Modeling of the anthropogenic heat flux and its effect on regional meteorology and air quality over the Yangtze River Delta region, China

Anthropogenic heat (AH) emissions from human activities caused by urbanization can affect the city environment. Based on the energy consumption and the gridded demographic data, the spatial distribution of AH emission over the Yangtze River Delta (YRD) region is estimated. Meanwhile, a new method for the AH parameterization is developed in the WRF/Chem model, which incorporates the gridded AH emission data with the seasonal and diurnal variations into the simulations. By running this upgraded WRF/Chem for 2 typical months in 2010, the impacts of AH on the meteorology and air quality over the YRD region are studied. The results show that the AH fluxes over the YRD have been growing in recent decades. In 2010, the annual-mean values of AH over Shanghai, Jiangsu and Zhejiang are 14.46, 2.61 and 1.63aEuro-WaEuro-m(-2), respectively, with the high value of 113.5aEuro-WaEuro-m(-2) occurring in the urban areas of Shanghai. These AH emissions can significantly change the urban heat island and urban-breeze circulations in the cities of the YRD region. In Shanghai, 2aEuro-m air temperature increases by 1.6aEuro-A degrees C in January and 1.4aEuro-A degrees C in July, the PBLH (planetary boundary layer height) rises up by 140aEuro-m in January and 160aEuro-m in July, and 10aEuro-m wind speed is enhanced by 0.7aEuro-maEuro-s(-1) in January and 0.5aEuro-maEuro-s(-1) in July, with a higher increment at night. The enhanced vertical movement can transport more moisture to higher levels, which causes the decrease in water vapor at ground level and the increase in the upper PBL (planetary boundary layer), and thereby induces the accumulative precipitation to increase by 15-30aEuro-% over the megacities in July. The adding of AH can impact the spatial and vertical distributions of the simulated pollutants as well. The concentrations of primary air pollutants decrease near the surface and increase at the upper levels, due mainly to the increases in PBLH, surface wind speed and upward air vertical movement. But surface O-3 concentrations increase in the urban areas, with maximum changes of 2.5aEuro-ppb in January and 4aEuro-ppb in July. Chemical direct (the rising up of air temperature directly accelerates surface O-3 formation) and indirect (the decrease in NOx at the ground results in the increase in surface O-3) effects can play a significant role in O-3 changes over this region. The meteorology and air pollution predictions in and around large urban areas are highly sensitive to the anthropogenic heat inputs, suggesting that AH should be considered in the climate and air quality assessments.