monsoon trough中文是什么意思

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中文翻译
造句

季风槽
季风低压槽
季候风槽

monsoon n. 1.季(节)风〔在印度洋和亚洲南部5-9月自西南、 ...
trough n. 1.木盆；马槽，猪槽；承溜；水笕；洗矿槽。 2.( ...
monsoon n. 1.季(节)风〔在印度洋和亚洲南部5-9月自西南、10-12月自东北吹的风〕。 2.(印度的)雨季,夏季季风期。 the Indian monsoon 东亚季候风。 the dry [wet] monsoon 冬[夏]季季风；干[湿]季风。 a monsoon forest 季雨林。 the monsoon rain 季风雨。
trough n. 1.木盆；马槽，猪槽；承溜；水笕；洗矿槽。 2.(面包店的)揉面盆，面钵。 3.【航海】(深6000米以上的)深海漕；【电学】电槽 (＝ trough battery)；【物理学】波谷；【数学】凹点；【气象学】槽形低气压。 4.〔美剧〕脚光。 a pneumatic trough 集气槽。 a trough truck 油槽车。
asian monsoon 季风亚洲
breaking of monsoon 季风爆发
burst of the monsoon 季风爆发
burstof monsoon 季风爆发
burstof the monsoon 季风爆发
continental monsoon 大陆性季节风
dry monsoon 冬季风
equatorial monsoon 赤道季风
extratropical monsoon 中纬度气旋
global monsoon 异域采风
indian monsoon 印度季风; 尤季风
lightning monsoon 闪电季风
little monsoon 小季节风
monsoon air 季风气候; 季风气流
monsoon circulation 季风环流
monsoon climate 季风气候以干旱的冬; 气候
monsoon climatology 季风气候学
monsoon cloud 雨季云
monsoon cluster 季风云团
monsoon current 季风海流; 季风洋流
monsoon currents 季风洋流

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例句与用法

In june , 2004 , the rain - bearing monsoon trough spent less time near the south china coast , resulting in more sunshine and hence higher temperatures in hong kong
4度。由于带雨的季风槽在二四年六月份较少在华南沿岸附近出现，所以阳光较正常充沛，温度亦较高。
The monsoon trough also brought less than normal rainfall to hong kong in may and june . 2004 was the 17th driest year in hong kong since records began in 1884
五、六月份的季风槽为本港带来的雨量亦比正常偏少，这些因素令二四年成为自一八八四年有记录以来第17个最少雨的年份。
The southerly water vapor can progress to 50 n near north - east in china - , the southeasterly water vapor from south side of the west pacific subtropical high and north side of the monsoon trough can march westward to 100 e near south - east part of gansu in summer
东亚夏季偏南风水汽输送所能到达的北界为50 n附近的东北北部。西太平洋副高南侧、亚洲季风槽北侧的东南风水汽输送在夏季可向西扩展到甘肃东南部地区( 100 e附近) 。
When the tcf in nwp is high , the bengal bay cef which located at 90 e is strong and the new guinea cef located at 150 e is weak ; there is a anti - cyclonic circulation near the equator . the equatorial buffer zone is fortified : it is propitious to the equatorial anticyclones activated and push monsoon trough to higher latitude , this circulation pattern can promote the genesis of tc in nwp
多热带气旋年，位于90 e附近的孟加拉湾越赤道气流显著增强，而位于150 e附近的新几内亚越赤道气流异常偏弱；在赤道附近存在一个异常的反气旋性环流，赤道缓冲带较强，有利于赤道高压的活跃，季风槽被推向较高纬度，从而有利于热带气旋的生成。
As a result , we find that in winter when the kuroshio is cooler than the normal , at following summer , the continental cyclone deepen and the east asia monsoon strengthen , that the mid - latitude blocking high weaken and zonal circulation develop , the east asia teleconnection of " - + - " is stired up , so that subtropical high weaken and diminish , and tend to east north , tropical monsoon trough strengthen and mei - yu front weaken , and tend to north , meanwhile south asia high weaken and diminish , and tend to eastvnorth , is easy to form eastern region type
结果发现当黑潮海温冷异常时，后期夏季大陆热低压加深，东亚夏季风偏强。中纬度阻塞高压减弱，东亚地区纬向环流发展，在东亚-西太平洋地区激发“ - + - ”的东亚遥相关型，从而西太平洋副高强度偏弱，面积偏小，位置偏东、偏北，东亚梅雨锋也偏弱，季风槽则变强，位置偏北。同时南亚高压偏弱，位置偏北、偏东，易形成东部型。