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大气流的英文

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"大气流"怎么读用"大气流"造句

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  • atmospheric current

例句与用法

  • Afbc atmospheric fluidized bed combustion
    大气流化床燃烧
  • In contrast , the baroclinic component over low levels was stronger to south of wuhan and the barotropic component was strong to north of wuhan
    暴雨期间实际大气流场高层的斜压分量很强;低层武汉以南斜压分量较强,而武汉以北的正压分量强。
  • Such results are gotten : due to the unique topography the wind of beijing area during the day time is southern anabatic wind and in the night is northern katabatic wind in summer
    研究结果表明: 1北京区域夏季边界层风场受西北特殊地形的影响,夜间低层大气流场常表现为由北向南的下坡风,白天逐渐转为由南往北的上坡风。
  • The baroclinic component of the real atmospheric flow fields played a dominant role during the torrential rain . with the development of the rainstorm , the barotropic component of the real atmospheric flow fields decreased , along with the baroclinic component increasing
    暴雨前后,实际大气流场的斜压性一直占主导地位,并且随着暴雨的发展,实际大气流场的正压性减弱而斜压性进一步增强。
  • Although the knowledge of wind effects on tall buildings has significantly improved over the last decades , an understanding of the mechanism that the atmospheric flow field to various wind include effects on structures has not been developed sufficiently for formulation of functional expressions . not only is the wind approaching a building complex , but the flow pattern generated around a building is complicated by the distortion of the mean flow field , the flow separation , the vortex formation , and the wake development
    在过去的几十年里,虽然人们对高层建筑风效应的了解已有显著提高,但对大气流场与结构物各种风致响应的关系还不能用解析表达式加以描述。由于平均流场的奇变、流动分离、旋涡形成以及紊流的发展,不仅使得流向建筑物的风,而且使得绕建筑物的流谱变得十分复杂。
  • With the research of the evolvement features of barotropic and baroclinic atmosphere flow fields , the mechanism has been studied of the formation , development and die out of the heavy rainfall which occurred in wu - han during the period of 21 - 22 , july 1998 . the results are shown as follows : the evolvement of the rainstorm has a close relation to the barotropic component of the real atmospheric flow filed . and the barotropic component is , to a certain degree , also responsible for the coupling characteristics of high - and low - level jets
    本文从研究大气正、斜压流场的演变特征入手研究了1998年7月武汉的一次强暴雨发生、发展、消亡全过程的机理,研究结果表明: ( 1 )未经过尺度分离的实际大气流场正压分量的演变与此次暴雨的酝踉、发展和消亡相对应,并且正压分量在一定程度上反映高、低空急流耦合特征。
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