- 更多网络例句与黑潮相关的网络例句 [注：此内容来源于网络，仅供参考]
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The process of the anticyclonic eddy breaking off from the Kuroshio bend is closely related with the increase of the cyclonic eddy at the southern part of the Kuroshio bend.
反气旋涡从黑潮弯曲中脱落的过程和黑潮弯曲南部气旋涡的增长密切相关。
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The results show that: There exists the Kuroshio deformation in the form of the Kuroshio bend at Luzon Strait. The degree of this bend varies with time and is accompanied by the anticyclonic eddy shedding from the Kuroshio bend.
研究表明：吕宋海峡处黑潮形变以黑潮弯曲的形式存在，黑潮弯曲程度随时间变化，并伴随反气旋涡从黑潮弯曲中脱落。
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The re sults show that: the SCS branch of the Kuroshio Current is an important part in the north SCS from Jan. to Dec.; there always exists a large-scale anticyclonic warm vortex on the right of the Kuroshio Current in the whole year.
模拟结果表明：1～12月，黑潮南海分支是南海北部的一支重要海流；黑潮右侧的大尺度反气旋性暖涡全年都存在。
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The dominant mechanism of the periodical variation of the Kuroshio bend and the breaking off of anticyclonic eddies is the frontal instability.
非线性平流作用是吕宋海峡黑潮弯曲发生周期性变化的主要原因，吕宋海峡黑潮锋附近的锋面不稳定机制是决定黑潮弯曲周期性变化及反气旋涡从黑潮弯曲中脱落的主要物理机制。
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There may be anticyclonic eddies separating from the loop and then entering the SCS; 3 There is only the Kuroshio front, bending slightly to the SCS, and the Kuroshio does not directly enter the SCS.
目前国内外对该问题的研究有三种不同的观点：1黑潮以分支的形式深入南海；2黑潮以流套的形式进入南海，并有涡旋从黑潮主体中分离后进入南海；3在吕宋海峡处黑潮锋向南海弯曲，但没有明显的黑潮分支进入南海。
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By using the NCEP reanalysis data to run POM, the basical characteristics of the Kuroshio Current, the large-scale anticyclonic warm vortex on the right of it, and the SCS warm current are well simulated. The feature of the great influence of the monsoon on the SCS currents is also shown.
4使用NCEP再分析资料驱动区域海洋模式POM，较好地模拟出了黑潮海流、黑潮右侧的大尺度反气旋性暖涡及南海暖流等海流的基本特征，并反映出南海海流受季风影响较大的特点。
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Based on the former studies, this paper promotes an innovation about this topic using new satellite altimetry data and hydrographic data along with numerical experiments: Firstly, the temporal variation of the deformation of Kuroshio accompanied by the periodically shed anticyclonic eddies from the Kuroshio bend is discovered; Secondly, the major mechanism of the anticyclonic eddy separating from the Kuroshio bend, which is the frontal instability, is brought forward and then proved; Thirdly, the factors with important impact on the periodical variation of the Kuroshio bend and the eddy shedding, which are the strength of the Kuroshio transport and the circulation in the winter SCS, are determined.
本文在前人工作的基础上，利用了最新的卫星遥感资料和海洋调查资料，通过数值模式的数值实验，得到了以下前人没有得到的创新成果：发现在吕宋海峡处黑潮的形变随时间变化，并伴有反气旋涡周期性地从黑潮主体中脱落；提出并证明了吕宋海峡黑潮锋附近的锋面不稳定是反气旋涡从黑潮弯曲中脱落的主要机制；确定了对黑潮弯曲周期性变化以及反气旋涡脱落有重要影响的物理因素是黑潮流量的大小及冬季南海局地环流。
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Based on the analyses of the observation data and numerical model of ocean circulation, the variations of the Kuroshio in Luzon strait (included Bashi strait and Balintang strait) have been studied by using the theories of potential vorticity conservation and oceanic Rossby wave; It was first discovered that the climatologic mean state of the Kuroshio exhibits a westward bending through the Luzon strait. The location of the Kuroshio bending is limited to the east of 119E and frequently flanked by a cold eddy to southwest of the Kuroshio; This bending of the Kuroshio favors the formation of the anticycle eddy in the east of the Luzon strait.
依据对海洋观测资料的分析，运用位涡守恒，海洋Rossby波动理论和数值模式，研究了黑潮在吕宋海峡（包括巴士海峡和巴林塘海峡）的形变特征；首次确定了在吕宋海峡黑潮的形变的平均状态是黑潮向南海的弯曲，该弯曲西端位置一般不超过119E，该弯曲的西南侧常常出现冷涡；该弯曲有利于吕宋海峡东侧形成一个反气旋涡旋。
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The study of the deformation of Kuroshio is an instructive complementarity to the theory of the western boundary current.
吕宋海峡深度约2500m，宽度跨越3 个纬度，是黑潮沿太平洋西边界北上途中遇到的一个明显的边界豁口，在这里黑潮失去陆坡支持而发生一系列动力学和运动学性质的改变，我们称其为黑潮的形变。
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However, this does not disprove that short changes in intensity or direction of the Kuroshio ever occurred at certain short cooling events. The 10Be minimum during the Younger Dryas event may indicate that the Kuroshio had been once greatly weakened or even terminated in the Okinawa Trough area which could be related to the response of the Pacific Ocean to the Younger Dryas. The 10Be and 9Be in surface sediment show totally different distribution patterns. The 10Be distribution is dominated by the input from Kuroshio and its branch, the Yellow Sea Current, whereas 9Be is mainly influenced by terrestrial input of suspended materials from the Yellow River discharge and deposited in the fine-grain size sediment zone southwest of the island of Jeju. Both 10Be and 9Be distribution patterns are different from anthropogenic pollutants such as heavy metal Pb which is dominantly distributed closely to the coastal areas.
冰期时冲绳海槽北部10Be的沉积通量远远高于太平洋大洋海区，充分反映了黑潮的传送带作用和边缘海的聚焦沉积作用，并表明末次冰期时在千年尺度上黑潮仍流经冲绳海槽，且强度并未减弱。10Be的通量在新仙女木时降到整个岩芯所跨时期的最低点，甚至低于10Be的现代大气平均生产率，因此推测在新仙女木事件时，黑潮的变动特别大，有可能改向或断流。
- 更多网络解释与黑潮相关的网络解释 [注：此内容来源于网络，仅供参考]
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Kuroshio：黑潮黑潮黑潮
Krarupcable 连续加感电缆 | Kuroshio 黑潮黑潮黑潮 | KuweitGlobalTankersCompany 科威特环球油轮公司
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Kuroshio current：黑潮
1336年,他的父母--张翠山和殷素素--被抢走屠龙刀的谢逊挟持着乘船出海,因为遭遇暴风雨而被黑潮(黑潮(Kuroshio Current)为西太平洋最大的洋流,从菲律宾流到北极海域)裹挟,越过日本以东洋面,带到白令海上.
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Kuroshio Extension：黑潮尾
黑潮反流 Kuroshio countercurrent | 黑潮尾 Kuroshio extension | 黑潮系 Kuroshio system
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Kuroshio Extension：黑潮尾流
克立维药风 kriva | 黑潮反流 Kuroshio countercurrent | 黑潮尾流 Kuroshio extension
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Kuroshio countercurrent：黑潮反流
黑潮 Kuroshio | 黑潮反流 Kuroshio countercurrent | 黑潮尾 Kuroshio extension
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Kuroshio system：黑潮系
黑潮反流 Kuroshio countercurrent | 黑潮尾 Kuroshio extension | 黑潮系 Kuroshio system
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Kuroshio region：黑潮区域
Kuroshio current;黑潮;; | Kuroshio region;黑潮区域;; | Kurtosis;峰度;;
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black current：黑潮
black conical shape 黑色锥形号型 | black current 黑潮 | black current 黑潮黑潮
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black current：黑潮黑潮
black current 黑潮 | black current 黑潮黑潮 | black diamond 煤
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japan current：黑潮黑潮
Japan Container Service 日本集装箱公司 | Japan current 黑潮黑潮 | Japan Electro-Technical Committee 日本电工委员会