Local winds over the central Namib.
Local winds over the central Namib.
复制标题
纳米布中部有局地风。
DOI：
10.1080/03736245.1980.10559630
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发表时间：
1980
影响因子：
1.4
通讯作者：
M. Seely
中科院分区：
文献类型：
--
作者：
P. Tyson;M. Seely
广泛分布的热地形风在纳米布沙漠中部上空的大气下边界层产生明显的日振荡和季节振荡。在冬季的夜晚，在戈巴布的Kuiseb山谷以及高原和沿海地区之间，山脉和山脉平原风中的冷空气广泛的东南至东向平流。白天，尤其是夏季，当地的逆风占主导地位。海风向戈巴布的内陆渗透只限于下午晚些时候。在山谷风和平原山风开始之前的早晨，贝格风似乎是最频繁的。
Abstract Widespread thermo-topographic winds are shown to produce marked diurnal and seasonal oscillations of the lower boundary layer of the atmosphere over the central Namib desert. By night in winter, extensive south-easterly to easterly advection of cool air in mountain and mountain-plain winds occurs down the Kuiseb valley at Gobabeb and between the plateau and coastal regions. By day, and most strongly in summer, reverse local winds predominate. Inland penetration of the sea breeze to Gobabeb is shown to be confined to the late afternoon. Berg winds appear to be most frequent during the morning prior to the onset of valley and plain-mountain winds.