Urban Surface Temperature Reduction via the Urban Aerosol Direct Effect: A Remote Sensing and WRF Model Sensitivity Study

<table>Aerosol reduction on surface insolation calculated from the radiative transfer model for Beijing and New York City in January and July, respectively.</table>

Advances in Meteorology

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Figure 5

Figure 5: Urban Surface Temperature Reduction via the Urban Aerosol Direct Effect: A Remote Sensing and WRF Model Sensitivity Study 