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1)  Low-latitude upward flow
低纬上行尾向流
2)  low-latitude circulation
低纬环流
1.
Results show that there are close relationships between the interannual intensity changes of the cross-equatorial flows and the low-latitude circulations in Southern and Northern Hemispheres,especially the Asia-Australia pressure difference.
结果表明,越赤道气流强度的年际变化和同期南北半球低纬环流系统,特别是亚澳大陆气压差关系密切。
3)  upward flow
上升流,上行流,向上流动,向上流,上流
4)  zonal circulation
纬向环流
1.
It indicates that the obvious decrease of sandstorm and flying-sand in the Spring of 2003 in Shaanxi is due to upper air strong zonal circulation, weak radial circulation and previous excessive precipitation.
通过对2003年春季天气气候背景和天气气候变化的研究,指出2003年春季陕西沙尘暴、扬沙明显减少是由高空纬向环流偏强、径向环流偏弱和前期降水偏多共同所致。
2.
In warm winter it is found that the westerlies at Asia prevail zonal circulation and the subtropical high at west Pacific Ocean is stronger and extends more westerly than normal.
利用1951年以来的冬季(12月~2月)气温资料,对暖冬年进行划分,发现暖冬年西风带亚洲地区常出现纬向环流,低纬度西太平洋副热带高压偏强,位置偏西。
5)  zonal current
纬向流
1.
It is proved again that there always are zonal currents in the Luzon Strait, but the zonal currents are great vareations in the synoptic time scale.
分析和计算了吕宋海峡PR21断面最近海洋调查的部分CTD资料和ADCP资料,再一次证明吕宋海峡常年存在纬向流。
6)  zonal flow
纬向气流
补充资料:涂覆织物纬向拉伸强度
分子式:
CAS号:

性质:沿涂覆织物纬线方向拉伸至断裂时的最大强度。测定方法与径向拉伸强度的一样。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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