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Home > chinese-english > "热带季风" in English

English translation for "热带季风"

tropical monsoons

Related Translations:
热带季风气候:  tropical mo oon climatetropical monsoon climatetropical monsson climatetropicalmo oonclimate
热带季风林:  tropical monsoon forest
Example Sentences:
1.Territory area belongs to tropical monsoon climate about 67 . 660000 square kilometers , mainly with mountainous region , plain and hills
国土面积约67 . 66万平方公里,以山地、平原、丘陵为主,属热带季风气候。
2.It belongs to subtropical monsoon climate , and is adapted for the bamboo growing , and which is the important district for bamboo growing in china
这? ? ? ?热带季风气候?十分适宜毛竹生长?是国内重点毛竹生产区。
3.Climate : this zone mostly belongs to the subtropical monsoon climate , where four seasons are distinguishable , mild climate , winter is not too cold , summer is not too hot , rain fall is abundant
气候:大多属于中亚热带季风湿润气候,四季分明,气候温和,冬无严寒,夏无酷暑,雨量充沛。
4.The institute s major initiative , a laboratory for tropical monsoon environmental remote sensing , is a groundbreaking , state - of - the - art , comprehensive laboratory in geoinformation and earth sciences
由研究所建议设立的热带季风环境遥感实验室,更是一所创新而又具备尖端科技的地球信息和地球科学综合实验室。
5.Abstract : characterized by a lower subtropical monsoon evergreen forest as the zonal vegetation , guangdong province has a rich diversity in community structure and forest stratification , as well as abundant groundcover plants species
摘要:广东地带性植被为南亚热带季风常绿阔叶林,群落结构和层次都很丰富,处于林木下层的地被植物资源也十分丰富。
6.( 3 ) when the heat source over the bay of bengal is abnormally strong ( weak ) , the sourthern asian high extends westward ( eastward ) , and the western pacific subtropical high extends eastward ( westward ) , and the indian summer monsoon is stronger ( weaker ) , and the eastern asian tropical summer monsoon is weaker ( stronger )
( 3 )当孟加拉湾热源异常强(弱)时,南亚高压偏西(东) ,西太平洋副热带高压位置偏东(西) ;印度夏季风偏强(弱) ,东亚热带季风偏弱(强) 。
7.When the heat source over the bay of bengal was abnormally strong ( weak ) , the southern asian high extended westward ( eastward ) , and the western pacific subtropical high extended eastward ( westward ) , and the indian summer monsoon was stronger ( weaker ) , and the eastern asian tropical summer monsoon was weaker ( stronger )
当孟加拉湾热源异常强(弱)时,南亚高压偏西(东) ,西太平洋副热带高压位置偏东(西) ;印度夏季风偏强(弱) ,东亚热带季风偏弱(强) 。
8.One is located in south china and south east inshore of china , mainly affected by the eastern asian tropical summer monsoon ; the other is located in shandong peninsula and liaodong peninsula and heilongjiang of china , mainly affected by the eastern asian subtropical summer monsoon
( 6 )夏季菲律宾热源异常强年,副热带高压异常偏北,中国雨区分为南北两个区域,一个位于华南、东南沿海,受东亚热带季风影响;另一个位于山东半岛、辽东半岛和黑龙江地区,受副热带季风的影响。
9.( 4 ) there exists obviously negative correlation between the heat source over the bay of bengal and the precipitation of the sourtn of the yangtze river and the parts of the east of south china in summer , and there exists obviously positive correlation between the heat source over the bay of bengal and the precipitation of the area from the sourth west in china to the west of south china
孟加拉湾热源异常对南亚高压、南亚季风、副热带高压的影响是显著的,对东亚热带季风的影响并不显著。 ( 4 )夏季孟加拉湾热源与同期长江以南、华南东部的部分地区的降水存在明显的负相关关系,而与西南到华南西部地区呈明显的正相关关系。
10.When the heat source over philippines is abnormally weak , the southern asian high becomes only one part and its location extends southward , the indian summer monsoon is stronger , the eastern asian tropical summer monsoon is weaker , and the western pacific subtropical high extends southward ; the influence of the heat source strong anomalies over philippines on the east part of the southern asian high and the western pacific subtropical high and the east asian tropical summer monsoon is significant and whic h on the indian summer monsoon is not significant ; the influence of the heat source weak anomalies over philippines on the east asian tropical summer monsoon and the indian summer monsoon and the western pacific subtropical high and the southern asian high is significant
东亚热带季风加强,南亚季风也有所加强,西太平洋副热带高压位置偏北;当夏季菲律宾热源异常减弱时,南亚高压只表现为一个部分,且位置偏南,南亚季风加强,东亚热带季风减弱,西太平洋副热带高压位置偏南。夏季菲律宾热源异常强年,东部的南亚高压异常显著,副热带高压位置异常偏北也达到显著水平,东亚热带季风的加强是显著的,而南亚季风的加强并不显著;而热源异常减弱时,东亚热带季风的减弱、南亚季风的加强都达到显著水平,副热带高压、南亚高压的位置异常偏南也是显著的。
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