测绘与空间地理信息
測繪與空間地理信息
측회여공간지리신식
GEOMATICS & SPATIAL INFORMATION TECHNOLOGY
2013年
10期
40-43
,共4页
雷鸣%薛丹%李成范%尹京苑
雷鳴%薛丹%李成範%尹京苑
뢰명%설단%리성범%윤경원
MODIS%V5 .2算法%上海市%气溶胶光学厚度%太阳光度计
MODIS%V5 .2算法%上海市%氣溶膠光學厚度%太暘光度計
MODIS%V5 .2산법%상해시%기용효광학후도%태양광도계
NODIS%V5.2 algorithm%Shanghai%aerosol optical depth ( AOD)%photometer
基于6S传输模型,本文利用中分辨率成像光谱仪( MODIS)数据并结合较新的NASA的V5.2气溶胶业务反演算法,以上海市MODIS数据为研究数据源,结合晴朗天气(晴朗且无云或云稀薄)与AERONET发布的探测日(即发布AOD探测值日期)选取8组MODIS LIB 数据集,对其进行气溶胶厚度反演。同时将反演结果与AERONET架设在太湖区域点(31N,120E)的太阳光度观测的光学厚度进行验证。结果表明:V5.2反演算法结果与观测值呈现相同的变化趋势,反演值与观测值误差不大,在气溶胶光学厚度反演中具有较好的应用。
基于6S傳輸模型,本文利用中分辨率成像光譜儀( MODIS)數據併結閤較新的NASA的V5.2氣溶膠業務反縯算法,以上海市MODIS數據為研究數據源,結閤晴朗天氣(晴朗且無雲或雲稀薄)與AERONET髮佈的探測日(即髮佈AOD探測值日期)選取8組MODIS LIB 數據集,對其進行氣溶膠厚度反縯。同時將反縯結果與AERONET架設在太湖區域點(31N,120E)的太暘光度觀測的光學厚度進行驗證。結果錶明:V5.2反縯算法結果與觀測值呈現相同的變化趨勢,反縯值與觀測值誤差不大,在氣溶膠光學厚度反縯中具有較好的應用。
기우6S전수모형,본문이용중분변솔성상광보의( MODIS)수거병결합교신적NASA적V5.2기용효업무반연산법,이상해시MODIS수거위연구수거원,결합청랑천기(청랑차무운혹운희박)여AERONET발포적탐측일(즉발포AOD탐측치일기)선취8조MODIS LIB 수거집,대기진행기용효후도반연。동시장반연결과여AERONET가설재태호구역점(31N,120E)적태양광도관측적광학후도진행험증。결과표명:V5.2반연산법결과여관측치정현상동적변화추세,반연치여관측치오차불대,재기용효광학후도반연중구유교호적응용。
Based on transmission model 6S, this paper uses the moderate resolution imaging spectroradiometer ( MODIS) data com-bined with a new aerosol business inversion algorithm , V5.2 of NASA ,to retrieve the atmospheric aerosols optical depth .We take MODIS data in Shanghai as the research data , select 8 groups of MODIS LIB data set combined with Sunny weather ( Sunny and cloud-less or thin cloud ) and AERONET release detection date ( NASA release the date of detection value ) , and validate the retrieved results with the aerosol optical depth (AOD) of the solar luminosity observations erected in Taihu area (31N, 120E)by AERONET.The re-sults show that the V5.2 inversion algorithm results and observations presented the same change trend .The retrieved results are nearly close to observed value, and the V5.2 inversion algorithm has better application in aerosol optical thickness retrieval .