kuroshio造句

• In winter when the kuroshio is wormer than the normal , the situation is different
  当黑潮海温暖异常时，形势相反。
• The branch of kuroshio is the direct dynamic factor of the formation of this eddy
  黑潮分支大约是该涡旋的主要动力因子。
• Tosa kuroshio railway
  土佐黑潮铁道
• On the continental shelf , left of kuroshio ( 125 . 3e , 28 . 5n ) , there exists a large cyclonic eddy
  5叩）存在一个大型的气旋式涡旋。
• Theirconveyor belt was the kuroshio ( black ) current , named after the deep colour ofits waters
  他们的“传送带”是黑潮? ?因其水流颜色而得名。
• ( 3 ) the previously winter kuroshio ssta relates greatly to the east asian summer monsoon ( easm )
  ( 3 )前期冬季黑潮区域海温异常与东亚夏季风存在显著的联系。
• From the pictures of the three - dimensional current system , we can see that the magnitude of the kuroshio current minishes as it deepens
  从三维流场图可以看出，黑潮的强度随深度明显地减弱。
• Conclusions are drawn as follows : ( 1 ) there is a closely relationship between the autumn kuroshio ssta and the east asian winter monsoon ( eawm )
  ( 1 )秋季黑潮区域海温异常与东亚冬季风有明显的正相关关系。
• 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，黑潮海流把高咸度的温暖海水由太平洋经吕宋海峡带入本港。
• An anticlockwise gyre near the kuroshio north of japan inland is simulated using a high - resolution topography
  在高分辨的地形条件下，日本西海岸外侧的黑潮北部存在一逆时针漩涡，这可能与该区域的漏斗型地形诱导有关。
• South china sea gain heat by yearly average with 58wm - 2 . a maximum of heat loss exists in kuroshio area and it can get - 330 wm - 2 in december
  在黑潮流区存在最大的净热通量损失值区，在冬季12月份最大损失值可达- 300wm ~ ( - 2 ) 。
• By using of eof analysis , distribution of sst over the kuroshio area during winter are identified , which show cold or warm anomaly
  本文首先通过eof分析确定了冬季黑潮区sst的主要分布形势，发现冬季黑潮区海温主要表现为冷异常或暖异常。
• 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
  黑潮海流的大海盛产大龙虾和黑边石斑鱼，用它们做成的酱汤和龟肉料理等，都值得一尝。
• By use of the observational and numerical methods , the interaction of kuroshio ssta and the east asian monsoon are studied in this paper
  本文利用统计分析和数值模拟的方法研究了黑潮区域海温异常与东亚季风之间的相互作用，得到了以下结论。
• The analytical result showed that , the width of kuroshio in the middle part became wider from south to north , and the velocity increased , and the depth of the core became shallow
  分析结果表明，中段黑潮流幅山南至北增宽，流速变大，流核所达深度变浅。
• Results of the eof and correlation analyses showed that the climatological shifts were primarily influenced by the variability of the kuroshio with period longer than 40 years
  Eof分解和相关分析表明，该气候跃变主要受黑潮的影响，自60年代以来呈上升趋势。
• The results show that , the kuroshio flows along the continental slope of the east china seas , its trajectory varies along with the slope topography , and some eddies appear on the both sides of it
  数值模拟和数值实验的结果表明，黑潮在流经东海时沿东海陆坡流动，在其两侧出现一些涡旋。
• The results show that kuroshio intrudes onto the continental shelf of east china sea in large scale and during its flow water is exchanged ceaselessly with outer sea along ryukyu island
  模拟结果表明黑潮在东海陆架有大规模的入侵，其在沿东海陆坡流动途中沿着冲绳岛与外海不断的进行水体交换。
• In the northeast continental shelf in ecs , the kuroshio intruded towards north in several branches in winter , while in summer , the kuroshio intruded the northern shelf through continental marginal flow
  东海东北部陆架海域冬季黑潮以其分支形式向北入侵，夏季则主要以大陆边缘流的形式向北进入陆架。
• For a full meal experience , we recommend hachijojima s various set menus , including the runin , the kuroshio , and the oshamen . there is only one restaurant in kashidate that serves these home - style menus
  建议饮食行家们可在这里品味一下流人定食套餐、黑潮定食套餐、御赦免定食套餐等八丈独特的料理。