kuroshio extension 中文意思是什麼
kuroshio extension
解釋
黑潮續流-
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
結果表明:穿過這四個斷面的流量均呈現夏大冬小的季節變化趨勢，其中140 「 e和170 「 e兩個斷面的季節變化比較明顯。黑潮延續體另一顯著特徵是主軸南北兩側的多渦結構。 -
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
黑潮延續體的表層流速最大值則由6月份的61 . 5cm / s （最大值）變化到3月份的48 . 1cm / s （最小值） ，極值則出現在黑潮延續體西段大彎曲路徑的第一個峰處。 -
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
黑潮延續體最大流速主軸在西段的第一個峰處，冬季的峰值點比其它各季向東移了一個經度；第二個峰處，則以夏季彎曲最為平緩，且在155 e附近有一個向南的小彎曲路徑。 -
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
本文選用美國海軍gdem全球氣候月平均溫鹽資料，空間解析度為0 . 5 0 . 5 ，應用p矢量方法對日本以南黑潮和黑潮延續體三維流場進行了診斷計算和分析研究。 -
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
日本以南黑潮彎曲路徑呈一「 v 」字型，黑潮延續體西段的大彎曲路徑呈現一「 m 」字型，即「兩峰一谷」的彎曲形態，兩峰分別位於144 e和150 e ，且彎曲程度和彎曲位置都呈現較明顯的季節變化。
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