vicinity of Indonesian waters in early 2000.
      
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The water volume,heat and salt transports between the Southern South China Sea and its adjacent waters are estimated from the simulated results of a high resolution(1/6°)numerical circulation model of the Pacific Asian marginal seas.The contribution of these transports to the Indonesian Throughflow is also evaluated.The study area covers the entire Southern South China Sea from 0° to 14°N.The calculation shows that the mean volume,heat and salt transports through the study area are 5.2Sv(1Sv=1×10...

The water volume,heat and salt transports between the Southern South China Sea and its adjacent waters are estimated from the simulated results of a high resolution(1/6°)numerical circulation model of the Pacific Asian marginal seas.The contribution of these transports to the Indonesian Throughflow is also evaluated.The study area covers the entire Southern South China Sea from 0° to 14°N.The calculation shows that the mean volume,heat and salt transports through the study area are 5.2Sv(1Sv=1×10 6m 3·s -1 ),0.57PW(1PW=1×10 15 W)and 184 Gg·s -1 ,respectively,with the flow being directed toward the Indonesian waters and eventually entering the Indian Ocean.These transports account for around 1/4 of the corresponding transports of the Indonesian Throughflow.The results indicate that the South China Sea is an important passage of the Great Ocean Conveyor,the most important global thermohaline circulation belt.Among the passway for water to flow from the South China Sea to the Indonesian area the Karimata Strait is the most important,followed by subsequently the Balabac,Mindoro and Malacca Straits.More intense southward transports mainly occur in winter and autumn,while in later spring and summer the total transports are towards the north.As revealed by the calculation of heat balance,the heat entering the study area is less than that leaving the study area by an amount of 0.064PW, implying that the mean net heat flux through the sea surface is about 30 W·m -2 ,from the atmosphere to the ocean.

根据中国近海高分辨率 ( 1 / 6°)环流模式的模拟结果 ,计算了南沙邻近海域与外海之间的海水体积、热量和盐量输运及其对印度尼西亚贯穿流的贡献。研究海域为 0°— 1 4°N的整个南海南部海域。计算得出 ,穿过研究海域流向印度尼西亚海域 ,最终流向印度洋的年平均体积、热量和盐量输运分别为 5 .2Sv( 1Sv =1× 1 0 6m3·s- 1 )、0 .5 7PW和 1 84Gg·s- 1 ,大约占印度尼西亚贯穿流相应输运量的 1 / 4。这一结果表明南海是全球大传送带这一全球海洋最主要热盐环流系统的重要通道之一。从南海流向印度尼西亚海域的通道以卡里马塔海峡为最主要 ,以下依次为巴拉巴克海峡、民都洛海峡和马六甲海峡。大的南向通量主要发生在冬、秋季 ,春末夏初总的通量向北。计算还得出输入本海区的热输运量比输出少 0 .0 64PW ,由这一结果推得 ,通过海 -气界面由大气进入海洋的年平均净热通量约为 30W·m- 2 。

This paper deals with the trawlnets used by fishing vessels of China in Indonesian waters. Based on the dimension,shrinkage and construction of the trawlnets,an analysis and discussion on the performance of this fishing gear are made.It shows that this kind of trawlnet is well suitable for catching hairtail in shallow waters,but the ropes of some sections are unsuitable to dispose,and the net in contact with sea bottom does not reach to the optimum condition. The reform in some parts of the net may...

This paper deals with the trawlnets used by fishing vessels of China in Indonesian waters. Based on the dimension,shrinkage and construction of the trawlnets,an analysis and discussion on the performance of this fishing gear are made.It shows that this kind of trawlnet is well suitable for catching hairtail in shallow waters,but the ropes of some sections are unsuitable to dispose,and the net in contact with sea bottom does not reach to the optimum condition. The reform in some parts of the net may lead to sensitive reactions due to the large mesh. In order to increase some high quality fishes,trawling speed should be raised in futtre reform of the net.

本文探讨了中国渔船在印度尼西亚海域使用的拖网渔具 ,从渔具使用规格、缩结状态和结构等方面进行了分析 ,指出这类渔具在浅水渔场捕捞带鱼时有良好适应性 ,但局部配纲不当 ,网具贴底程度未达到最佳状态。由于网目大 ,有些局部改革可能导致敏感的负面反应。作者认为 ,这类网具今后的改革应着眼于提高拖速 ,以增加对某些优质鱼的兼捕比例

Based on the Modular Ocean Model(MOM) of GFDL, a global diagnostic model is established to study the world ocean circulation, the model has a horizontal resolution of 1 °×1 ° and 21 vertical (levels), and the integrated time length is 11 years. The water depth data for the model are taken from DBDB5 data of National Geodetic Center, Boulder, Colorado, the temperature and salinity data are taken from Levitus(1994) data, and the sea surface wind stress data are taken from Hellerman and Rosenstein(1983) data. It...

Based on the Modular Ocean Model(MOM) of GFDL, a global diagnostic model is established to study the world ocean circulation, the model has a horizontal resolution of 1 °×1 ° and 21 vertical (levels), and the integrated time length is 11 years. The water depth data for the model are taken from DBDB5 data of National Geodetic Center, Boulder, Colorado, the temperature and salinity data are taken from Levitus(1994) data, and the sea surface wind stress data are taken from Hellerman and Rosenstein(1983) data. It is shown from the simulated results that the main circulation systems in the world ocean have been represented. The subtropic gyre in the North Pacific is reasonably simulated with the maximum transport of more than 50 Sv. The North Equatorial Current splits off into two branches at about 12 °N, the north branch forms the origin of the Kuroshio, the south branch is the Mindanao Current, and the Mindanao Cold Eddy east of the Mindanao Current is fairly reproduced. A current flows through the Luzon Strait to enter the South China Sea to form a cyclonic circulation, and then flows into the Indonesian waters through the passages of the southern South China Sea. The simulated results indicate that the Antarctic Circumpolar Current and the Kuroshio can go down to the bottom layer, but the Gulf Stream cannot, and there is a southward deep current at depths of 1000 to 2000m beneath the Gulf Stream, which indicates the southward movement of the North Atlantic Deep Water.

基于GFDL的MOM模式建立一个全球大洋环流的诊断模式(Robustdiagnosticmodel)来研究全球大洋环流。水平空间分辨率1°×1°。垂向分为21层。分别进行月平均和年平均模拟,积分的时间长度为11a。模式水流来自DBDB5(NationalGeodeticCenter,Boulder,Colorado)。所用的温度、盐度数据根据Levitus(1994)的资料,表面风应力根据HellermanandRosenstein(1983)的全球风场数据插值而来。从模拟结果看,全球大洋中的主要环流结构均得到体现。北太平洋副热带流圈得到合理的模拟,其最大的输运超过50Sv。北赤道流在12°N附近分为南北两支。北支形成黑潮,而南支为棉兰老海流,在其东边,棉兰老冷涡得到很好的再现。在吕宋海峡有海水进入南海,在南海形成一个气旋式流圈,进而通过南海南部水道流入印度尼西亚海。模拟结果表明南极绕极流和黑潮可以深达底层。湾流则不能深达底层,其下方在1000~2000m深度存在南向的深层流,显示了大西洋深层水的流动。

 
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