4.7 Article

Mesoscale spatio-temporal variability of airborne lidar-derived aerosol properties in the Barbados region during EUREC4 A

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 22, Issue 2, Pages 1271-1292

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-22-1271-2022

Keywords

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Funding

  1. European Research Council (ERC) under the European Union [694768]
  2. French Space Agency CNES through the EECLAT project

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During the EUREC4A field campaign, 20 ATR-42 scientific flights were conducted over the tropical Atlantic, off the coast of Barbados, with the use of a sideway-pointing lidar to retrieve the optical properties of aerosols in the sub-cloud layer and below the trade wind inversion. The study identified two distinct periods with significant aerosol contents related to trade wind and tropical regimes, highlighting the mixings of dust and carbonaceous aerosols from West Africa. The aerosol vertical structures were well reproduced using atmospheric composition reanalyses from CAMS when compared with lidar-derived vertical profiles.
From 23 January to 13 February 2020, 20 ATR-42 scientific flights were conducted in the framework of the EUREC4A field campaign over the tropical Atlantic, off the coast of Barbados (13 degrees 30' N, -58 degrees 30' W). By means of a sideway-pointing lidar, these flights allowed us to retrieve the optical properties of the aerosols found in the sub-cloud layer and below the trade wind inversion. Two distinct periods with significant aerosol contents were identified in relationship with the so-called trade wind and tropical regimes, respectively. For these two regimes, mixings of two air mass types encompassing dust and carbonaceous aerosols have been highlighted. Both were mainly from West Africa with similar optical contributions and linked to dust uptake above Sahara and biomass burning between Guinea-Bissau and Cote d'Ivoire. In the tropical transport regime, the wind within the planetary boundary layer is stronger and favours a contribution of marine aerosols (sulfate and sea salt aerosol components) in shallower aerosol layers than for the trade wind transport regime. The latter is responsible for advecting dust-biomass-burning-aerosol mixtures in the deeper, well-mixed layer, in part due to the complex interactions of the easterly flow from West Africa with mid-latitude dynamics. The aerosol vertical structures appear to be well reproduced using atmospheric composition reanalyses from CAMS when comparing with lidar-derived vertical profiles. The competition between the two types of transport regimes leads to strong heterogeneity in the optical properties of the horizontal aerosol field. Our study highlights the transport regime under which a significant mixture of dust and biomass burning aerosols from West Africa can be observed over the Caribbean and Barbados in particular, namely the trade wind regime.

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