环流圈的英文

• circulation cell

• "环流"英文翻译    circulation; circulating cur ...
• "圈"英文翻译    circle; ring
• "极地环流圈" 英文翻译 :    polar circulation cell
• "逆环流圈" 英文翻译 :    reverse cell
• "转子；环流圈" 英文翻译 :    gyre
• "哈德里环流圈" 英文翻译 :    hadley cell
• "哈得来环流圈" 英文翻译 :    hadley cell; hadleycell
• "中纬度环流圈" 英文翻译 :    middle latitude circulation cell
• "环流" 英文翻译 :    [气象学] circulation; circulating current; circumferential motion; circular current; ring current; streaming; interchange current◇环流器 circulator; 环流气体 recycle stream; 环流型 circulation pattern
• "软流圈；岩流圈" 英文翻译 :    astheno here; asthenosphere
• "对流圈" 英文翻译 :    convection cell; convective cell; troposphere
• "扼流圈" 英文翻译 :    [电学] choke; choke coil; reactor; choking turn; choking coil; retardation coil; reactance coil
• "节流圈" 英文翻译 :    ferrule; orifice plug; throttle washer
• "抗流圈" 英文翻译 :    [电工] choke coil; choke; choking turn
• "气流圈" 英文翻译 :    air flow pattern
• "软流圈" 英文翻译 :    aesthenosphere; asthenosphere; rheosphere
• "岩流圈" 英文翻译 :    asthenosphere
• "阻流圈" 英文翻译 :    stop coil
• "半环流" 英文翻译 :    half circulation; half-circulation
• "超环流" 英文翻译 :    supercirculation
• "反环流" 英文翻译 :    counter circulation; counter-circulation
• "非环流" 英文翻译 :    non circulatory flow; non-circulatory flow
• "风环流" 英文翻译 :    wind circulation
• "环环流" 英文翻译 :    direct circulation
• "环流，循环" 英文翻译 :    circulation

• The northern hemisphere hadley cell now overlaps 1000km into the southern hemisphere .
  这时，北半球哈得来环流圈伸进南半球约1000公里。
• If the pressure changes over a large area , winds start to blow in a huge circle . high - pressure air is pulled into a low - pressure center
  如果气压在一个大的区域上方改变，风开始形成巨大的环流圈。高压空气进入低压空气的中心。
• ( 3 ) on interannual timescale , the changes in the sh ferrel cell lead to the anti - phase variation of the subtropical high and the circumpolar low , i . e . , the antarctic oscillation ( aao )
  ( 3 )南半球ferrel环流圈的异常使绕极低压带和副热带高压带的强度出现了反位相的变化特征，即南极涛动。
• 3 ) , the joint uprising branch is located around the equation , basically on the summer hemispheric side , and it is strong in january and july and weak in april and october , which has a two - year oscillation period
  3 ，北、南半球hadley环流圈及其共同上升支位于赤道附近，但偏于夏半球一侧，其强度1 、 7月强， 4 、 10月弱，做年双周振荡。
• The strengths of hemispheric hadley circulations are strong in winter and weak in summer , which have one - year oscillation period . 2 , it is basically equivalent of the strengths of the both hemispheric hadley circulations in april and october
  2 ，半球hadley环流圈强度冬强夏弱，做年单周振荡，过渡季节( 4月和10月)两半球hadley环流圈强度相当。
• The seasonal variation of the mean meridional circulation and the double - level structure of the hadley circulation are analyzed by the two methods . the paper also studies the zonal difference of the anomalous meridional circulation and the impacts of el nino / la nina events on the local meridional circulation anomaly . conclusions are drawn as follows : 1 , the hadley circulations in both hemisphere and the position of their joint uprising branch move wholly with the heat equation , with most north in july and most south in january
  然后用简化方法分析了气候平均经圈环流的季节变化，论文还对hadley环流的双层结构和异常经圈环流的纬向差异以及elnino 、 lanina事件对局地经圈环流异常的影响作了研究，结果表明： 1 ，北、南半球hadley环流圈及其共同上升支的位置随热赤道作整体性移动， 7月最北， 1月最南。
• 4 , there are obvious differences of the seasonal variations of the hadley circulations and the strength and position of their joint uprising branch . the strengths of winter hadley circulations and their joint uprising branch is strong in the south hemisphere and weak in the north , with it is nearer to the equation in the south hemisphere than in the north of their centers
  4 ， hadley环流圈及其共同上升支强度、位置的季节变化存在明显半球际差异：冬季hadley环流及其共同上升支强度南半球( 7月)明显强于北半球( 1月) ，其中心位置在南半球较北半球靠近赤道。
• In the second part of the paper , with employing the game reanalysis data and on the basis of the theories of the baroclinic vorticity development , this paper inferred from the dynamic analysis that the horizontal vorticity can represent the baroclinic intensity of the large - scale atmosphere , and the conversion of the horizontal vorticity converting into the vertical vorticity is actually the phenomenon that the horizontal vorticity flux of the summer monsoon owning the striking longitudinal - direction vertical structure and the strong baroclinicity , influence on the horizontal movement of the atmosphere
  在第二部分，基于第一部分的结果，本文在斜压涡度发展理论的基础上，用在我国季风区具有更高准确性的game再分析资料，讨论分析了能代表大尺度大气斜压性强度的水平涡度在向垂直涡度转化的情况，说明了此转化就是具有明显经向垂直结构特征和强斜压性的夏季风环流圈将其经向垂直剖面上的涡旋通量强迫于水平运动的现象。