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Home > english-chinese > "greenland sea" in Chinese

Chinese translation for "greenland sea"

格林兰岛
格陵兰海


Related Translations:
greenlands:  格林兰兹
greenland:  n.格林兰〔姓氏〕。n.格林兰(岛)〔丹麦〕。n.-er 格林兰人。adj.-ish
greenland res:  格林兰水库
greenland anticyclone:  格林兰反气旋格陵兰反气旋
greenland current:  格林兰海流格陵兰洋流
royal greenland:  皇家格陵兰鱼虾公司
greenland shark:  格陵兰鲨小头睡鲨
greenland high:  格林兰高压格陵兰高压
greenland basin:  格陵兰海盆
greenland garden:  翠林花园
Example Sentences:
1.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。
2.3 . 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。
3.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。
4.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。
5.( 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) 。
6.( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ) , and the low of the asian land is stronger ( weaker ) , which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ) , then the southeastern , warm and damp airflow towards the north china is stronger ( weaker ) , and the cold airflow of the high level over the north china is also stronger ( weaker ) , which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ) , while the sst of west wind drift is higher ( lower )
( 5 )春季格陵兰海冰面积偏大(小) :后期夏季日本海高压偏强(弱) ,而大陆上低压也偏强(弱) ,易(不易)形成西低东阻的形势;华北地区的上升运动增强(减弱) ;东亚夏季风偏强(弱) ,向华北地区输送的西南暖湿气流偏强(弱) ,而对应高空华北地区上空冷空气活动偏强(弱) ,利于(不利于)华北上空冷暖空气的交汇;夏季赤道东太平洋海温偏低(高) ,西风漂流区海温偏高(低) 。在以上的环流背景下,华北夏季降水偏多(少) ,易涝(旱) 。
7.In this paper , the spatial and temporal distribution of the summer rainfall of north china and the sea - ice extent of north arctic are firstly analyzed , by the way of svd we also analyze the correlation distribution pattern of the spring north arctic sea - ice and the summer rainfall of china , and find out that the key section of north arctic sea - ice is the greenland sea , then the climate characteristics of the spring greenland sea - ice are analyzed , at last we have discussed the infection of the spring greenland sea - ice on the summer rainfall of north china and its possible ways
本文首先分析了华北夏季降水和北极海冰面积的时空变化特征,并通过svd方法分析了春季北极海冰面积与中国夏季降水的相关分布型,确定出北极海冰的关键区格陵兰海,然后分析了春季格陵兰海冰变化的气候特征,最后讨论了春季格陵兰海冰对华北夏季降水的影响及其可能影响途径。
Similar Words:
"greenland halibut" Chinese translation, "greenland high" Chinese translation, "greenland iceland rise" Chinese translation, "greenland res" Chinese translation, "greenland right whale" Chinese translation, "greenland shark" Chinese translation, "greenland spar" Chinese translation, "greenland type glacier" Chinese translation, "greenland wentletrap" Chinese translation, "greenland-iceland rise" Chinese translation