Observed Relationships Between the Urban Heat Island, Urban Pollution Island, and Downward Longwave Radiation in the Beijing Area

• Published in: Earth and space science (Hoboken, N.J.) Vol. 7; no. 6
• Main Authors: Li, Ju, Zhou, Mingyu, Lenschow, Donald H., Cheng, Zhigang, Dou, Youjun
• Format: Journal Article
• Language: English
• Published: Hoboken John Wiley & Sons, Inc 01.06.2020; American Geophysical Union (AGU)
• Subjects: Aerosols; Air pollution; Air temperature; downward longwave radiation; Humidity; Investigations; Mitigation; Net radiation; Particulate matter; Pollutants; Radiation; Rural areas; Suburban areas; Summer; Temperature; Topography; Urban areas; urban heat island; Urban heat islands; urban pollution island; Water vapor; Winter; Beijing China
• ISSN: 2333-5084; 2333-5084
• DOI: 10.1029/2020EA001100

We used the mean air temperature and particulate matter concentration at northern and southern rural stations as rural background values to calculate the urban heat island intensity (UHII) and urban pollution island intensity (UPII) for Beijing. The correlation between UHII and UPII is significantly negative in winter during the daytime and nighttime when selecting southern rural background stations but significantly positive in spring during both daytime and nighttime and in winter during the nighttime when selecting northern rural background stations. The downward longwave radiation (DLR) is highly correlated with surface air temperature and water vapor, and with particulate matter concentration in winter and summer. Water vapor also has a high correlation with particulate matter concentration in winter and summer. Winter data were used to investigate the particulate matter contribution to DLR to minimize the effect of humidity. The results indicate that in winter the urban area DLR and net radiation increased more than rural area under polluted conditions compared with clean conditions, which may lead to an increase in UHII. But in other seasons with more moisture, the aerosol effect on DLR is smaller than water vapor. Our results imply that the contribution of air pollutants to DLR had been overestimated in recent studies without removing water vapor effects on the longwave radiation. We suggest that the interaction between the urban heat island and the urban pollution island and related mitigation strategies needs to be carefully studied in the future by considering different climate zone and seasons. Key Points The urban pollution island intensity is more sensitive to the selection of rural background stations than the urban heat island intensity The downward longwave radiation is highly correlated with temperature and water vapor and with particulate matter in winter Pollutants can enhance downward longwave radiation and net radiation distributions in urban areas more than in rural areas only in winter