季风爆发的英文

• breaking of monsoon
• burn-out monsoon
• burst of the monsoon
• burstof monsoon
• burstof the monsoon

• "季风"英文翻译    monsoon
• "爆发"英文翻译    erupt; burst; break out; blo ...
• "西风爆发" 英文翻译 :    westerly wind burst
• "风爆" 英文翻译 :    windblast
• "季风" 英文翻译 :    [气象学] monsoon 冬季风 dry monsoon; 夏季风 wet monsoon; 季风气侯 monsoon climate; 季风区 monsoon region; 季风雨 monsoon rain; 季风云团 monsoon cluster
• "火风爆" 英文翻译 :    firestorm
• "爆发" 英文翻译 :    erupt; burst (out); break out; blow up; detonate; explode; flare up; outburst 火山爆发 volcanic eruption; 人群中爆发出一片欢呼声。 the crowd burst into cheers. 战争爆发。 the war broke out
• "红色风爆" 英文翻译 :    redwind
• "逆通风爆炸" 英文翻译 :    back draft explosion
• "冬季风" 英文翻译 :    dry monsoon
• "反季风" 英文翻译 :    antitrade wind; counter trade; counter-trades
• "季风槽" 英文翻译 :    monsoon trough
• "季风带" 英文翻译 :    monsoon zone
• "季风林" 英文翻译 :    mo oon forest; mo oonforest; monsoon forest
• "季风流" 英文翻译 :    monsoon drift
• "季风区" 英文翻译 :    monsoon region
• "季风雾" 英文翻译 :    monsoon fog
• "季风绪" 英文翻译 :    fengxu ji
• "季风雨" 英文翻译 :    monsoon rain
• "蜗季风" 英文翻译 :    southwest mo oon; southwest monsoon
• "夏季风" 英文翻译 :    summer monsoon; the summer wind
• "尤季风" 英文翻译 :    indian monsoon
• "季风, 吹季风的季节, 雨季" 英文翻译 :    monsoon
• "潮湿季风" 英文翻译 :    wet monsoon
• "赤道季风" 英文翻译 :    equatorial monsoon

• Impact of the convection over the indo - china peninsula on the onset of scs summer monsoon
  中南半岛地区热力特征对南海季风爆发的可能影响及机理
• The relations between the sst anomalies in south china sea - tropical eastern indian ocean and the south china sea monsoon
  热带东印度洋海温年际变化与南海季风爆发关系的初步分析
• The results show that before the summer monsoon onset , the air - sea heat exchange near xisha area is weak , the vapor flux is small and the main trend is that the ocean is being heated ; while after its onset , the air - sea heat exchange is balanced roughly
  结果表明：季风爆发前，西沙海气界面热量交换较弱，水汽通量较小，以海洋获得热量为主；季风爆发后，海气界面热量交换接近平衡。
• At the same time , the rapid enhancement of scs cef can also result in the northward march of wpsh and the onset of scssm . the earlier establishment and stronger southerlies correspond to the earlier onset time of scssm , and vice versa
  不仅如此，二者对季风爆发的早晚也有重要影响，当前期这两支南风气流建立偏早、强度偏强时，南海夏季风爆发易偏早；反之，当南风气流建立偏晚、强度偏弱时，南海夏季风爆发易偏晚。
• The analysis of the large - scale synoptic situation shows that strong precipitation is closely related to the explosion of monsoon and the intensification of cross - equatorial flow which bring a lot of vapor and meet with cold masses at the eastern of northwest district on 8th , june causing extremely heavy rainfall ; that subtropical high - level jet at 200hpa , subtropical high at 500hpa and low - level jet at 850hpa are the weather backgrounds favorable to strong precipitation ; that the pattern of eastern highs and western lows and the establishment of a low - level jet and the coupling between upper - and low - level patterns that determine that the rain occurred in the east of the northwest china ( on average , this is the rainy season for the south of china , but not for the northwest china ) ; that water vapor comes from southerly and easterly flow which converge at the eastern of northwest district with convergence mainly in lower levels and pbl ; that the high value of the whole - level apparent heat source < q1 > is near the area of large rainfall in the direction of northeasterly - southwesterly agreeable to shear line very well and the condensation latent heat releasing is main heat source with vertical advection item playing key role in q1 and q2 ; that there is a vertical secondary circulation crossing low - lever jet whose ascending branch is at the area of large rainfall ; that the construction of convection instability and conditional symmetry instability results that there is not only deep thermal instability , but also moisture influx and triggering mechanism of thermal instability causing strong torrential rain
  作为对比，本文还对2002年6月24 - 25日发生在北京地区的强地形雨进行了分析，并讨论陕南、北京地区两地暴雨的异同点以及地形作用的共性和个性，为两地暴雨预报提供有益的参考，得出了一些很有意义的结果： 1大尺度环流背景分析表明： ( 1 ) “ 02 . 6 ”强降水与6月上旬越赤道气流和季风爆发密切相关，携带大量水汽的偏南气流与冷空气于6月8日交汇在西北地区东部，导致了这次强降水的发生； ( 2 ) 200hpa的副热带西风急流、 500hpa副高以及850hpa的低空急流的配置非常有利于本文分析之陕西强降水的发展与维持。大尺度形势分析表明，东高西低形势场、低空急流的建立和高低空形势的配置决定了这场降雨出现在西北地区东部。与暴雨区相联系，存在一支横越低空急流的经向垂直环流，暴雨区处于该垂直环流的上升支； ( 3 )偏南和偏东气流水汽通道在西北地区东部交汇，水汽的辐合积聚主要在对流层低层和行星边界层内完成； ( 4 )整层的视热源< q _ 1 >高值区在暴雨区附近呈东北-西南向分布，与切变线走向非常一致，降水产生的凝结潜热释放是强降水区大气的主要热源。
• To the large - scale atmosphere , we separate the terms of the horizontal vorticity converting into the vertical vorticity , which considered as the baroclinic terms , from the terms that not including horizontal vorticity by the rules of the p coordinate transforming to the z coordinate in the traditional vorticity equation , and carry out the scale analysis , and then conclude that the baroclinic terms are able to reach the same magnitude grade as the partial derivative of the vertical vorticity to time when it takes place the large scale precipitation in the summer monsoon period in china . by analyzing the game reanalysis data from april to august in 1998 in the region of chinese continent , we found that the baroclinic terms is important to the large - scale cyclone developing above the 600hpa , and the magnitude changing of the baroclinic terms is nearly in - phase as the monsoon movement , so which imply exactly that the magnitude changing of the baroclinic terms is the one of the natural characters of the summer monsoon evolution and equivalent to the movement rule of the subtropical high of the western pacific
  在p坐标垂直涡度方程中，利用p坐标向z坐标转换的公式将水平涡度向垂直涡度转化的所有项分离出来，这些项具有明显的斜压特征，对其进行尺度分析后，得出在可以忽略潜热释放对涡度影响的对流层中、高层，此转化项是大尺度斜压涡度发展的重要项。通过对1998年48月的game再分析资料进行实际计算也发现，转化项在东亚夏季风上升支的600hpa及以上层次对垂直涡度的局地变化贡献很大，不能忽略。同时发现水平涡度向垂直涡度的转化在南海季风爆发时和江淮梅雨入梅及发展过程中均有指示性意义，在南海季风爆发以后，在中国东南部地区，转化项的大小与夏季风的活跃和中断等活动有着几乎一致的变化规律，这从侧面也指出了，此转化项的变化是夏季风演变所具有的本质特征，并且它反映出了西太平洋副高在中国大陆的活动情况。