Suppression of deep convection over the tropical North Atlantic by the Saharan Air Layer
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[1] N. Mahowald,et al. Observational evidence of African desert dust intensification of easterly waves , 2004 .
[2] Stanley G. Benjamin,et al. Radiative Heating Rates for Saharan Dust , 1980 .
[3] T. Carlson,et al. The Large-Scale Movement of Saharan Air Outbreaks over the Northern Equatorial Atlantic , 1972 .
[4] Graeme L. Stephens,et al. On the radiative effects of dust on tropical convection , 2004 .
[5] A. da Silva,et al. Quantification of dust-forced heating of the lower troposphere , 1998, Nature.
[6] C. Velden,et al. ARTICLES: The Impact of the Saharan Air Layer on Atlantic Tropical Cyclone Activity. , 2004 .
[7] B. Holben,et al. Validation of MODIS aerosol retrieval over ocean , 2002 .
[8] W. Paul Menzel,et al. The MODIS cloud products: algorithms and examples from Terra , 2003, IEEE Trans. Geosci. Remote. Sens..
[9] R. Reynolds,et al. The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.
[10] Toby N. Carlson,et al. Vertical and areal distribution of Saharan dust over the western equatorial north Atlantic Ocean , 1972 .
[11] W. Menzel,et al. Discriminating clear sky from clouds with MODIS , 1998 .
[12] E. Vermote,et al. Operational remote sensing of tropospheric aerosol over land from EOS moderate resolution imaging spectroradiometer , 1997 .
[13] W. Paul Menzel,et al. Cloud and aerosol properties, precipitable water, and profiles of temperature and water vapor from MODIS , 2003, IEEE Trans. Geosci. Remote. Sens..
[14] Yoram J. Kaufman,et al. Evaluation of the Moderate‐Resolution Imaging Spectroradiometer (MODIS) retrievals of dust aerosol over the ocean during PRIDE , 2003 .