格陵兰海 meaning in Chinese
greenland sea
greenlandsea
Examples
- The anomaly of greenland sea - ice area can affect sand - storm ' s occurrence times in ningxia ( north of china ) in later through affecting air circulation backgrounds
格陵兰海冰面积的异常变化通过影响后期的大气环流，从而影响于夏(我国北方)沙尘暴的发生。 - 3 . the correlations are significant between sea - ice area index of kara barents and greenland seas , which locate on the north of the continent of europe and asian , and spring sand - storm ' s occurrence times in ningxia
3 、宁夏春季沙尘暴发生次数与欧亚大陆北部的喀拉海、巴伦支海、格陵兰海冰面积指数之间有显著的相关关系。 - There is an evident decrease of the spring greenland sea - ice extent since the 1970s , especially from the 1980s to the 1990s . with the method of mann - kendall , we find that the spring greenland sea - ice extent clearly takes place a catastrophe around 1972
自二十世纪70年代以来，春季格陵兰海海冰面积有一明显的减少趋势，其中80年代至90年代这种减少趋势是十分显著的，由mann - kendall方法确定出春季格陵兰海冰面积在1972年发生突变。 - Based on sand - storm ' s occurrence times data in ningxia , arctic sea - ice area index data , height and wind fields data of ncar / ncar reanalysis , the basic variable rules and anomalous air circulation background fields of spring sand - storm ' s occurrence times in ningxia are systematically analyzed . more attention was paid on studying the tele - connections between arctic sea - ice areas and spring sand - storm ' s occurrence times in ningxia , and impossible affecting process of greenland sea - ice areas " anomalies on sand - storm ' s occurrence times . the results are as follows : 1
本文根据宁夏沙尘暴发生次数资料、北极海冰密集度资料和ncar / ncep再分析资料，较系统地分析了宁夏春季沙尘暴发生次数的基本变化规律及其异常的大气环流背景场，重点研究了北极海冰与宁夏春季沙尘暴发生次数之间的遥相关关系以及格陵兰海冰异常变化对沙尘暴的可能影响途径，结果表明： 1 、夏春季沙尘暴发生次数在1960 - 2000年有明显的年代际和年际变化特点，总体呈减少趋势，且在1984年发生了明显的突变，有10年和7年左右的周期。 - ( 3 ) by using the method of svd and its second spatial distribution pattern , we can find that there is an evident positive relationship between the spring greenland sea - ice extent and summer rainfall of north china , that is to say , if the spring sea - ice extent of greenland is larger ( smaller ) , then there is much more ( less ) summer rainfall in north china
( 3 )采用奇异值分解方法，由第二对空间分布型可以看出，春季格陵兰海冰与华北夏季降水存在明显的正相关关系，即春季格陵兰海冰面积偏大(小) ，则后期华北夏季降水偏多(少) 。