meridional circulation中文是什么意思

• 经向环流

• "meridional"中文翻译    adj. 1.子午圈[线]的；最高的，全盛的。 2.南欧 ...
• "circulation"中文翻译    n. 1.循环；运行。 2.传播；环流(量)，流通(量) ...
• "isentropic mean meridional circulation" 中文翻译 :    等熵平均经向环流
• "mean meridional circulation" 中文翻译 :    平均径向环流
• "three-cell meridional circulation" 中文翻译 :    三胞经向环流
• "meridional" 中文翻译 :    adj. 1.子午圈[线]的；最高的，全盛的。 2.南欧(人)的，法国南部人的；南方的。 n. 南欧人，(尤指)法国南部人。
• "meridional aberration" 中文翻译 :    子午圈象差
• "meridional aniseikonia" 中文翻译 :    经线向物象不等
• "meridional canal" 中文翻译 :    子午管
• "meridional cell" 中文翻译 :    经向环流
• "meridional cleavage" 中文翻译 :    经裂; 经线裂
• "meridional coma" 中文翻译 :    子午彗差
• "meridional component" 中文翻译 :    子午分量
• "meridional contour" 中文翻译 :    子午线剖面轮廓
• "meridional difference" 中文翻译 :    纬差
• "meridional division" 中文翻译 :    经分裂
• "meridional ellipse" 中文翻译 :    子午椭圆
• "meridional fibers" 中文翻译 :    经线纤维
• "meridional flow" 中文翻译 :    经向流
• "meridional foci" 中文翻译 :    子午焦点
• "meridional furrow" 中文翻译 :    经线沟
• "meridional index" 中文翻译 :    经向指数
• "meridional part" 中文翻译 :    渐长纬度
• "meridional parts" 中文翻译 :    渐长纬度; 纬度渐长率
• "meridional plane" 中文翻译 :    子午面; 子午平面

• 5 , there is extremely difference of the locally climatic meridional circulations , as well as there is obviously different seasonal changes
  5 ，局地经圈环流纬向差异很大并且存在明显季节变化。
• 6 , the zonal difference and seasonal change of locally anomalous meridional circulation are great . the meridional circulation anomaly over the pacific ocean relates closely with the el nino / la nina events
  6 ，局地异常经圈环流存在明显纬向差异和季节变化；太平洋经圈环流异常与elnino 、 lanina事件关系密切。
• In terms of the real data , the mass stream function is calculated by two methods , results indicate that both methods fit well with the need for calculating the climate and its anomaly of the mean meridional circulation
  本文通过实际资料的计算比较了质量流函数的两种计算方案，验证了简化方法同样适用于平均经圈环流的气候及其异常的分析需要。
• 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。
• The main factors affecting the precipitation in the first stage of rainy season in fujian province are pacific sst in preceding june , the western pacific subtropical high area index in preceding may , the asia polar vortex area index in preceding september , the eurasian meridional circulation index in preceding april to june , the 500hpa height in northwest asia in preceding spring . the main factors affecting the precipitation in the second stage of rainy season in fujian province are pacific sst in preceding july and august , the northern hemisphere polar vortex area index in january in same term , the pacific polar vortex intensity index in preceding september , the 500hpa height in south europe in preceding summer
  ( 2 )影响福建省前汛期的主要因子有：前期6月太平洋海温场、前期5月西太平洋副高面积指数、前期9月亚洲区极涡面积指数、前期4 - 6月欧亚径向环流指数和前期春季亚洲西北部500hpa高度场；影响后汛期的主要因子有：前期7月太平洋海温场、前期8月太平洋海温场、同期1月北半球极涡面积指数、前期9月太平洋区极涡强度指数和前期夏季欧洲南部500hpa高度场。
• All these results confirm the important of wind in meridional circulation and heat transport . based on mom2 model , a rectangular basin model with ideal w ind stress and other ideal conditions is designed to study the main processes and dynamical mechanism in setting the depth of cross - equator flow . the effects of horizontal diffusivity , seasonal variations of
  我们还通过全球海洋环流模式，进一步证实了风应力的季节变化在北印度洋热收支、 sst以及海洋环流变化中的作用:即包含风应力的季节变化将使长期平均的sst降低，海面净热通量增加。
• 4 ) during the meiyu , the precipitation in middle and lower reaches of yangtze river has the relationship with southern hemisphere circulation in early april and may . when the meridional circulation in middle and high latitude of south pacific in april and may is rather obvious and the south pole eddy is rather strong , the precipitation in middle and lower reaches of yangtze river may be bigger than ever
  4 )梅雨期长江中下游降水多寡与前期4 、 5月南半球环流存在联系，当4 、 5月南太平洋中高纬度地区经向环流较为明显，南极涡偏强时，长江中下游地区梅雨期降水易偏多；反之，当4 、 5月南太平洋中高纬度地区纬向气流较为明显，高纬度西风较弱，南极涡偏弱时，长江中下游地区梅雨期降水易偏少。

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