Can desert dust explain the outgoing longwave radiation anomaly over the Sahara during July 2003
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Nicolas Clerbaux | Jim Haywood | Sean Milton | Richard P. Allan | John M. Edwards | R. Allan | S. Milton | J. Edwards | J. Haywood | I. Culverwell | N. Clerbaux | I. Culverwell | Tony Slingo | I. D. Culverwell | Tony Slingo | Ian Culverwell
[1] P. Formenti,et al. Measurement and modeling of the Saharan dust radiative impact: Overview of the Saharan Dust Experiment (SHADE) , 2003 .
[2] A. Kirkevåg,et al. Intercomparison of models representing direct shortwave radiative forcing by sulfate aerosols , 1998 .
[3] A. Slingo,et al. Studies with a flexible new radiation code. I: Choosing a configuration for a large-scale model , 1996 .
[4] Sundar A. Christopher,et al. Longwave radiative forcing of Saharan dust aerosols estimated from MODIS, MISR, and CERES observations on Terra , 2003 .
[5] A. Ipe,et al. Outgoing longwave flux estimation: improvement of angular modelling using spectral information , 2003 .
[6] Alexander Ignatov,et al. Intercomparison of Satellite Retrieved Aerosol Optical Depth over the Ocean , 2004 .
[7] P. Bhartia,et al. Global distribution of UV-absorbing aerosols from Nimbus 7/TOMS data , 1997 .
[8] M. Ringer,et al. Inconsistencies between satellite estimates of longwave cloud forcing and dynamical fields from reanalyses , 2003 .
[9] Filipe Aires,et al. Land surface skin temperatures from a combined analysis of microwave and infrared satellite observations for an all-weather evaluation of the differences between air and skin temperatures , 2003 .
[10] David J. Diner,et al. MISR aerosol optical depth retrievals over southern Africa during the SAFARI‐2000 Dry Season Campaign , 2001 .
[11] Alexander Smirnov,et al. Comparisons of the TOMS aerosol index with Sun‐photometer aerosol optical thickness: Results and applications , 1999 .
[12] R. A. Sutherland,et al. Broadband and Spectral Emissivities (2–18 μm) of Some Natural Soils and Vegetation , 1986 .
[13] P. Formenti,et al. The mean physical and optical properties of regional haze dominated by biomass burning aerosol measured from the C-130 aircraft during SAFARI 2000 , 2003 .
[14] N. B. Ingleby,et al. The Met. Office global three‐dimensional variational data assimilation scheme , 2000 .
[15] Frank-M. Göttsche,et al. Modelling of diurnal cycles of brightness temperature extracted from METEOSAT data , 2001 .
[16] A. Ipe,et al. Validation and homogenization of cloud optical depth and cloud fraction retrievals for GERB/SEVIRI scene identification using Meteosat-7 data , 2004 .
[17] A. Smirnov,et al. AERONET-a federated instrument network and data archive for aerosol Characterization , 1998 .
[18] C. Thorncroft,et al. THE JET2000 PROJECT Aircraft Observations of the African Easterly Jet and African Easterly Waves , 2003 .
[19] Steven A. Ackerman,et al. Radiative Effects of Airborne Dust on Regional Energy Budgets at the Top of the Atmosphere , 1992 .
[20] Gerard Brogniez,et al. Observations of Saharan Aerosols: Results of ECLATS Field Experiment. Part II: Broadband Radiative Characteristics of the Aerosols and Vertical Radiative Flux Divergence , 1987 .
[21] Irina N. Sokolik,et al. Modeling the radiative characteristics of airborne mineral aerosols at infrared wavelengths , 1998 .
[22] P. Koepke,et al. Optical Properties of Aerosols and Clouds: The Software Package OPAC , 1998 .
[23] Jonathan P. Taylor,et al. Optical properties and direct radiative effect of Saharan dust: A case study of two Saharan dust outbreaks using aircraft data , 2001 .
[24] Oleg Dubovik,et al. Non‐spherical aerosol retrieval method employing light scattering by spheroids , 2002 .
[25] R. Allan,et al. Can desert dust explain the anomalous greenhouse effect observed over the Sahara during July 2003 revealed by GERB/UM intercomparisons. , 2004 .
[26] John E. Harries,et al. The Geostationary Earth Radiation Budget (GERB) Experiment: Science and Applications , 2004 .
[27] C. Bertrand,et al. Estimation of the 2002 Mount Etna eruption cloud radiative forcing from Meteosat-7 data , 2003 .
[28] F. Volz,et al. Infrared optical constants of ammonium sulfate, sahara dust, volcanic pumice, and flyash. , 1973, Applied optics.
[29] C. Velden,et al. ARTICLES: The Impact of the Saharan Air Layer on Atlantic Tropical Cyclone Activity. , 2004 .
[30] B. Barkstrom,et al. Clouds and the Earth's Radiant Energy System (CERES): An Earth Observing System Experiment , 1996 .
[31] P. Formenti,et al. Radiative properties and direct radiative effect of Saharan dust measured by the C-130 aircraft during SHADE: 1. Solar spectrum , 2003 .
[32] B. Holben,et al. Comparison of aerosol size distributions, radiative properties, and optical depths determined by aircraft observations and Sun photometers during SAFARI 2000 , 2003 .
[33] W. C. Snyder,et al. Classification-based emissivity for land surface temperature measurement from space , 1998 .
[34] Hester Volten,et al. Aerosol retrievals from AVHRR radiances: effects of particle nonsphericity and absorption and an updated long-term global climatology of aerosol properties , 2003 .
[35] Jonathan P. Taylor,et al. Radiative properties and direct effect of Saharan dust measured by the C‐130 aircraft during Saharan Dust Experiment (SHADE): 2. Terrestrial spectrum , 2003 .
[36] Michael D. King,et al. A flexible inversion algorithm for retrieval of aerosol optical properties from Sun and sky radiance measurements , 2000 .