上升支 meaning in English
ascending ramus
Examples
- The eastward shift in the walker circulation and western wind anomolis are the possible reasons of the change of relationships between summer cross equator flows and enso
赤道太平洋西风异常及walker环流上升支的东移使得夏季越赤道气流与enso的关系产生了明显的年代际变化。 - 3 ) , the joint uprising branch is located around the equation , basically on the summer hemispheric side , and it is strong in january and july and weak in april and october , which has a two - year oscillation period
3 ，北、南半球hadley环流圈及其共同上升支位于赤道附近，但偏于夏半球一侧，其强度1 、 7月强， 4 、 10月弱，做年双周振荡。 - The seasonal variation of the mean meridional circulation and the double - level structure of the hadley circulation are analyzed by the two methods . the paper also studies the zonal difference of the anomalous meridional circulation and the impacts of el nino / la nina events on the local meridional circulation anomaly . conclusions are drawn as follows : 1 , the hadley circulations in both hemisphere and the position of their joint uprising branch move wholly with the heat equation , with most north in july and most south in january
然后用简化方法分析了气候平均经圈环流的季节变化，论文还对hadley环流的双层结构和异常经圈环流的纬向差异以及elnino 、 lanina事件对局地经圈环流异常的影响作了研究，结果表明： 1 ，北、南半球hadley环流圈及其共同上升支的位置随热赤道作整体性移动， 7月最北， 1月最南。 - 4 , there are obvious differences of the seasonal variations of the hadley circulations and the strength and position of their joint uprising branch . the strengths of winter hadley circulations and their joint uprising branch is strong in the south hemisphere and weak in the north , with it is nearer to the equation in the south hemisphere than in the north of their centers
4 ， hadley环流圈及其共同上升支强度、位置的季节变化存在明显半球际差异：冬季hadley环流及其共同上升支强度南半球( 7月)明显强于北半球( 1月) ，其中心位置在南半球较北半球靠近赤道。 - 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。