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Optimal Estimation Of Surface Reflectance From Landsat Tm Visible And Mid Infrared Data Over Penang Island

Authors: H. S. Lim; M. Z. MatJafri; K. Abdullah; N. Mohd. Saleh;

Optimal Estimation Of Surface Reflectance From Landsat Tm Visible And Mid Infrared Data Over Penang Island

Abstract

{"references": ["Slater, J. F., Dibba, J. E., Campbell, J. W. and Moore, T. S. 2004,\nPhysical and chemical properties of surface and column aerosols at a\nrural New England site during MODIS overpass, Remote Sensing of\nEnvironment, Volume 92, Issue 2, 173-180.", "Wald, L. and Baleynaud, J-M., 1999, Observing air quality over the city\nof Nantes by means of Landsat thermal infrared data, International\nJournal of Remote Sensing, 20 (5), 947-959.", "Kokhanovskya,b, A.A., Mayer, B. and Rozanov, V. V., 2005, A\nparameterization of the diffuse transmittance and reflectance for aerosol\nremote sensing problems, Atmospheric Research, 73, 37 - 43.", "Kaufman, Y. J., Wald, A. E., Remer, L. A., Gao, B. C., Li, R. R. and\nFlynn, L., 1997, The MODIS 2.1- m cannel\u00d4\u00c7\u00f6correlation with visible\nreflectance for use in remote sensing of aerosol, IEEE Transactions On\nGeoscience and Remote Sensing, V. 35, NO. 5, 1286 - 1298.", "Wen, G. Y., Tsay, S. C., Cahalan, R. F and Oreopolos, L., (1999). Path\nradiance technique for retrieving aerosol optical thickness over land,\nJournal of Geophysical Research, 104 (D24), 31321 - 31332.", "Vermote, E. and Roger, J. C., 1996, Radiative transfer modeling for\ncalibration and atmospheric correction, Advances in the Use of NOAA\nAVHRR Data for Land Applications, 49-72."]}

Retrieval of the surface reflectance is important in the remotely sensed data analysis to obtain the atmospheric reflectance or atmospheric correction. The relationship between visible and mid infrared reflectance over land was investigated and developed in this study. The surface reflectances of the two visible bands were measured using a handheld spectroradiometer collected around Penang Island. In this study, we use the assumption that the 2.1 μm band is not affected by aerosol and it is transparent to most aerosol types (except dust). Therefore the satellite observed signal is the same as the surface signal in 2.1 μm band. The correlation between the surface reflectance measured by the spectroradiometer in the blue and red region and the 2.1 μm observed by the satellite has been established. We investigate five dates of Landsat TM scenes in this study. The finding obtained by this study indicates that the surface reflectance can be retrieved from the 2.1 μm band.

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Keywords

Landsat TM, Spectroradiometer., Aerosol, Surface Reflectance

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