kuroshio extension meaning in Chinese
黑潮续流
Examples
- The result shows the volume transport in the four sections have the maximum in summer and the minimum in winter , especially in the two sections of 140 band 170 e . the eddy structure in both sides of the kuroshio extension is another distinct character
结果表明:穿过这四个断面的流量均呈现夏大冬小的季节变化趋势，其中140 “ e和170 “ e两个断面的季节变化比较明显。黑潮延续体另一显著特征是主轴南北两侧的多涡结构。 - The velocity varies from 61 . 5cm / s ( maximum ) in june to 48 . 1cm / s ( minimum ) in march in the kuroshio extension , and the extreme appear at the position of the first meander . the extreme minish , and the month and position of the extreme change accordingly as it deepens
黑潮延续体的表层流速最大值则由6月份的61 . 5cm / s (最大值)变化到3月份的48 . 1cm / s (最小值) ，极值则出现在黑潮延续体西段大弯曲路径的第一个峰处。 - South of japan , the kuroshio path of maximal velocity is outside the other three seasons in winter . in the kuroshio extension , the two points of the lee - wave also shows seasonal variabilities , and the path is most winding in summer , straight in fall
黑潮延续体最大流速主轴在西段的第一个峰处，冬季的峰值点比其它各季向东移了一个经度；第二个峰处，则以夏季弯曲最为平缓，且在155 e附近有一个向南的小弯曲路径。 - Based on the u . s . navy generalized digital environmental model ( gdem ) climatological temperature and salinity data on a 0 . 5 x 0 . 5 grid , the three - dimensional current system in the kuroshio south of japan and kuroshio extension is determined and analyzed by using the p - vector method
本文选用美国海军gdem全球气候月平均温盐资料，空间分辨率为0 . 5 0 . 5 ，应用p矢量方法对日本以南黑潮和黑潮延续体三维流场进行了诊断计算和分析研究。 - The kuroshio meander south of japan and the two lee - wave meanders in the kuroshio extension are well presented by the p - vector method . the path of the kuroshio meander , the position of the meanders in the kuroshio extension , the bifurcation of the kuroshio extension and the width of the current display seasonal variation evidently
日本以南黑潮弯曲路径呈一“ v ”字型，黑潮延续体西段的大弯曲路径呈现一“ m ”字型，即“两峰一谷”的弯曲形态，两峰分别位于144 e和150 e ，且弯曲程度和弯曲位置都呈现较明显的季节变化。