A43B-0268
Impact of spatial resolution on cirrus infrared satellite retrievals in the presence of cloud heterogeneity

Thursday, 17 December 2015
Poster Hall (Moscone South)
Thomas Fauchez, Oak Ridge Associated Universities, Oak Ridge, TN, United States, Steven E Platnick, NASA Goddard Space Flight Center, Greenbelt, MD, United States, Kerry Meyer, Universities Space Research Association Greenbelt, Greenbelt, MD, United States, Zhibo Zhang, University of Maryland Baltimore County, Baltimore, MD, United States, Céline Cornet, Laboratoire d'Optique Atmosphérique (Lille), Villeneuve, France, Frédéric Szczap, Laboratoire de Météorologie Physique, University Blaise Pascal, Clermont-Ferrand, France and Philippe Dubuisson, Lab. d'Optique Atmosphérique, Villeneuve D'Ascq, France
Abstract:
Cirrus clouds are an important part of the Earth radiation budget but an accurate assessment of their role remains highly uncertain. Cirrus optical properties such as Cloud Optical Thickness (COT) and ice crystal effective particle size are often retrieved with a combination of Visible/Near InfraRed (VNIR) and ShortWave-InfraRed (SWIR) reflectance channels. Alternatively, Thermal InfraRed (TIR) techniques, such as the Split Window Technique (SWT), have demonstrated better accuracy for thin cirrus effective radius retrievals with small effective radii. However, current global operational algorithms for both retrieval methods assume that cloudy pixels are horizontally homogeneous (Plane Parallel Approximation (PPA)) and independent (Independent Pixel Approximation (IPA)). The impact of these approximations on ice cloud retrievals needs to be understood and, as far as possible, corrected.

Horizontal heterogeneity effects in the TIR spectrum are mainly dominated by the PPA bias that primarily depends on the COT subpixel heterogeneity; for solar reflectance channels, in addition to the PPA bias, the IPA can lead to significant retrieval errors due to a significant photon horizontal transport between cloudy columns, as well as brightening and shadowing effects that are more difficult to quantify. Furthermore TIR retrievals techniques have demonstrated better retrieval accuracy for thin cirrus having small effective radii over solar reflectance techniques. The TIR range is thus particularly relevant in order to characterize, as accurately as possible, thin cirrus clouds.

Heterogeneity effects in the TIR are evaluated as a function of spatial resolution in order to estimate the optimal spatial resolution for TIR retrieval applications. These investigations are performed using a cirrus 3D cloud generator (3DCloud), a 3D radiative transfer code (3DMCPOL), and two retrieval algorithms, namely the operational MODIS retrieval algorithm (MOD06) and a research-level SWT algorithm.

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