西风槽的英文

• westerly trough

• "西风"英文翻译    westerly wind; west wind
• "槽"英文翻译    trough; manger
• "西风" 英文翻译 :    westerly wind; west wind◇西风带 westerlies
• "背风槽" 英文翻译 :    lee trough
• "导风槽" 英文翻译 :    hot air path
• "东风槽" 英文翻译 :    easterly trough
• "焚风槽" 英文翻译 :    foehn trough
• "季风槽" 英文翻译 :    monsoon trough
• "进风槽" 英文翻译 :    air intake duct
• "通风槽" 英文翻译 :    vent gutter; ventilating slot; ventilation slot
• "偏西风 偏西风" 英文翻译 :    westerly wind
• "西风，西风带" 英文翻译 :    westerlies
• "大西风" 英文翻译 :    amasaki; asamaki
• "暖西风" 英文翻译 :    zephyr
• "偏西风" 英文翻译 :    westerly wind
• "强西风" 英文翻译 :    brave west winds
• "西风；向西" 英文翻译 :    wester
• "西风波" 英文翻译 :    westerly wave
• "西风带" 英文翻译 :    subpolar westerlies; subtropical westerlies; temperate westerlies; westerly belt; westerly winds; westerly zone; zonal westerlies; zonal winds
• "西风古" 英文翻译 :    redroot amaranth
• "西风流" 英文翻译 :    west-wind drift
• "西风龙" 英文翻译 :    zephyrosaurus
• "西风神" 英文翻译 :    zephyr
• "西风颂" 英文翻译 :    ode to the west wild; ode to the west wind
• "西风涡" 英文翻译 :    westerly vortex

• The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high , south asia high , low latitude systems , upper level jet ( ulj ) , low level greater wind speed axes , westerly trough and plateau trough , low level vortex , cold frontal , occluded front in qinghai lake , mesoscale low pressure , heat low - pressure in qinghai , shear line and convergence line , mesoscale cloud cluster , etc . the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area
  3 、西太平洋副高、南亚高压、低纬系统、高空急流、低空大风速轴；西风槽和高原槽、低涡、冷锋、青海湖锢囚锋以及中尺度低压、青海热低压、切变线与辐合线、中尺度云团等系统是高原东北部地区大到暴雨的主要相关系统。 100hpa上的南亚高压中心强度加强，位置东西摆动预示高原地区将有降水产生，中心强度减弱，降水过程结束。南亚高压西部副型是高原东北部地区大到暴雨的主要流型。
• While the precipitation of southeast of inner - mogolio is attributed as the strong convective precipitation , the rainfall of liaoning and northeast of heilongjiang is induced by subtropical high and westerly trough , and that of west of heilongjiang is influenced directly by vortex in upper air
  各区域产生极端降水的天气背景也不相同：内蒙古东南部的降水是前倾槽引起的强对流降水天气，辽宁和黑龙江东北部的降水是由于副热带高压和西风槽的共同作用引起的。黑龙江西部的降水是由于高空涡的直接作用引起的。
• The summer rainfall anomaly of north china is closely related to indian low , west pacific subtropical high , westerly troughs and ridges in mid - latitude , south asia high , subtropical monsoon circulation and cold air activity on the corresponding period , and similar circulation pattern also appears in the preceding spring
  结果表明： ( 1 )华北夏季降水异常与同期印度低压、西太平洋副高、中纬度西风槽脊、南亚高压、副热带季风环流和冷空气活动的异常都密切相关。华北夏季降水异常年春季的环流特征与夏季类似。
• The rsults are as follows : ( 1 ) precipitation shows the decreasing trend and remarkable interannual and interdecadal variations in flood season in the last 44 years . ( 2 ) precipitation anomalies in flood season have a good correlations with southwest and southeast summer monsoon , polar vortex , west wind trough , the subtropical high over west pacific and south asia high
  ( 2 )辽宁汛期水汽来源于西南夏季风和我国东部海域，汛期降水异常与低空的西南、东南夏季风、中空的极涡、西风槽、西太平洋副热带高压活动及高空的南亚高压关系密切。
• ( 4 ) flood season precipitation anomalies has a good correlations with southwest and southeast summer monsoon , polar vortex , west wind trough and west pacific high ( 5 ) the ssta anomalies of west pacific key regions combine with south atlantic key regions has a good predict to the flood season precipitation anomalies in liaoning areas
  辽宁夏季多雨水汽来源于西南夏季风和我国东部海域，汛期降水异常与西南、东南夏季风，极涡，西风槽以及西太平洋副高活动关系密切。西太平洋和南大西洋海温关键区冷暖水年结合对辽宁汛期多少雨年有很好的指示作用。
• In 1999 , the dipole existed in between the okhotsk high and the depression in the north of northeast china , thus the okhotsk high became active and maintained , the subh was located to an area quite further south than usual . the high persisted in the east region of nw china , the cold air flowed to the mid - lower reaches of the yangtze river along the high . in the east region of nw china , air steam under troposphere was strong sinking motion , and formatted the negative vorticity region , the vapour flux divergence was divgence . lt was apparently that the rain could n ' t occur in the eastern portin of nw china . in 2000 year , okhotsk high was very weak or did n ' t exist in , there was high in the east asia - japan , the subh is located to an area further north than usual . in the east region of nw china , the trough maintained , air stream under troposphere was strong ascending motion , the cycolonic circulation was prevailing , the vapour flux divergence was intensive convergences the rain easy happened in the east areas of northwest china
  4多梅雨1999年鄂霍茨克海阻塞高压与我国东北北部低压形成偶极子，使得阻塞高压稳定少动，西太副高位置偏南，西北地区东部持续受高压控制，冷空气沿此高压流经长江中下游地区上空；在西北地区东部对流层中下层气流下沉运动较强，呈反气旋涡度，水汽通量散度辐散，不利于西北地区东部降水。空梅雨2000年相反，鄂霍茨克海高压减弱甚至不存在，东亚-日本为高压，西太副高位置偏西偏北，西北地区东部处于西风槽中，对流层中下层气流上升运动增强，盛行低压环流，水汽通量散度强烈辐合，有利于降水生成。