4.7 Article

Diurnal and seasonal patterns of global urban dry islands

期刊

ENVIRONMENTAL RESEARCH LETTERS
卷 17, 期 5, 页码 -

出版社

IOP Publishing Ltd
DOI: 10.1088/1748-9326/ac68f8

关键词

urban dry island; urban moisture island; urban heat island; urban climate; urbanization effects; humidity

资金

  1. National University of Singapore [223637-A0001]
  2. NERC [NE/S003495/1]
  3. 'The Branco Weiss Fellowship-Society in Science'

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Urban heat islands (UHIs) are extensively studied, but there is less research on urban-rural differences in humidity. This study quantifies the seasonal and diurnal patterns of urban dry or moisture islands (UDIs, UMIs) using global temperature and humidity measurements. The results show that absolute UDI is largest during daytime, while relative UDI is largest during night. These findings are essential for understanding the impacts of humidity on urban ecology and building energy consumption.
Urban heat islands (UHIs) are a widely studied phenomenon, while research on urban-rural differences in humidity, the so called urban dry or moisture islands (UDIs, UMIs), is less common and a large-scale quantification of the seasonal and diurnal patterns of the UDI is still lacking. However, quantification of the UDI/UMI effect is essential to understand the impacts of humidity on outdoor thermal comfort, building energy consumption, and urban ecology in cities worldwide. Here, we use a set of globally distributed air temperature and humidity measurements (1089 stations) to quantify diurnal and seasonal patterns of UHI and UDI resulting from rapid urbanization over many regions of the world. The terms 'absolute UDI' and 'relative UDI' are defined, which quantify urban-rural differences in actual and relative humidity metrics, respectively. Results show that absolute UDI is largest during daytime with the peak humidity decrease in urban areas occurring during late afternoon hours. In contrast, relative UDI is largest during night and the peak urban relative humidity (RH) decrease and vapor pressure deficit (VPD) increase occurs in the late evening hours with values of around -10% to -11% for RH and 2.9-3.6 hPa for VPD between 20-00 local time during summer. Relative and absolute UDIs are largest during the warm season, except for daytime RH UDI, which does not show any seasonal pattern. In agreement with literature, canopy air UHI is shown to be a nighttime phenomenon, which is larger during summer than winter. Relative UDI is predominantly caused by changes in actual humidity during day and UHI during nighttime.

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