Articles | Volume 19, issue 1
Atmos. Chem. Phys., 19, 205–218, 2019
https://doi.org/10.5194/acp-19-205-2019
Atmos. Chem. Phys., 19, 205–218, 2019
https://doi.org/10.5194/acp-19-205-2019
Research article
07 Jan 2019
Research article | 07 Jan 2019

Quantifying the direct radiative effect of absorbing aerosols for numerical weather prediction: a case study

Mayra I. Oyola et al.

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Cited articles

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Alpert, P., Krichak, S. O., Tsidulko, M., Shafir, H., and Joseph, J. H.: A dust prediction system with TOMS initialization, Mon. Weather Rev., 130, 2335–2345, https://doi.org/10.1175/1520-0493(2002)130<2335:ADPSWT>2.0.CO;2, 2002. 
Bauer, S. E. and Menon, S.: Aerosol direct, indirect, semidirect, and surface albedo effects from sector contributions based on the IPCC AR5 emissions for preindustrial and present-day conditions, J. Geophys. Res., 117, D01206, https://doi.org/10.1029/2011JD016816, 2012. 
Bucholtz, A., Hlavka, D. L., McGill, M. J., Schmidt, K. S., Pilewskie, P., Davis, S. M., Reid, E. A., and Walker, A. L.:  Directly measured heating rates of a tropical subvisible cirrus cloud, J. Geophys. Res., 115, D00J09, https://doi.org/10.1029/2009JD013128, 2010. 
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We conceptualized the aerosol radiative impact of an inline aerosol analysis field coupled with a global meteorological forecast system utilizing NAAPS and NAVGEM analysis and surface albedo fields. Model simulations were compared with in situ validation data collected during the NASA 2013 SEAC4RS experiment. Instantaneous heating rates peaked around 7 K day-1 in the lower part of the troposphere, while the HSRL profiles resulted in values of up to 18 K day-1 in the in the mid-troposphere.
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