Abstract

Abstract. In this paper, we rectify inconsistencies that emerge in the Weather Research and Forecasting model with chemistry (WRF-Chem) v3.2 code when using the Goddard Chemistry Aerosol Radiation and Transport (GOCART) aerosol module. These inconsistencies have been reported, and corrections have been implemented in WRF-Chem v4.1.3. Here, we use a WRF-Chem experimental setup configured over the Middle East (ME) to estimate the effects of these inconsistencies. Firstly, we show that the old version underestimates the PM2.5 diagnostic output by 7 % and overestimates PM10 by 5 % in comparison with the corrected one. Secondly, we demonstrate that submicron dust particles' contribution was incorrectly accounted for in the calculation of optical properties. Therefore, aerosol optical depth (AOD) in the old version was 25 %–30 % less than in the corrected one. Thirdly, we show that the gravitational settling procedure, in comparison with the corrected version, caused higher dust column loadings by 4 %–6 %, PM10 surface concentrations by 2 %–4 %, and mass of the gravitationally settled dust by 5 %–10 %. The cumulative effect of the found inconsistencies led to the significantly higher dust content in the atmosphere in comparison with the corrected WRF-Chem version. Our results explain why in many WRF-Chem simulations PM10 concentrations were exaggerated. We present the methodology for calculating diagnostics we used to estimate the impacts of introduced code modifications. We share the developed Merra2BC interpolator, which allows processing Modern-Era Retrospective Analysis for Research and Applications, version 2 (MERRA-2) output for constructing initial and boundary conditions for chemical species and aerosols.

Highlights

  • Produced by wind erosion, mineral dust is one of the major drivers of climate over the Middle East (ME) (Osipov et al, 2015)

  • We demonstrate the methodology for calculating diagnostics that we used to estimate the impact of the introduced corrections

  • To calculate the chemical IC&BC using MERRA-2 output, we develop an interpolator (Merra2BC; Ukhov and Stenchikov, 2020), which uses gaseous and aerosol fields from MERRA2 reanalysis to construct the IC&BC required by the WRFChem simulation

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Summary

Introduction

Mineral dust is one of the major drivers of climate over the Middle East (ME) (Osipov et al, 2015).

WRF-Chem experimental setup
Dust emission tuning
Tuning the C parameter
Tuning the sp fractions
Results
Calculation of aerosol optical properties
Effect of small particles
Bin concentration interpolation
Gravitational settling
Case study
Effect of initial and boundary conditions
Conclusions
Reconstruction of the pressure in MERRA-2 and in WRF-Chem
Mapping chemical species between MERRA-2 and WRF-Chem
Interpolation procedure
Typical workflow
Grid column area
Dust emission
Gravitational settling and dry deposition
Dust in the atmosphere
Full Text
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