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气旋式的英文

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"气旋式"怎么读用"气旋式"造句

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  • cyclonic

例句与用法

  • On the continental shelf , left of kuroshio ( 125 . 3e , 28 . 5n ) , there exists a large cyclonic eddy
    5叩)存在一个大型的气旋式涡旋。
  • The cyclonic circulation associated with sam is well depicted by the storm motion vectors . fig
    可从图中风暴运动向量清楚看到与森姆相关的气旋式环流。
  • The cyclonic circulation associated with sam is well depicted by the storm motion vectors . fig
    可从图中风暴运动向量清楚看到与森姆相关的气旋式环流。
  • The numerical simulation with complete forcing produces the main characteristics of yellow and east china seas circulation in summer . baroclinic effect plays a important role on yellow seas circulation that yellow seas cold water mass induces a anticlockwise circulation . tide also strengthens it
    夏季黄海的环流结构体现了较强的斜压性,主要以密度流为主,黄海冷水团在黄海中部诱导了一个气旋式环流,潮汐作用亦对这一环流有贡献。
  • The basic requirements include good cyclonic inflow i . e . for the northern hemisphere , inward spiralling in an anti - clockwise sense at the lower levels for the initial spin - up process , and good outflow channels at the upper levels for effective ventilation . the convergence of air at the lower levels and divergence aloft imply a vertical circulation which is schematically shown in the following cross - sectional diagram
    热带气旋的诞生及发展的基本条件是:在大气低层必须有充份的气旋式气流辐合(在北半球,沿反时针方向螺旋形地流入) ,在大气高层要提供足够的气流外溢通道,这样才可以建立有效的通风机制。
  • Otherwise , further development and intensification will be inhibited . the basic requirements include good cyclonic inflow i . e . for the northern hemisphere , inward spiralling in an anti - clockwise sense at the lower levels for the initial spin - up process , and good outflow channels at the upper levels for effective ventilation
    热带气旋的诞生及发展的基本条件是:在大气低层必须有充份的气旋式气流辐合在北半球,沿反时针方向螺旋形地流入,在大气高层要提供足够的气流外溢通道,这样才可以建立有效的通风机制。
  • The salinity distribution characteristics are the high - salinity in the bohai bay and the low - salinity in the boahi strait . the density distribution shows that there is a large cyclonic density circulation in bohai sea and it is likely to exist some density current gyre in the middle part of the bohai sea . in winter the saddle - like pattern of the bohai sea temperature and salinity shows that the circulation structure is much complexer than the previous research results
    密度分布表明:夏季渤海湾口已经由以前的低密度中心变为现在的高密度中心,相应的环流结构也必会发生大的变化;夏季渤海中部会存在一个反气旋式的密度环流,并在局部可能存在多个密度流涡环;冬季渤海“马鞍状”温盐结构反映其密度环流结构要比以往研究结果复杂得多。
  • The basic requirements include good cyclonic inflow ( i . e . for the northern hemisphere , inward spiralling in an anti - clockwise sense ) at the lower levels for the initial spin - up process , and good outflow channels at the upper levels for effective ventilation . the convergence of air at the lower levels and divergence aloft imply a vertical circulation which is schematically shown in the following cross - sectional diagram
    热带气旋的诞生及发展的基本条件是:在大气低层必须有充份的气旋式气流辐合(在北半球,沿反时针方向螺旋形地流入) ,在大气高层要提供足够的气流外溢通道,这样才可以建立有效的通风机制。
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