Atmospheric Measurement Techniques Discussions www.atmos-meas-tech-discuss.net 1867-8610 2 5 2009 10.5194/amtd-2-2707-2009 http://www.atmos-meas-tech-discuss.net/2/2707/2009/ http://www.atmos-meas-tech-discuss.net/2/2707/2009/amtd-2-2707-2009.html http://www.atmos-meas-tech-discuss.net/2/2707/2009/amtd-2-2707-2009.pdf 2707 2748 2009-10-28 Detection of multi-layer and vertically-extended clouds using A-train sensors J. Joiner joanna.joiner@nasa.gov A. P. Vasilkov P. K. Bhartia G. Wind S. Platnick W. P. Menzel Goddard Space Flight Center, Laboratory for Atmospheres, Greenbelt, MD, USA Science Systems and Applications, Inc., 10210 Greenbelt, Rd., Ste 400, Lanham, MD, USA Cooperative Institute for Meteorological Satellite Studies, Space Science and Engineering Center, University of Wisconsin–Madison, Madison, WI, USA The detection of multiple cloud layers using satellite observations is important for retrieval algorithms as well as climate applications. In this paper, we describe a relatively simple algorithm to detect multiple cloud layers and distinguish them from vertically-extended clouds. The algorithm can be applied to coincident passive sensors that derive both cloud-top pressure from the thermal infrared observations and an estimate of solar photon pathlength from UV, visible, or near-IR measurements. Here, we use data from the A-train afternoon constellation of satellites: cloud-top pressure, cloud optical thickness, and the multi-layer flag from the Aqua MODerate-resolution Imaging Spectroradiometer (MODIS) and the optical centroid cloud pressure from the Aura Ozone Monitoring Instrument (OMI). The cloud classification algorithms applied with different passive sensor configurations compare well with each other as well as with data from the A-train CloudSat radar. <br><br> We compute monthly mean fractions of pixels containing multi-layer and vertically-extended clouds for January and July 2007 at the OMI spatial resolution (12 km&times;24 km at nadir) and at the 5 km&times;5 km MODIS resolution for infrared cloud retrievals. There are seasonal variations in the spatial distribution of the different cloud types. The fraction of pixels containing distinct multi-layer cloud is a strong function of the pixel size. Globally averaged, these fractions are approximately 20% and 5% for OMI and MODIS, respectively. These fractions may be significantly higher or lower depending upon location. 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