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作 者:陈英英[1] 唐仁茂[1] 周毓荃[2] 袁正腾[1] 向玉春[1] 李德俊[1]
机构地区:[1]湖北省人工影响天气办公室,武汉430074 [2]中国气象科学研究院,北京100081
出 处:《应用气象学报》2011年第6期691-697,共7页Journal of Applied Meteorological Science
基 金:中国气象局云雾物理环境重点开放实验室开放科研课题(2009Z0039);湖北省气象局科技发展基金(2010Q02)
摘 要:为更好地利用FY-3A气象卫星上中分辨率光谱成像仪(MERSI)资料高空间分辨率及多光谱的优势,细致分析云系在宏、微观方面的多重特征,首先利用平面平行辐射传输模式(SBDART)证明了MERSI的0.65,1.6μm和11.25μm通道能够分别反映云光学厚度、云粒子大小、云顶高度的信息,然后采用三通道合成彩色图像的方法,对FY-3A气象卫星云图进行云的分类解释判读。该技术可直观区分有云区、无云区,显示海陆分界,并且使不同云类在云图上体现为不同颜色。同时,FY-3A气象卫星高达1000 m甚至250 m的空间分辨率也使云的细致结构更为清晰,两项优势的叠加,大大提升了云的分类解释判读的准确程度和精细化水平。文中还尝试寻找典型云系的三通道特征值,以期为模糊C均值聚类(FCM)方法中聚类中心的选定提供经验值参考。Clouds are the result of atmosphere dynamical and thermo-dynamical process.Different cloud types reflect different weather situations and cloud microphysical structure features.Satellite image offers largearea and all-day information of the cloud formation,gathering or disperse.Cloud classification is one of the most important objectives of the satellite image research. At present,only one single channel can be used to identify cloud category at one time.A quick,direct and accurate method of the interpretation of cloud classification has not yet been developed.It becomes particularly important to get the composed information of cloud optical thickness,effective particle radius and cloud top height information quickly. In order to better use the multiple spectral data of Medium Resolution Spectral Imager(MERSI) on FY-3A meteorological satellite to carefully analyze the macro and micro physical parameters of cloud system,according to the fact that the 0.65,1.6μm and 11.25μm channel on MERSI is respectively sensitive to cloud optical thickness, effective particle radius and cloud top height based on the Santa Barbara DISORT Atmospheric Radiative Transfer,SBDART,which is that larger 0.65μm reflectance means larger optical thickness,larger 1.6μm reflectance means smaller effective particle radius,larger black body temperature of cloud top means lower cloud top height or warmer surface under clear air,the method of three color compositions is used to the explanation and interpretation of the cloud classification by FY-3A meteorological satellite data on 20 June 2009.The color is composed of red for visible reflectance,green for near infrared reflectance,and blue for the infrared brightness temperature. Redder means larger optical thickness,greener represents the smaller cloud top particles,and bluer means lower cloud tops or warmer surface under clear air. The technology makes different cloud types show in different colors,which is beneficial to directly distinguish cloud pixel from clear sky area,and the land
分 类 号:P455[天文地球—大气科学及气象学]
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