kuroshio region meaning in English
黑潮区
Examples
- Finally the article discusses the physical mechanism of meridional and zonal wind field ' s effect on sst in kuroshio region and think that justly the adjustion of macro - dimension wind field connects the two facts
考虑到赤道中太平洋风场异常与el - nino及la - nina事件关系密切，进一步的研究证实el - nino及la - nina事件与黑潮海温异常有着密切的关系。 - On the other hand , the methods of reof analysis was also used to north pacific ssta on spring and summer . the middle and eastern equatorial pacific and the kuroshio region of northwestern pacific are two mostly anomaly regions
另一个方面，对太平洋春季、夏季海表温度进行reof分析，表明太平洋海表温度分布具有明显的区域特征，其中最强的异常分布区是赤道中东太平洋和西北太平洋黑潮海区。 - The well correlation times persist for about six months and the incidence level is reach or pass 0 . 01 . the meridional wind field which persistly impacting on sst in kuroshio region is near the west tropical pacafic . the result also behave as distinctly positive correlativity . afterwards we investigate the relationship between sst in kuroshio region and ninoc , 4 region and integrate the front conclusion . as a resultjt display that the sst in kuroshio region persists for positive relevance during the course of el - nino and inversely during the course of la - nina . subsequentl y the synthetic fields of kuroshio region ' s ssta in el - nino and la - nina years have proved the front outcome
对与黑潮海温异常变化关系密切的风场关键区及两者的相互关系研究表明：黑潮本身的风场和其源地北赤道流海域的风场异常对黑潮海温的影响仅限于同期及海温滞后1到2个月，而能持续影响黑潮海温异常的经向风场的关键区出现在赤道西太平洋( 140 - 160e ， 5s - 5n ) ，纬向的关键区则在赤道中太平洋( 160e - 150w ， 5s - 5n ) ，且纬向关键区的强度和范围均大于经向，两者对黑潮海温的影响均能持续六个月左右。 - Our conlusion is : during the coruse of the nov in el - nino year ( start from the westerly anomalous ) to apr of next year , it is just the intensity of east asian monsoon that influents the sst variety in kuroshio region . the heat flux is the bridge links the two facts . and the gene which affects winter monsoon is the pea circumfluence
分析还显示影响黑潮海温异常的主要机制有：由赤道中太平洋西风异常而产生的pea遥相关、夏季太阳辐射的加强、低纬向高纬暖水输送的增加及黑潮自身海表水的辐合。 - Further , correlation analysis is used to the summer rainfall and four seasonal north pacific ssta , the results suggest north pacific ssta which notability cause the summer rainfall anomaly over eastern china are prophase winter ssta of kuroshio region of northwestern pacific , prophase spring ssta of middle and eastern equatorial pacific and summer ssta of west wind drift region
进一步对上述东部夏季降水异常区夏季降水与春夏秋冬太平洋海温异常作相关分析，表明对中国东部夏季降水有显著影响是：西北太平洋黑潮海区前期冬季海温异常、赤道中东太平洋前期春季海温异常、中高纬太平洋西风漂流区同期夏季海温异常。