ascending motion中文是什么意思

• 上升运动

• "ascending"中文翻译    adj. 1.上升的；向上的。 2.【植物；植物学】上向 ...
• "motion"中文翻译    n. 1.运动,动,移动(opp. rest)。 2.( ...
• "ascending" 中文翻译 :    adj. 1.上升的；向上的。 2.【植物；植物学】上向的；【解剖学】上行的。 an ascending slope 上坡。
• "in-motion" 中文翻译 :    运转着航行时
• "motion" 中文翻译 :    n. 1.运动,动,移动(opp. rest)。 2.(天体的)运行；(车、船等的)动摇；(机器的)开动,运转；【机械工程】机械装置,机制。 3.动作,举动；手势；眼色；姿态；〔pl.〕(个人或团体的)行动,举动,活动。 4.(议会中的)提议,动议；动机,意向；刺激；【法律】申请,请求。 5.大便；〔pl.〕排泄物。 6.【音乐】(旋律、曲调的)变移。 M- itself is a contradiction. 运动本身就是矛盾。 All her motions were graceful. 她的一举一动都优美。 The motion to adjourn was carried. 休会的提议通过了。 in motion 动着,运转着,活动着。 make a motion [motions] 用手势示意；提议。 motion study 操作研究。 of one's own motion 自动地,自愿地,出自本意。 on the motion of 经…的动议。 put [set] in motion 使动，启动,发动。 vi. 打手势要求[指示](to towards away)。 motion (to) sb.to take a seat 用手指椅子请某人坐下。 vt. 向某人打手势；向某人点头或摇头示意。 motion sb. away [out] 打手势叫某人走开[出去]。 n. -less 不动的,静止的。
• "ascending ability" 中文翻译 :    上升能力
• "ascending aestivation" 中文翻译 :    上升花被卷迭式
• "ascending air" 中文翻译 :    上升空气流; 上升气流; 向上气流
• "ascending angle" 中文翻译 :    爬坡角; 上升角
• "ascending aorta" 中文翻译 :    上行织脉; 升主动脉
• "ascending aortography" 中文翻译 :    上行性主动脉造影术
• "ascending arc" 中文翻译 :    上升弧线
• "ascending artery" 中文翻译 :    升动脉,肠系膜间动脉
• "ascending axis" 中文翻译 :    上升轴(指茎)
• "ascending belt" 中文翻译 :    上行输电带
• "ascending bottoms" 中文翻译 :    上升底
• "ascending branch" 中文翻译 :    上升段; 上升枝; 上升支流; 升带; 升弧; 向上分支
• "ascending bucket" 中文翻译 :    上升吊桶
• "ascending buoy" 中文翻译 :    上升浮标
• "ascending chain" 中文翻译 :    升链; 升序列
• "ascending check" 中文翻译 :    在上升状态中检查
• "ascending cholangiohepatitis" 中文翻译 :    上升性胆管性肝炎
• "ascending chrimatography" 中文翻译 :    上行层析法
• "ascending chromatogram" 中文翻译 :    上行色谱图
• "ascending chromatography" 中文翻译 :    上升色谱法; 上行色层分离; 上行色谱法；上行层析; 上行色谱分离法

• The compensating descending motions normally occur over a much larger area than the ascending motion .
  补偿下沉运动通常出现在比上升运动大得多的区域上。
• Ascend motion analysis of reusable launch vehicle
  可重复使用运载器上升段运动分析
• The results show that the " 8 . 11 " rainstorm had significant mesoscale character . ascending motion , divergence and vorticity field intensified rapidly in the narrow area of rainstorm
  11 ”暴雨过程的常用物理量场的分析表明：这次暴雨过程的中尺度特征非常明显，在分辨率较低的大尺度场上很难分析出其物理量场的迅速变化。
• Analyzing the physics structure of vorticity , divergence , vertical velocity , frontogenesis " function , apparent heat source and apparent moist sink etc . indicated the physics fields are favorable for the occurance of the heavy rain over changjiang - huaihe river basin where the physics values are well according to the heavy rainstorm positions ; the low level jet is closely subject to the moisture and the coupled system of the low and the upper level jetstreams induced the strongly " ascending motion ; the intensity of the frontogenesis varies with the development of the rainfall system and reacts the rainfall intensity
  主要分析了这次过程中的多种物理量，包括涡度、散度、垂直速度、锋生函数、视热源、视水汽汇等，对这一暴雨过程有了比较系统的认识。结果表明：在江淮流域存在着有利于发生暴雨的物理量场配置，涡度、散度、垂直速度等物理量，与暴雨的落区都很吻合的；低空急流的产生不仅有利于水汽的输送，而且高低空急流的耦合造成了有利于强上升运动的配置；锋生强度随着降水系统的发展变化，并影响降水强度。
• The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows , so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening , one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea . furthermore , with the effect of terrain , the southern shaanxi province became the center of this extremely heavy rain process
  中尺度结构分析表明，本次暴雨具有明显的中尺度特征，是由三支气流共同作用的结果，分析发现( 1 )地面东南风和地形在这次大暴雨过程起主要作用； ( 2 )东路冷空气主要是通过中低层侵入陕南地区的，并与地面冷式锢囚锋的形成密不可分； ( 3 )夜博士论文:中尺度地形对陕南暴雨的影响研究间垂直次级环流发展加强可能有两个原因，一个是由于地形山谷风的作用，另一个是降水的潜热释放激发了上升运动: ( 4 )位势不稳定层结的形成与低层暖湿平流的发展有很好的对应关系; ( 5 )本次暴雨的水汽主要靠偏南风急流将孟加拉湾和中国南海的水汽输送至西北地区东部，为暴雨的发生提供了必要热力条件。
• 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。

• ascending motion перевод