摘要
雾作为边界层内一种特殊的天气现象与边界层结构有着密切联系。本文利用天津边界层梯度观测平台分析2010年11月28日至12月2日一次雾过程的边界层结构特征。结果表明:此次过程雾Ⅰ阶段水汽最先在离地面80~100 m的高度凝结,雾Ⅱ(平流雾)阶段水汽由上往下传输;雾Ⅰ前,大气有明显的逆温,雾Ⅱ前大气处于不稳定状态,雾中大气趋于中性,在雾变薄过程中,边界层气象塔可观测到雾顶的强逆温;雾中长波辐射达到平衡,净长波辐射为0,可用此区分水雾和霾;雾对光化学烟雾有抑制作用,NO_x和小粒子会出现累积,影响人体健康。
The fog is a kind of special weather phenomenon and is closely related with structures of the at- mospheric boundary layer. Based on the Tianjin boundary gradient observation system, we have analyzed a fog process from November 28 to December 2, 2010, which can be divided into two episodes, fog I and fog II. The results showed that: first the condensation of water was found from 80 to 100 m heights during fog I and then vapor was transported downward during fog 1I. There was obvious inversion temperature before fog ~[ and unstable atmosphere before fog II. While fog 11 happened, the atmospheric status was tending to be neutral, and there was a strong inversion temperature at the top of fog. Analysis on charac- teristics of radiation and pollution during fog process shows that, there was a long-wave radiation equilibri- um, an inhibition effect to the photochemical smog, and an accumulated effect of small particle and NOx during fog.
出处
《气象》
CSCD
北大核心
2012年第9期1103-1109,共7页
Meteorological Monthly
基金
国家自然科学基金项目(41075004)
公益性行业(气象)科研专项(GYHY201006011)
环保公益行业科研专项(201009001-4)
天津市气象局科研课题(201104)共同资助
关键词
雾
边界层
热力结构
动力结构
大气污染物
fog, atmospheric boundary layer, dynamic structures, thermal structures, air pollution