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AEROSOL RETRIEVAL AND ATMOSPHERIC CORRECTION FOR MERIS DATA OVERLAKES

机译:梅里斯数据超标的气溶胶反演和大气改正

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One of the objectives of the ENVISAT project AO-164 on “Environmental Research in the Eastern Alps” is therndevelopment of algorithms for retrieval of water quality parameters of lakes from MERIS data. In order to test and validaternatmospheric correction algorithms and to provide basic data for the development of algorithms for retrieval of limnologicalrnparameters and aerosol loadings, several field campaigns were carried out in summer 2003 on the lakes Garda (Italy) andrnMondsee (Austria) parallel to MERIS overflights. Field measurements of aerosol optical thickness (AOT) were used asrninput for atmospheric correction by means of the 6S model, and field spectra measured above the water surface were used tornvalidate the at-surface reflectance derived from MERIS data. The agreement between field and MERIS reflectance spectrarnis in general good. Some differences are found at short wavelengths which can be attributed to insufficient knowledge ofrnaerosol properties. The sensitivity of the radiative transfer model to changes in AOT and the aerosol model wasrninvestigated. For a day with strong variability in the aerosol loading the spatial gradient of AOT was estimated from MERISrndata and compared with the temporal evolution of AOT at a field measurement site.
机译:ENVISAT项目AO-164关于“东部阿尔卑斯山的环境研究”的目标之一是开发用于从MERIS数据中检索湖泊水质参数的算法。为了测试和验证大气层校正算法,并为开发用于检索物性学参数和气溶胶负荷的算法提供基础数据,2003年夏季,在平行于MERIS飞越的意大利加尔达湖(意大利)和rnMondsee湖(奥地利)开展了几次野战。通过6S模型将气溶胶光学厚度(AOT)的现场测量值用于大气校正,并使用在水面以上测得的现场光谱来验证源自MERIS数据的表面反射率。场和MERIS反射光谱之间的一致性总体良好。在短波长下发现了一些差异,这可能归因于对rnaerosol性质的了解不足。研究了辐射传递模型对AOT和气溶胶模型变化的敏感性。对于气溶胶负荷变化很大的一天,根据MERISrndata估算了AOT的空间梯度,并将其与现场测量地点的AOT的时间演变进行了比较。

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