We use historical materials of monthly foggy days from 84 stations of Shandong Province during the latest decades,analyze the spatial distribution features of mean foggy days during autumn and winter and annual mean f...We use historical materials of monthly foggy days from 84 stations of Shandong Province during the latest decades,analyze the spatial distribution features of mean foggy days during autumn and winter and annual mean foggy days in Shandong.Result shows that foggy weather have strong regional characteristics,there are obvious difference between Shandong inland and coast in terms of the frequency of foggy days,winter and autumn are the peak period of dense fog in the inland of Shandong,however,dense fog is less in coastal area.Take Jinan for example,we have emphatically analyzed the activity change rules of foggy days during autumn and winter since 1952 in the inland,as well as the characteristics of atmospheric circulation during the frequently-occurring year and less frequently-occurring year of dense fog.展开更多
利用由多个美国研究部门及大学的共同参与研发的新一代中尺度预报模式和同化系统——WRF(Weather Research Forecast)模式,对2006年12月24—27日沪宁高速公路及其周边地区出现的一次罕见的持续性大雾过程进行数值模拟研究。结果表明,此...利用由多个美国研究部门及大学的共同参与研发的新一代中尺度预报模式和同化系统——WRF(Weather Research Forecast)模式,对2006年12月24—27日沪宁高速公路及其周边地区出现的一次罕见的持续性大雾过程进行数值模拟研究。结果表明,此次大雾过程属于较典型的平流雾,其生成和维持的主要原因是大气层结稳定、系统的下沉运动、充足的水汽;同时也有辐射作用,地面的大气长波辐射冷却是雾维持的重要因素。大范围下沉运动使中低层大气增温与地面辐射降温配合,形成深厚的逆温层,对大雾长时间维持起决定性作用。所以这是一次以平流雾为主伴随辐射雾的过程。27日14时后干冷空气南下才使大雾消散。展开更多
文摘We use historical materials of monthly foggy days from 84 stations of Shandong Province during the latest decades,analyze the spatial distribution features of mean foggy days during autumn and winter and annual mean foggy days in Shandong.Result shows that foggy weather have strong regional characteristics,there are obvious difference between Shandong inland and coast in terms of the frequency of foggy days,winter and autumn are the peak period of dense fog in the inland of Shandong,however,dense fog is less in coastal area.Take Jinan for example,we have emphatically analyzed the activity change rules of foggy days during autumn and winter since 1952 in the inland,as well as the characteristics of atmospheric circulation during the frequently-occurring year and less frequently-occurring year of dense fog.
文摘利用由多个美国研究部门及大学的共同参与研发的新一代中尺度预报模式和同化系统——WRF(Weather Research Forecast)模式,对2006年12月24—27日沪宁高速公路及其周边地区出现的一次罕见的持续性大雾过程进行数值模拟研究。结果表明,此次大雾过程属于较典型的平流雾,其生成和维持的主要原因是大气层结稳定、系统的下沉运动、充足的水汽;同时也有辐射作用,地面的大气长波辐射冷却是雾维持的重要因素。大范围下沉运动使中低层大气增温与地面辐射降温配合,形成深厚的逆温层,对大雾长时间维持起决定性作用。所以这是一次以平流雾为主伴随辐射雾的过程。27日14时后干冷空气南下才使大雾消散。
