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Simulations of Infrared Radiances over a Deep Convective Cloud System Observed during TC4: Potential for Enhancing Nocturnal Ice Cloud Retrievals
NASA Langley Research Center, Hampton, VA 23681, USA
Science Systems and Applications, Inc., Hampton, VA 23666, USA
Earth System Laboratory, National Center for Atmospheric Research, Boulder, CO 80301, USA
NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
Science Systems and Applications, Inc., Lanham, MD 20706, USA
LASP, University of Colorado, Boulder, CO, USA
Universities Space Research Association, Columbia, MD 21044, USA
Department of Meteorology, Pennsylvania State University, State College, PA 16802, USA
GESTAR, Morgan State University, Baltimore, MD 21251, USA
Department of Atmospheric Sciences, Texas A&M University, College Station, TX 77843, USA
* Author to whom correspondence should be addressed.
Received: 20 August 2012; in revised form: 29 September 2012 / Accepted: 6 October 2012 / Published: 11 October 2012
Abstract: Retrievals of ice cloud properties using infrared measurements at 3.7, 6.7, 7.3, 8.5, 10.8, and 12.0 mm can provide consistent results regardless of solar illumination, but are limited to cloud optical thicknesses t < ~6. This paper investigates the variations in radiances at these wavelengths over a deep convective cloud system for their potential to extend retrievals of t and ice particle size De to optically thick clouds. Measurements from an imager, an interferometer, the Cloud Physics Lidar (CPL), and the Cloud Radar System (CRS) aboard the NASA ER-2 aircraft during the NASA TC4 (Tropical Composition, Cloud and Climate Coupling) experiment flight during 5 August 2007, are used to examine the retrieval potential of infrared radiances over optically thick ice clouds. Simulations based on coincident in situ measurements and combined cloud t from CRS and CPL measurements are comparable to the observations. They reveal that brightness temperatures at these bands and their differences (BTD) are sensitive to t up to ~20 and that for ice clouds having t > 20, the 3.7–10.8 µm and 3.7–6.7 µm BTDs are the most sensitive to De. Satellite imagery appears to be consistent with these results suggesting that t and De could be retrieved for greater optical thicknesses than previously assumed. But, because of sensitivity of the BTDs to uncertainties in the atmospheric profiles of temperature, humidity, and ice water content, and sensor noise, exploiting the small BTD signals in retrieval algorithms will be very challenging.
Keywords: clouds; optical depth; particle size; satellite; TC4; multispectral thermal infrared
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MDPI and ACS Style
Minnis, P.; Hong, G.; Ayers, J.K.; Smith, W.L., Jr.; Yost, C.R.; Heymsfield, A.J.; Heymsfield, G.M.; Hlavka, D.L.; King, M.D.; Korn, E.; McGill, M.J.; Selkirk, H.B.; Thompson, A.M.; Tian, L.; Yang, P. Simulations of Infrared Radiances over a Deep Convective Cloud System Observed during TC4: Potential for Enhancing Nocturnal Ice Cloud Retrievals. Remote Sens. 2012, 4, 3022-3054.
Minnis P, Hong G, Ayers JK, Smith WL, Jr, Yost CR, Heymsfield AJ, Heymsfield GM, Hlavka DL, King MD, Korn E, McGill MJ, Selkirk HB, Thompson AM, Tian L, Yang P. Simulations of Infrared Radiances over a Deep Convective Cloud System Observed during TC4: Potential for Enhancing Nocturnal Ice Cloud Retrievals. Remote Sensing. 2012; 4(10):3022-3054.
Minnis, Patrick; Hong, Gang; Ayers, J. Kirk; Smith, William L., Jr.; Yost, Christopher R.; Heymsfield, Andrew J.; Heymsfield, Gerald M.; Hlavka, Dennis L.; King, Michael D.; Korn, Errol; McGill, Matthew J.; Selkirk, Henry B.; Thompson, Anne M.; Tian, Lin; Yang, Ping. 2012. "Simulations of Infrared Radiances over a Deep Convective Cloud System Observed during TC4: Potential for Enhancing Nocturnal Ice Cloud Retrievals." Remote Sens. 4, no. 10: 3022-3054.