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https://gmd.copernicus.org/articles/17/607/2024/

*Authors*
Haiqin Li <[email protected]>, Georg A. Grell, Ravan Ahmadov, Li Zhang, Shan
Sun, Jordan Schnell, and Ning Wang
*Citations*: Li, H., Grell, G. A., Ahmadov, R., Zhang, L., Sun, S.,
Schnell, J., and Wang, N.: A simple and realistic aerosol emission approach
for use in the Thompson–Eidhammer microphysics scheme in the NOAA UFS
Weather Model (version GSL global-24Feb2022), Geosci. Model Dev., 17,
607–619, https://doi.org/10.5194/gmd-17-607-2024, 2024.

*Published: 25 Jan 2024*
*Abstract*

A physics suite under development at NOAA's Global Systems Laboratory (GSL)
includes the aerosol-aware double-moment Thompson–Eidhammer microphysics
(TH-E MP) scheme. This microphysics scheme uses two aerosol variables
(concentrations of water-friendly aerosol (WFA) and ice-friendly aerosol
(IFA) numbers) to include interactions with some of the physical processes.
In the original implementation, WFA and IFA depended on emissions derived
from climatologies. In our approach, using the Common Community Physics
Package (CCPP), we embedded modules of sea-salt emissions, dust emissions,
and biomass-burning emissions, as well as of anthropogenic aerosol
emissions, into the Unified Forecast System (UFS) to provide realistic
aerosol emissions for these two variables. This represents a very simple
approach with no additional tracer variables and therefore very limited
additional computing cost. We then evaluated a comparison of simulations
using the original TH-E MP approach, which derives the two aerosol
variables using empirical emission formulas from climatologies (CTL) and
simulations that use the online emissions (EXP). Aerosol optical depth
(AOD) was derived from the two variables and appears quite realistic in the
runs with online emissions when compared to analyzed fields. We found less
resolved precipitation over Europe and North America from the EXP run,
which represents an improvement compared to observations. Also interesting
are moderately increased aerosol concentrations over the Southern Ocean
from the EXP run, which invigorate the development of cloud water and
enhance the resolved precipitation in those areas. This study shows that a
more realistic representation of aerosol emissions may be useful when using
double-moment microphysics schemes.

*Source: EGU Sphere*

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