kuroshio current 中文意思是什麼
kuroshio current
解釋
黑潮暖流-
Theirconveyor belt was the kuroshio ( black ) current, named after the deep colour ofits waters
他們的「傳送帶」是黑潮? ?因其水流顏色而得名。 -
From the pictures of the three - dimensional current system, we can see that the magnitude of the kuroshio current minishes as it deepens
從三維流場圖可以看出，黑潮的強度隨深度明顯地減弱。 -
During the winter dry season, the kuroshio oceanic current brings warm water of high salinity from the pacific through the luzon strait
在乾旱的冬季，黑潮海流把高鹹度的溫暖海水由太平洋經呂宋海峽帶入本港。 -
They also make miso soup from the prawns and rockcod that swim on the kuroshio current. the taste of their dishes made with turtle meat is beyond compare
黑潮海流的大海盛產大龍蝦和黑邊石斑魚，用它們做成的醬湯和龜肉料理等，都值得一嘗。 -
By contrast, the eastern waters are more strongly influenced by oceanic currents, specifically the hainan current in the summer which flows from the south - west to the north - east and the kuroshio current in the winter which flows in the opposite direction
本港受到兩股主要海流的影響，夏季受到海南海流的影響由西南流至東南，而冬季則受到黑潮海流的影響流向相反。 -
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。 -
Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature
其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同，強冬季風使得黑潮與我國近海海洋過多散熱，海溫降低；在西北太平洋暖池北部，強冬季風引起西風異常，從而引發異常氣旋性環流，海水輻合下沉加熱其表層以下海水，同時異常環流使得更多東側異常暖水向西加熱其表層水；在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常，海水輻合下沉升溫。 -
A 3d baroclinc ocean model is used to model the ocean current around the kuroshio area on the condition of successively anomalous east asia winter monsoon, some significant results are obtained, and the influence of strong ( weak ) winter monsoon on sea surface height ( ssh ), sea surface temperature ( sst ) and sea current around the kuroshio area is analyzed preliminarily
摘要運用一個三維斜壓海洋模式對冬季風風場持續異常時期的黑潮區海洋進行了模擬，初步分析了冬季風風場持續異常對黑潮區海面高度、海流和海溫的影響。 -
The surface current velocity displays the seasonal variability, too. the velocity varies from 71. 6cm / s ( maximum ) in december to 55. 4cm / s ( minimum ) in may in the kuroshio south of japan, and the position 01 extreme appear to the south of kii peninsula
黑潮表層流速最大值同樣存在著季節性變化特徵：日本以南黑潮表層流速最大值由12月份的71 . 6cm / s （最大值）變化到5月份的55 . 4cm / s （最小值） ，極值均出現在紀伊半島以南海域。 -
It is indicated that, because of the strong influence of fluvial carbonates, the pco2 of surface water in the changjiang estuarine area and near the hangzhou bay were obviously higher than the pco2 of air ( especially in summer, autumn and winter ), while the pco2 in the mid east china sea was apparently lower than the atmospheric pco2. it is also shown that the pco2 in the southern east china sea, near the black ( kuroshio ) current, is higher than atmospheric pco2, especially in spring and summer
東海表層海水的pco :分佈大致有以下幾個特點:有明顯的空間和季節變化;長江口及杭州灣鄰近海域海水pco :明顯高於大氣pcoz ，尤其是在夏、秋、冬季尤為突出，表明有河流碳酸鹽系統的強烈影響;在東海中部有大片區域海水pco :顯著低於大氣pcoz ，在南部靠近黑潮的大片區域里，尤其是春、夏季節，海水的pco :高於大氣pc02 。
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