Synergy of active and passive airborne observations for heating rate calculation during the AEROCLO-sA field campaign in Namibia
Synergie des observations aéroportées actives et passives pour le calcul du taux de réchauffement lors de la campagne de terrain AEROCLO-sA en Namibie
Ventura, Mégane ; Waquet, Fabien ; Chiapello, Isabelle ; Brogniez, Gérard ; Parol, Frédéric ; Auriol, Frédérique ; Loisil, Rodrigue ; Delegove, Cyril ; Blarel, Luc ; Dubovik, Oleg ; Mallet, Marc ; Flamant, Cyrille ; Formenti, Paola
Année de publication
2025
Aerosols have important effects on both local and global climate, as well as on clouds and precipitations. We present original results derived from the airborne observations acquired from the AErosol RadiatiOn and CLOud in Southern Africa (AEROCLO-sA) field campaign led in Namibia in August and September 2017. In order to quantify the aerosols' radiative impact on the Namibian regional radiative budget, we use an innovative approach that combines the OSIRIS polarimeter, an airborne prototype of the future 3MI polarimeter of ESA, and lidar data to derive the heating rate of the aerosols. To calculate this parameter we use a radiative transfer code, meteorological parameters provided by dropsondes, and OSIRIS-retrieved aerosol optical thickness, size, and absorption above clouds. This approach is evaluated during massive transports of biomass-burning particles above clouds. We present vertical profiles of heating rates computed in the solar and thermal parts of the spectrum. Our results indicate strong positive heating rate values retrieved above clouds due to aerosols, between +2 and +5 K per day (vertically averaged). Within the smoke layer, water vapor's cooling effect through infrared radiation generally balances its warming effect from solar radiation. At the top of the layer, a stronger cooling effect of ?1.5 K d?1 often dominates due to water vapor. In order to validate this methodology, we use irradiance measurements acquired by aircraft during spiral descent during dedicated parts of their flights, which provides direct measurements of irradiance distribution and heating rates as functions of the altitude. Despite the challenges posed by cloud horizontal variability observed during the spiral descent, simulated and measured results generally agree in most cases. Finally, we discuss the possibility of applying this method to available and future spaceborne passive and active sensors.</div>
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