对流运动的英文

• countercurrent movement

• "对流"英文翻译    convection; convection curre ...
• "运动"英文翻译    arrange things or get things ...
• "肠电解质对流运动" 英文翻译 :    intestinal electrolyte movement by convection
• "对流运输" 英文翻译 :    convective transport; counter flow transport
• "对流运移" 英文翻译 :    convective transport
• "层流运动" 英文翻译 :    laminar motion; motion; laminar
• "环流运动" 英文翻译 :    circulatorymotion
• "率流运动" 英文翻译 :    stirring motion
• "乱流运动" 英文翻译 :    turbulent motion
• "偶环流运动" 英文翻译 :    bicirculating motion
• "平流运动层" 英文翻译 :    advection layer
• "势流运动" 英文翻译 :    motion; potential
• "紊流运动" 英文翻译 :    turbulent motion
• "涡流运动" 英文翻译 :    eddy motion; eddying motion; vortex motion
• "涡流运动学" 英文翻译 :    vorticity kinematics
• "旋流运动" 英文翻译 :    rotational fluid motion
• "表层吹流运动" 英文翻译 :    wind-drift surface movement
• "第一流运动员" 英文翻译 :    topnotcher
• "逆流运动粘度" 英文翻译 :    adverse flow kinematic viscosity
• "强迫涡流运动" 英文翻译 :    forced vortex motion
• "涡流运动粘度" 英文翻译 :    eddy kinematic viscosity
• "粘流运动方程" 英文翻译 :    viscous equation of motion
• "可压流运动方程" 英文翻译 :    compressible flow equation of motion
• "粘性流运动方程" 英文翻译 :    viscous equation of motion
• "扰动运动, 乱流运动, 扰乱运动" 英文翻译 :    turbulent motion

• The behavior of convective motion is not laminar but turbulent .
  对流运动的行为不是片流式而是湍流式。
• At the solar surface, convective motions of heated gases jostle the magnetic field line .
  在太阳表面，炽热气体的对流运动把这根磁力线冲来撞去。
• Within the rock which forms the highly permeable reservoir convection currents of hot water or steam occur .
  在形成高渗透性热储的岩体内，存在水或蒸汽的对流运动。
• As warm moist air flows into a storm , it gets pushed up and twisted by upper level winds
  一旦被卷入风暴中，暖湿气流就在高层气流的压迫下产生上升和对流运动。
• In day time , especially in mid - summer , the ground heats up under the sun and spurs convection in the air . this lifts moisture up the atmosphere aloft , which gradually develops into isolated , floating cumulus
  在日间，特别是在盛夏时候，地面吸收大量太阳的热量，引起大气对流运动，将水气带上上空，慢慢形成孤立悬浮的积云。
• In day time , especially in mid - summer , the ground heats up under the sun and spurs convection in the air . this lifts moisture up the atmosphere aloft , which gradually develops into isolated , floating cumulus
  在日间，特别是在盛夏时候，地面吸收大量太阳的热量，引起大气对流运动，将水气带上上空，慢慢形成孤立悬浮的积云。
• Nothing can be cooler than 0k . the gas below the photosphere has a higher temperature and so will rise up to the photosphere . after releasing its energy , the gas will become cooler and darker
  光球层之下的气体温度比光球层高，就好像沸腾的水，底层的气体会向上升，当这些炽热气体把能量释放后，便会变冷变暗，然后沉降回光球层之下，这种对流运动产生了称为
• A transverse secondary circulation is produced by the coupling of high and low jets , while the sinking branch of the secondary circulation providing the dynamic conditions for the dry intrusion air . during the period of the heavy rain process , dry intrusion descends southward along the intense constant potential temperature lines , which promotes the lower cyclone . in addition , the pouring of upper - level dry air not only decreases ground temperature behind the front but also increases surface pressure and velocity
  由于高、低空急流耦合，在高空急流中心左侧产生的下沉运动和高空急流中心右侧、低空急流左侧产生的上升运动在锋面上形成一次级环流，次级环流的下沉支运动为对流层高层干空气和高位涡的下传提供了动力条件；进一步研究发现，干侵入沿相当位温密集带向南向下伸展，引起对流层低层气旋性涡度的发展；此外，高层干冷空气向下注入，导致地面温度降低、气压升高、风速加大、低层辐合增强、上升速度加大，从而促进了新的对流运动，引起降水增强。
• The first diagnostic analyses show that the heavy rainfalls are produced together by vortex , shear line and upper and lower jets , meiyu front . the condition of high energy , saturation , potential instability is propitious to the form and maintenance of heavy rainfall . the result of numerical simulation by mm5 model shows that heavy . rainfall has close relation with meso - scale vortex pole and strong convection
  采用ncep全球谱模式和常规观测资料对“ 03 . 7 ”江淮地区的两次暴雨过程的影响系统及其可能机制进行了初步诊断分析，发现梅雨暴雨是受低槽、低涡、切变线、高、低空急流和梅雨锋区共同影响造成的，该地区维持高能、饱和、潜在不稳定的环境，有利于暴雨的产生中尺度数值模式( mm5 )模拟结果表明梅雨暴雨与中尺度涡柱、强对流运动密切相关。