Simulation of the radiative effect of haze on the urban hydrological cycle using reanalysis data in Beijing

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Kokkonen , T V , Grimmond , S , Murto , S , Huizhi , L , Sundström , A-M & Järvi , L 2019 , ' Simulation of the radiative effect of haze on the urban hydrological cycle using reanalysis data in Beijing ' , Atmospheric Chemistry and Physics , vol. 19 , no. 10 , pp. 7001-7017 . https://doi.org/10.5194/acp-19-7001-2019

Title: Simulation of the radiative effect of haze on the urban hydrological cycle using reanalysis data in Beijing
Author: Kokkonen, Tom V.; Grimmond, Sue; Murto, Sonja; Huizhi, Liu; Sundström, Anu-Maija; Järvi, Leena
Contributor: University of Helsinki, INAR Physics
University of Helsinki, Institute for Atmospheric and Earth System Research (INAR)
Date: 2019-05-24
Language: eng
Number of pages: 17
Belongs to series: Atmospheric Chemistry and Physics
ISSN: 1680-7324
URI: http://hdl.handle.net/10138/303117
Abstract: Although increased aerosol concentration modifies local air temperatures and boundary layer structure in urban areas, little is known about its effects on the urban hydrological cycle. Changes in the hydrological cycle modify surface runoff and flooding. Furthermore, as runoff commonly transports pollutants to soil and water, any changes impact urban soil and aquatic environments. To explore the radiative effect of haze on changes in the urban surface water balance in Beijing, different haze levels are modelled using the Surface Urban Energy and Water Balance Scheme (SUEWS), forced by reanalysis data. The pollution levels are classified using aerosol optical depth observations. The secondary aims are to examine the usability of a global reanalysis dataset in a highly polluted environment and the SUEWS model performance. We show that the reanalysis data do not include the attenuating effect of haze on incoming solar radiation and develop a correction method. Using these corrected data, SUEWS simulates measured eddy covariance heat fluxes well. Both surface runoff and drainage increase with severe haze levels, particularly with low precipitation rates: runoff from 0.06 to 0.18 mm d−1 and drainage from 0.43 to 0.62 mm d−1 during fairly clean to extremely polluted conditions, respectively. Considering all precipitation events, runoff rates are higher during extremely polluted conditions than cleaner conditions, but as the cleanest conditions have high precipitation rates, they induce the largest runoff. Thus, the haze radiative effect is unlikely to modify flash flooding likelihood. However, flushing pollutants from surfaces may increase pollutant loads in urban water bodies.
Subject: 114 Physical sciences
Urban hydrology
SUEWS
Urban climate
atmospheric pollution
ATMOSPHERIC AEROSOLS
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