Abstract

Abstract. The FLEXible PARTicle dispersion model FLEXPART, first released in 1998, is a Lagrangian particle dispersion model developed to simulate atmospheric transport over large and mesoscale distances. Due to FLEXPART's success and its open source nature, different limited area model versions of FLEXPART were released making it possible to run FLEXPART simulations by ingesting WRF (Weather Research Forecasting model), COSMO (Consortium for Small-scale Modeling) or MM5 (mesoscale community model maintained by Penn State university) meteorological fields on top of the ECMWF (European Centre for Medium-Range Weather Forecasts) and GFS (Global Forecast System) meteorological fields. Here, we present a new FLEXPART limited area model that is compatible with the AROME mesoscale meteorological forecast model (the Applications of Research to Operations at Mesoscale model).1 FLEXPART-AROME was originally developed to study mesoscale transport around La Réunion, a small volcanic island in the southwest Indian Ocean with a complex orographic structure, which is not well represented in current global operational models. We present new turbulent modes in FLEXPART-AROME. They differ from each other by dimensionality, mixing length parameterization, turbulent transport constraint interpretation and time step configuration. A novel time step was introduced in FLEXPART-AROME. Performances of new turbulent modes are compared to the ones in FLEXPART-WRF by testing the conservation of well-mixedness by turbulence, the dispersion of a point release at the surface and the marine boundary layer evolution around Réunion. The novel time step configuration proved necessary to conserve the well-mixedness in the new turbulent modes. An adaptive vertical turbulence time step was implemented, allowing the model to adapt on a finer timescale when significant changes in the local turbulent state of the atmosphere occur.

Highlights

  • Atmospheric transport models are divided into Eulerian and Lagrangian transport models

  • The Lagrangian models on the other hand describe the evolution of air masses in pregenerated 3-D meteorological fields obtained from a numerical weather prediction (NWP) model, allowing precise and fast modeling of atmospheric tracers released from point sources

  • FLEXPART-AROME was developed by the LACy laboratory to model particle transport around La Réunion, a French overseas territory which is covered by an AROME grid in the southwest Indian Ocean (SWIO) with 2.5 km × 2.5 km resolution in a Lambert conformal projection

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Summary

Introduction

Atmospheric transport models are divided into Eulerian and Lagrangian transport models. The limited area versions of FLEXPART (FLEXPART-WRF (Brioude et al, 2013), FLEXPARTCOSMO (Henne et al, 2016), FLEXPART-MM5) allow particle transport in higher-resolved grids to better represent mesoscale phenomena. The AROME (Applications de la Recherche à l’Opérationnel à Méso-Echelle) mesoscale forecast model has been the operation weather forecasting model at Météo France since 2008. It is designed for fine-scale modeling with grid sizes ranging from 0.5 to 2.5 km. FLEXPART-AROME was developed by the LACy laboratory to model particle transport around La Réunion, a French overseas territory which is covered by an AROME grid in the southwest Indian Ocean (SWIO) with 2.5 km × 2.5 km resolution in a Lambert conformal projection. The 3-D turbulent kinetic energy (TKE) field from the NWP in FLEXPART in order to harmonize turbulent motions between both

Turbulent inconsistency between NWP and LPDM
Turbulent scheme development
Particle time loop
Thomson’s approach
Turbulent mixing length
Validation
Turbulent conservation of a well-mixed passive tracer
Marine boundary layer tracer
Computation time
Findings
Conclusions
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