平流雾

WRF模式对平流雾的形势及物理量场的模拟是成功的，显示了WRF模式预报平流雾的潜在能力。

Potential ability of prediction the advection fog by WRF model is proved to some extent .

北京地区一次平流雾过程的分析和数值模拟

The Analysis and Simulation of an Advection Fog Event in Beijing

基于MODIS卫星数据的平流雾检测研究

Fog Detection Based on EOS MODIS Data

南京冬季平流雾微物理结构观测研究

Observational Studies on Microphysical Structures of Winter Advection Fogs in Nanjing

江面平流雾的数值研究

Numerical study on the advection-radiation fog of Yangtze River

一次持续稳定的平流雾天气

A Constantly Maintained Advection Fog

一次罕见的辐射-平流雾研究（Ⅰ）&生消物理过程分析

A study on a rare radiation-advection fog (ⅰ) & the analysis of physical process of genesis and dissipation

由于地面升温，逆温层从地面抬升至低空并稳定维持，是平流雾形成后能维持较久的又一重要原因。

The other important reason is that inversion layer were lifted from the ground to lower level of the air and maintained .

在自然界中最常见到的只有两种雾：一种是辐射雾，另一种是平流雾。

There are two kinds of fogs that are most common in nature : one is radiation fog and the other is advection fog .

从统计资料看，洛阳机场影响能见度的雾绝大多数是辐射雾，平流雾的出现低于0.1%。

According to the statistics , in Luoyang airport , it is radiation fog that mostly affect the visibility roughly , advection fog appears lower than 0.1 % .

其资料经迭代计算得到了黄海北部、青岛市近海平流雾季节海气间动量、热量和水汽的通量。

Through iterative calculation of the data . the seasonal air-sea fluxes of momentum . heat and moisture of the advection fog on northern Huanghai Sea near Qingdao city are obtained .

结果表明，半岛南部沿海城市雾季多平流雾，半岛北部沿海城市雾季多锋面雾，整个半岛沿海城市秋冬季多平流辐射雾；

The results show that , the advection fog prevails along the south part and the frontal fog prevails along the north part of the coast of Shandong peninsula in the fog season .

在北冰洋的南部，由于暖湿气流充分，易形成持续时间长、浓度大的平流雾；

In the southern part of the Arctic Ocean , due to the sufficient warm and wet flow there , it is favorable for advection fog to form , which is dense and lasts a long time .

最后对雾的红外衰减和可见光衰减进行了比较，结果表明浓平流雾对106μm红外辐射的雾衰减大于可见光的雾衰减。

Finally , the fog attenuation between 10.6 μ m and visible wavelength was compared , and the results show that the attenuation at 10.6 μ m is greater than that at visible wavelength for dense advection fog .

一次平流辐射雾的观测分析及数值模拟研究

Observational analysis and numerical simulation of an advection-radiation fog event

海陆交界处平流辐射雾的二维数值模拟

Two-dimensional modeling of the advection - radiation fogs on the sea-land interface

由海面蒸发波导预报平流海雾的方法

The way to forecast sea advection fog from evaporation duct

浅水湖沼&陆面地区平流辐射雾的数值模拟

A Numerical Model of Advection-Radiation Fog Within Shallow-Water Swamp & Land Area

冷海面对平流冷却雾起着很关键的作用。

The cold sea plays a key role in the advection cooling fog .

二维平流辐射雾的数值模拟

Two-Dimension Numerical Model of Advection - Radiation Fogs

平流海雾是黄海海雾的一种主要类型。

Advection fog is a main type of sea fog which occurs over the Yellow Sea .

一次平流辐射雾的边界层特征及雾水离子组分研究

On the Atmospheric Boundary Layer Character of an Advection-Radiation Fog Process and the Ionic Species Concentration of Fog Water

本文采用二维非定常数值模式，模拟了大气边界层内辐射雾、平流辐射雾和在海陆交界处的平流辐射雾的形成、演变规律。

A two dimentional , time - depending model has been developed to simulate the formation , evolution and dissipation of advection-radiation fogs in the atmospheric boundary layer .

逆温层是平流海雾形成的一个必要条件，分析它的形成和变化的天气学原因非常重要。

Since the inversion layer is a necessary condition for advection fog formation , it is very important to analyze its formation and evolution influenced by weather systems .

建立了一个二维时变数值模式，模拟了浅水湖沼&陆面地区平流辐射雾形成、演变和消散的基本过程。

A two-dimentional , time-dependent numerical model is developed to simulate the formation , evolution and dissipation of advection-radiation fogs within the shallow-water swamp & land area ( SWSLA ) .

它们均具有典型平流冷却海雾特征：形成之前受其东南高压系统影响，黄海海域受偏南风控制，导致暖平流输送，气温明显高于海温。

They have typical characteristics of stratospheric cooling sea fog . Such as their formation were impacted by the southeast high-pressure system . So the southerly winds over the Yellow Sea resulted in warm advection , leading to warm air mass over cold sea surface .