Multi-year downscaling application of two-way coupled WRF v3.4 and CMAQ v5.0.2 over east Asia for regional climate and air quality modeling: model evaluation and aerosol direct effects
In this study, a regional coupled climate–chemistry modeling system using the dynamical downscaling technique was established by linking the global Community Earth System Model (CESM) and the regional two-way coupled Weather Research and Forecasting – Community Multi-scale Air Quality (WRF-CMAQ)...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2017-06-01
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Series: | Geoscientific Model Development |
Online Access: | https://www.geosci-model-dev.net/10/2447/2017/gmd-10-2447-2017.pdf |
Summary: | In this study, a regional coupled climate–chemistry
modeling system using the dynamical downscaling technique was established by
linking the global Community Earth System Model (CESM) and the regional
two-way coupled Weather Research and Forecasting – Community Multi-scale Air
Quality (WRF-CMAQ) model for the purpose of comprehensive assessments of
regional climate change and air quality and their interactions within one
modeling framework. The modeling system was applied over east Asia for a
multi-year climatological application during 2006–2010, driven with CESM
downscaling data under Representative Concentration Pathways 4.5 (RCP4.5),
along with a short-term air quality application in representative months in 2013
that was driven with a reanalysis dataset. A comprehensive model evaluation was
conducted against observations from surface networks and satellite
observations to assess the model's performance. This study presents the first
application and evaluation of the two-way coupled WRF-CMAQ model for
climatological simulations using the dynamical downscaling technique. The
model was able to satisfactorily predict major meteorological variables. The
improved statistical performance for the 2 m temperature (T2) in this study
(with a mean bias of −0.6 °C) compared with the Coupled Model
Intercomparison Project Phase 5 (CMIP5) multi-models might be related to the
use of the regional model WRF and the bias-correction technique applied for
CESM downscaling. The model showed good ability to predict PM<sub>2. 5</sub> in
winter (with a normalized mean bias (NMB) of 6.4 % in 2013) and O<sub>3</sub> in
summer (with an NMB of 18.2 % in 2013) in terms of statistical performance
and spatial distributions. Compared with global models that tend to
underpredict PM<sub>2. 5</sub> concentrations in China, WRF-CMAQ was able to capture
the high PM<sub>2. 5</sub> concentrations in urban areas. In general, the two-way
coupled WRF-CMAQ model performed well for both climatological and air quality
applications. The coupled modeling system with direct aerosol feedbacks
predicted aerosol optical depth relatively well and significantly reduced the
overprediction in downward shortwave radiation at the surface (SWDOWN) over
polluted regions in China. The performance of cloud variables was not as good
as other meteorological variables, and underpredictions of cloud fraction
resulted in overpredictions of SWDOWN and underpredictions of shortwave and
longwave cloud forcing. The importance of climate–chemistry interactions was
demonstrated via the impacts of aerosol direct effects on climate and air
quality. The aerosol effects on climate and air quality in east Asia (e.g.,
SWDOWN and T2 decreased by 21.8 W m<sup>−2</sup> and 0.45 °C,
respectively, and most pollutant concentrations increased by 4.8–9.5 % in
January over China's major cities) were more significant than in other
regions because of higher aerosol loadings that resulted from severe regional
pollution, which indicates the need for applying online-coupled models over
east Asia for regional climate and air quality modeling and to study the
important climate–chemistry interactions. This work established a baseline
for WRF-CMAQ simulations for a future period under the RCP4.5 climate
scenario, which will be presented in a future paper. |
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ISSN: | 1991-959X 1991-9603 |