Chinese translation for "上升支"

ascending ramus

Related Translations:

上升爆破:  uplift blasting

急剧上升:  hoickhoiksteep rise

海岸上升:  coast elevation

上升轨迹:  ascending trajectory

上升断层:  up-faultupcast faultupthrow fault

上升脱离:  climb away

上升水:  ascending waterhypogene water

突然上升:  jump

稳定上升:  steady climb

上升通风:  ascensional ventilation

Example Sentences:

	1.	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。
	2.	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。
	3.	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.	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。
	5.	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。
	6.	6 % ) , its downtrend and uptrend were steep and its isis had two significant inflexion hi the trough . integer multiple pattern ( 7 . 7 % ) , its isis showed clear layered structure . there existed a basic isi and other isis were concentrated at about integer multiples of the basic isi 6 ，其下降支与上升支较为陡峭，且下降支与波谷以及波谷与上升支之间有两个明显的拐点；整数倍形占77 ， isi在连续变化的过程中显示分层结构，各层的isi为基础isi的整数倍；弥散形占6
	7.	During 1950 ~ 1976 / 1977 , the walker circulation over the tropical pacific and the vertical zonal monsoon circulation over the tropical indian ocean coupled at the oceanic continent , the same period when el nino occurs , the anomaly of the west wind over the tropical pacific can correlate with the departure of east wind over the tropical indian ocean through the two coupled vertical zonal circulation . but after 1976 / 1977 , the updraft of the walker circulation moved eastward . locating at the north of australia . therefore the two vertical zonal circulation could n ' t coupled , and the anomaly of west wind and the departure of east wind could n ' t geared . in the result . the signal of enso decreased in indian ocean after 1976 / 1977 1951 1976 1977年，热带太平洋的walker环流和热带印度洋的纬向季风环流在海洋性大陆附近耦合，当elnino事件发生时，太平洋的西风异常可以通过这两个纬向的垂直环流与印度洋的东风异常联系起来，而1976 1977年以后，由于西太平洋walker环流上升支东移到澳大利亚北部，热带两洋的纬向垂直环流无法耦合，热带太平洋elnino事件中的西风异常与热带印度洋的东风异常联系减弱，所以1976 1977年以后， enso在热带印度洋的信号减弱了。
	8.	In the sonograms of psittacula agapornis after the section of right side nxiits the ascending parts of the tone disappeared . this causes their vocalizations became the descendent - call . and in the sonograms with the left side nxiits sectioned , the harmonic parts above the basic song were weaken or disappeared 牡丹鹦鹉在断右侧nxllts后其声图中音调上升支消失，因而其叫声变为以降音调为主的降调叫声；在断左侧nxllts后的声图中，其基本音以上的谐波成分减弱或消失而在断双侧神经后其声图表现为一系列具有较低基频的宽带谐波谱。
	9.	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。

Similar Words：

"上升运动继电器" Chinese translation, "上升者" Chinese translation, "上升阵风" Chinese translation, "上升阵风产生的加速度" Chinese translation, "上升枝" Chinese translation, "上升支流" Chinese translation, "上升之子乐队" Chinese translation, "上升殖瓣" Chinese translation, "上升指令" Chinese translation, "上升中过渡" Chinese translation