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《Guangdong Meteorology》 2006-01
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More Discussions on the Differences between Haze and Fog in City

WU Dui~(1,2)(1.Institute of Tropical and Marine Meteorology,CMA,Guangzhou 510080,China;2.Department of Atmospheric Science,Sun Yai-sen University,Guangzhou 510275,China)  
The appearance of haze has important indication meaning to air quality,while the fog or light fog has specific weather indication relating to particular weather systems.With the rapid development of economy and urbanization,haze or haze weather become increasingly severe,so that,to distinguish haze and fog becomes a very realistic problem that need to be solved imminently.At the meteorological stations of China,the criterion to distinguish the haze and fog is relatively confusing and uncomparable.The widely adopted criterion of relative humidity to distinguish the haze and fog in many southeast coastal provinces is generally on the low side,leading to many haze weather events being recorded as light fog or fog.In the near surface atmosphere there always exists haze,while fog droplet hardly exists.Only under the enough supersaturation can the haze nuclei grow into fog droplet through moisture absorption,and such process is not easy to happen.Under non-saturation condition,it is impossible for even the soluble haze nuclei to grow into fog droplet not to speak of the insoluble ones.The observational data show that the minimum relative humidity for fog to occur is 91%,and there is no fog when the relative humidity is lower than 90%.The most important physical process to form fog droplets is cooling, down to the saturation point.It is almost impossible for haze nuclei to grow into fog droplet only through the natural moisture absorption.There is no such a supplement regulation ever saying that the relative humidity 70% shall be used to distinguish light fog and haze at any level of meteorological departments.Many haze weather events being recorded as light fog is purely due to misunderstanding.So it is necessary to take into consideration the change of weather system and other the macro-characteristics when distinguishing fog and haze,and it is reasonable to use the threshold value of relative humidity 90% as an assistant criterion to distinguish fog and haze.
【Fund】: 国家自然科学基金资助项目(40375002、40418008);; 广东省自然科学基金资助项目(033029);; 广东省重点科技攻关项目(2004A30401002、2005B32601011);; 广州市应用基础研究项目(2004J1-0021)
【CateGory Index】: P427.1;P426.4
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