Review comments for "The Lagrangian particle dispersion model FLEXPART version 10.3"
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Microbial richness and air chemistry in aerosols above the PBL confirm 2,000-km long-distance transport of potential human pathogens. [PDF]
Rodó X +13 more
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Global environmental plastic dispersal under OECD policy scenarios toward 2060. [PDF]
Sonke JE +3 more
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Emissions of HFC-23 do not reflect commitments made under the Kigali Amendment. [PDF]
Adam B +16 more
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A Comparative Analysis of Satellite-Derived CO Retrievals During the 2020 Wildfires in North America. [PDF]
Marey HS +6 more
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Effects of improved interpolation in the wet-scavenging scheme of FLEXPART
, 2021The Lagrangian dispersion model FLEXPART v10.4 uses cloud water content, temperature, and precipitation rates to calculate wet scavenging. Currently, only precipitation fields are interpolated spatially to the particle positions.
Anne Tipka, P. Seibert
semanticscholar +2 more sources
Revamping FLEXPART for the next generation of simulations
2022<p>The Lagrangian atmospheric transport model, FLEXPART, is used to investigate a broad spectrum of topics within the atmospheric sciences, from the propagation of particles emitted during nuclear accidents to global moisture transport.
Lucie Bakels +7 more
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Scavenging and Convective Clouds in the Lagrangian Dispersion Model FLEXPART
2017The Lagrangian particle dispersion model (LPDM) FLEXPART includes a parameterisation of wet scavenging. With FLEXPART version 8, an improved scheme was introduced which distinguishes between in-cloud and below-cloud scavenging. However, clouds are only diagnosed from grid-scale variables and thus convective clouds are neglected. Although the convection
Philipp, Anne, Seibert, Petra
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Seeking the origins of Arctic ice nucleating particles with FLEXPART-WRF
2023The Arctic region is subject to polar amplification, causing it to warm approximately four times faster than the global average. The predominance of ice and mixed-phase clouds in high latitude regions causes strong uncertainties in the determination of the cloud radiative effect and the cloud feedback.
Da Silva, Anderson +2 more
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