southwest monsoon中文是什么意思

• 蜗季风
• 西南季风

• "southwest"中文翻译    n. 1.西南〔泛指西南方向，或指正西以南45°；略作 ...
• "monsoon"中文翻译    n. 1.季(节)风〔在印度洋和亚洲南部5-9月自西南、 ...
• "monsoon" 中文翻译 :    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。
• "southwest" 中文翻译 :    n. 1.西南〔泛指西南方向，或指正西以南45°；略作 SW〕。 southwest by south 西南偏南〔即西南偏南11°15′；写为 S33°45′W〕。 southwest by west 西南偏西〔即西南偏西11°45′，写为 S56°15′W〕。 2.〔S-〕一国或一地区的西南部。 adj. 1.位于西南的；向西南的。 2.来自西南的。 a southwest wind 西南风。 adv. 在西南；向西南；从西南。
• "asian monsoon" 中文翻译 :    季风亚洲
• "breaking of monsoon" 中文翻译 :    季风爆发
• "burst of the monsoon" 中文翻译 :    季风爆发
• "burstof monsoon" 中文翻译 :    季风爆发
• "burstof the monsoon" 中文翻译 :    季风爆发
• "continental monsoon" 中文翻译 :    大陆性季节风
• "dry monsoon" 中文翻译 :    冬季风
• "equatorial monsoon" 中文翻译 :    赤道季风
• "extratropical monsoon" 中文翻译 :    中纬度气旋
• "global monsoon" 中文翻译 :    异域采风
• "indian monsoon" 中文翻译 :    印度季风; 尤季风
• "lightning monsoon" 中文翻译 :    闪电季风
• "little monsoon" 中文翻译 :    小季节风
• "monsoon air" 中文翻译 :    季风气候; 季风气流
• "monsoon circulation" 中文翻译 :    季风环流
• "monsoon climate" 中文翻译 :    季风气候 以干旱的冬; 气候
• "monsoon climatology" 中文翻译 :    季风气候学
• "monsoon cloud" 中文翻译 :    雨季云
• "monsoon cluster" 中文翻译 :    季风云团
• "monsoon current" 中文翻译 :    季风海流; 季风洋流
• "monsoon currents" 中文翻译 :    季风洋流

• While it ' s always hot and humid , the southwest monsoon period from may to november see the most rain and storms
  尽管那里终年湿热，但是降雨和风暴在5月至11月的西南季风期最为频繁。
• The northeast monsoon generally prevails over the coast of southern china in winter while the southwest monsoon dominates in summer
  在冬季华南沿岸常吹东北季候风而在夏季则常吹西南季候风。
• Under the influence of an active southwest monsoon , the weather remained unsettled with heavy rain and severe thunderstorms in july
  受活跃西南季候风影响，七月天气仍然不稳定，有大雨及强烈雷暴。
• The passing - obstructing effect led the southwest monsoon and the east asian monsoon meet around lrgr , which forced the rainfall distribution and spatial change present longitudinal features along the river
  纵向岭谷的这种“通道阻隔”效应使得西南季风和东南季风在区内交汇，并使区内夏季降水空间上及夏季降水的变化沿河流呈纵向分布。
• The west and the east of qinling mountains are being impacted by the southwest monsoon and the southeast monsoon at the same time , their response to the global and monsoon chang will be diffent , typical and sensitive ; on the other hand , the study on the two areas will contribute to the understandon the monsoon
  而秦岭东西部由于同时受到东亚季风与南业季风的影响，决定了它对全球气候的响应将更具典型性和代表性。同时，分析两地区气候与环境效应的变化并进行对比，这对于季风变化的研究也有很重要的意义。
• The positive load take absolutely advantage in the first spatial pattern of year and seasons . especially that the precipitation field load of winter is all positive . not in the southwest of china because of southwest monsoon etc . system ; the characteristics of the second spatial pattern are that most of the area is taken up by positive load in year and four seasons , the west of talimu basin is the center of negative load of the year , spring and autumn vector fields ; east of zhungeer basin is the center of positive load of the third spatial pattern of year , spring , summer and winter , the center of negative load is often in east of chaidamu basin , but the distribution center of autumn is in east of zhungeer basin ; the distribution of the fourth spatial pattern is difficult to describe and forms several centers of positive and negative load ; several centers of positive and negative load also appear , the distribution of load fields of the fifth spatial pattern of year , spring and winter represents the situation of " + , - , + " from southeast to northwest ; the complexity of the sixth spatial pattern is more stonger than that of the fourth and the fifth spatial pattern , several centers of load fields of year and each season often appears inverse situation of the positive and the negative load . but the centers are still most in zhungeer basin , chaidamu basin and talimu basin
  第一空间型中，年和四季都是正荷载占据绝对优势，特别是冬季降水场皆为正值，只是西南地区由于受西南季风等系统的影响，表现为与其它地区的不同；第二空间型的特点如下：年和四季分布皆为正荷载占据大部分区域，负荷载中心年、春季和秋季分布中都是位于塔里木盆地西部地区；第三空间型正荷载高值中心除秋季外都是处在准格尔盆地以东地区，负荷载中心多在柴达木盆地以东地区，秋季却处于准格尔盆地以东地区；第四空间型分布就较复杂无章法可言，形成多处正负荷载中心；第五空间型特征是这样的，同样是多个荷载中心出现，年、春季和冬季中的荷载场分布从东南到西北大体呈现“ + 、 - 、 + ”的特点；第六空间型分布的复杂程度较之第四、第五空间型更大，年和各季分布比较中多个荷载中心常出现正负相反的情况，但中心仍以柴达木盆地、准格尔盆地和塔里木盆地为主。