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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 6
Geosci. Model Dev., 7, 2709–2715, 2014
https://doi.org/10.5194/gmd-7-2709-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The community version of the Weather Research and Forecasting...

Geosci. Model Dev., 7, 2709–2715, 2014
https://doi.org/10.5194/gmd-7-2709-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Development and technical paper 19 Nov 2014

Development and technical paper | 19 Nov 2014

The impact of aerosol optical depth assimilation on aerosol forecasts and radiative effects during a wild fire event over the United States

D. Chen1, Z. Liu1, C. S. Schwartz1, H.-C. Lin1, J. D. Cetola2, Y. Gu3, and L. Xue1 D. Chen et al.
  • 1National Center for Atmospheric Research, Boulder, Colorado, USA
  • 2Air Force Weather Agency, Omaha, Nebraska, USA
  • 3University of California, Los Angeles, Los Angeles, California, USA

Abstract. The Gridpoint Statistical Interpolation three-dimensional variational data assimilation (DA) system coupled with the Weather Research and Forecasting/Chemistry (WRF/Chem) model was utilized to improve aerosol forecasts and study aerosol direct and semi-direct radiative feedbacks during a US wild fire event. Assimilation of MODIS total 550 nm aerosol optical depth (AOD) retrievals clearly improved WRF/Chem forecasts of surface PM2.5 and organic carbon (OC) compared to the corresponding forecasts without aerosol data assimilation. The scattering aerosols in the fire downwind region typically cooled layers both above and below the aerosol layer and suppressed convection and clouds, which led to an average of 2% precipitation decrease during the fire week. This study demonstrated that, even with no input of fire emissions, AOD DA improved the aerosol forecasts and allowed a more realistic model simulation of aerosol radiative effects.

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