cold advection中文是什么意思

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中文翻译
造句

冷平流

cold adj. 1.冷，寒，冻；冰凉的。 2.冷静的，冷淡的， ...
advection n. (热的)对流；(空气的)平流。 adj. -vec ...
advection n. (热的)对流；(空气的)平流。 adj. -vective
advection cooling 平流冷却
advection fog 海面雾; 平另; 平流雾
advection heat 对流热
advection inversion 平流逆温
advection layer 平流层; 平流运动层
advection of heat 平流热效
advection region 平流区
ageostrophic advection 非地平流
differential advection 差异平流
geostrophic advection 地转平流
horizontal advection 水平平流
temperature advection 温度平流
thermal advection 热平流; 温度平流
thickness advection 厚度平流
vertical advection 垂直平流
vorticity advection 涡度平流
warm advection 暖平流
advection radiation fog 平流辐射雾
cyclonic vorticity advection 气旋式涡度平流
differential thermal advection 差异热平流
geostrophic advection scale 地转平流尺度
thermal vorticity advection 热成涡度平流; 热力涡度平流

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例句与用法

The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation
结果表明：在中高层暖性高压脊及地面变性冷高压稳定维持的大尺度背景条件下，地表净辐射引起的近地层冷却是大雾过程的触发和加强机制；中低空下沉气流的存在有助于近地层的弱风条件和稳定层结的建立；低层暖平流的输入和边界层的浅层抬升是大雾长时间持续的原因；伴随冷空气南下的偏北大风是驱使大雾消散的动力因子。
There are two parts in this paper : firstly , a set of single doppler velocity models are presented for typical ambient windfields that include those of being uniform horizontally , macroscale convergence and divergence , which overlap warm and cold advection . which are marked by different signatures in the single doppler velocity field . the models proposed can help users identify useful information from the dopple velocity patterns
本论文包括两个部分：第一篇通过对典型风场的单多普勒天气雷达径向速度图象进行模拟，典型风场包括水平均匀一致的风场、非均匀水平风场的大尺度运动的辐合辐散风场以及大尺度运动的辐合辐散风场与冷暖平流的迭加等。