warm advection中文是什么意思

• 暖平流

• "warm"中文翻译    adj. 1.暖和的，温暖的；保暖的。 2.热情的，热心 ...
• "advection"中文翻译    n. (热的)对流；(空气的)平流。 adj. -vec ...
• "advection" 中文翻译 :    n. (热的)对流；(空气的)平流。 adj. -vective
• "advection cooling" 中文翻译 :    平流冷却
• "advection fog" 中文翻译 :    海面雾; 平另; 平流雾
• "advection heat" 中文翻译 :    对流热
• "advection inversion" 中文翻译 :    平流逆温
• "advection layer" 中文翻译 :    平流层; 平流运动层
• "advection of heat" 中文翻译 :    平流热效
• "advection region" 中文翻译 :    平流区
• "ageostrophic advection" 中文翻译 :    非地平流
• "cold advection" 中文翻译 :    冷平流
• "differential advection" 中文翻译 :    差异平流
• "geostrophic advection" 中文翻译 :    地转平流
• "horizontal advection" 中文翻译 :    水平平流
• "temperature advection" 中文翻译 :    温度平流
• "thermal advection" 中文翻译 :    热平流; 温度平流
• "thickness advection" 中文翻译 :    厚度平流
• "vertical advection" 中文翻译 :    垂直平流
• "vorticity advection" 中文翻译 :    涡度平流
• "in the warm" 中文翻译 :    在暖和的地方
• "to be warm" 中文翻译 :    天气热
• "warm" 中文翻译 :    adj. 1.暖和的，温暖的；保暖的。 2.热情的，热心的，热烈的；多情的。 3.易怒的；兴奋的；激烈的，激昂的。 4.亲热的；亲密的。 5.(颜色等)有温暖感觉的，暖色的；浓艳的；挑拨性的，色情的；【打猎】(嗅迹等)新鲜的，强烈的。 6.〔俚语〕富裕的，宽裕的。 7.〔口语〕费力的，困难的；不愉快的，待不下去的。 8.〔口语〕差一点就要找到[猜中]的。 9.(官员等)职位稳固的。 a warm heart 热情的心。 a warm water port 不冻港。 a warm welcome 热烈的欢迎。 a warm temper 急性子。 a warm friend 亲密的朋友。 warm descriptions 色情描写。 The place became too warm for him. 那里他已经待不下去了。 be getting warm (隐藏者、待猜事物)差一点就要被找到[猜中]；〔比喻〕接近真实。 get warm 暖起来；激昂起来，兴奋起来。 grow warm 激昂，热烈。 have warm work in doing it 那件事做起来有困难。 in warm blood 生气，激忿。 keep a place warm (代表人)暂时占据某地。 keep it warm 〔美国〕继续讨论某一问题〔不使冷却〕。 make things warm for sb. 烦扰[攻击]某人，使某人不愉快。 warm with 加开水和糖的白兰地酒 〔cf. cold without 〕。 warm words 〔美俚〕骂上帝(的话)。 warm work 吃力的[危险的]工作；激战，苦斗。 vt. 1.使暖，使加温；【体育】使热身，使作比赛前的准备活动；使热心，激发，鼓励，使兴奋。 2.〔口语〕占(座位)。 3.〔口语〕鞭打，责打。 warm oneself at the fire 烤火取暖。 vi. 暖，变暖；热中；兴奋；同情 (to towards)。 a warming match 热身赛。 warm sb.'s jacket 〔口语〕打某人。 warm up 加热，热一热(汤)；变暖；热中起来，兴奋起来；【运】作准备动作；(机件等)预热。 n. 〔口语〕暖一暖。
• "warm to" 中文翻译 :    同情, 爱好
• "advection radiation fog" 中文翻译 :    平流辐射雾

• The quasi - geostrophic process was diagnosed for a case of severe cold air breakout under the blocking situation during 16 - 18 march of 1998 . the attention was focused on the relationship between the surface anticyclone and 500hpa blocking high . the results indicate that the cold outbreak is associated with the adjustment of blocking situation in the ural area , i . e . the collapsing and rebuilding of the ural mountain blocking high . the temperature advections in the lower troposphere shown that the polar cold air invading from the northwest caused the ural blocking high collapsed , and a new ridge developed rapidly was due to the warm advection on the southwestern side which led to the ural blocking high rebuilt . in addition , the distribution of the vertical motion on 700hpa shown that the surface high splitting was related to the considerable upward motion located on the southeastern part of surface high
  对1998年3月中旬一次高空阻塞形势下强冷空气过程进行了诊断分析，着重讨论强冷空气爆发前后地面反气旋活动与高空阻塞形势调整的关系。研究结果表明，强冷空气的爆发与乌拉尔地区阻塞形势的调整阻塞高压的崩溃和重建紧密相关。对流层下部的温度平流分析表明，阻塞形势的调整是由于阻塞高压上游西北方有冷空气侵入导致了阻塞高压的崩溃，而上游来自西南方向的强暖流则导致高压脊迅速发展，使阻塞高压重新建立。
• The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation
  结果表明：在中高层暖性高压脊及地面变性冷高压稳定维持的大尺度背景条件下，地表净辐射引起的近地层冷却是大雾过程的触发和加强机制；中低空下沉气流的存在有助于近地层的弱风条件和稳定层结的建立；低层暖平流的输入和边界层的浅层抬升是大雾长时间持续的原因；伴随冷空气南下的偏北大风是驱使大雾消散的动力因子。
• The findings show that there exists overlap between macroscale convergence and warm advection if the degree of clock - wise turn dosen " t keep constant on both sides of zero doppler velocity contour about the near range of the observational site . the overlap produces vertical vapor transport and upward convergence movement favorable for formation and continuation of rain gush
  结果表明：零速度带在测站近距离两侧的弯曲程度不一致是暖平流与大尺度辐合运动的迭加所造成，这一结构为暴雨产生和维持提供了有利的水汽垂直输送和辐合上升运动。

• warm advection перевод