Research on quantitative evaluations of heat islands for the Beijing-Tianjin-Hebei Urban Agglomeration

Yonghong, 刘勇洪 Liu; Xiaoyi, 房小怡 Fang; Shuo, 张硕 Zhang; Qingzu, 栾庆祖 Luan; Weijun, 权维俊 Quan

doi:10.5846/stxb201606031074

Cited by 1 publication

(1 citation statement)

References 0 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…As the main parameter for the quantitative study of surface urban heat islands (SUHIs), LST is an important data source for monitoring urban thermal environments [ 4 ]. At present, domestic and foreign scholars have made many achievements in the quantitative assessment of SUHI [ 16 , 17 ], the distribution characteristics of SUHI [ 18 , 19 ], and the analysis of SUHI influencing factors [ 20 , 21 ], based on LST. Studies have shown that the heterogeneity of urban and suburban surfaces, caused by the substitution of natural surfaces by large impervious surfaces during urbanization, is the fundamental reason for the formation of SUHI [ 22 , 23 , 24 ].…”

Section: Introductionmentioning

confidence: 99%

A Quantitative Study of a Directional Heat Island in Hefei, China Based on Multi-Source Data

Shi

Jiang

et al. 2023

Sensors

View full text Add to dashboard Cite

Surface urban heat islands (SUHIs) are essential for evaluating urban thermal environments. However, current quantitative studies of SUHIs ignore the thermal radiation directionality (TRD), which directly affects study precision; furthermore, they fail to assess the effects of TRD characteristics at different land-use intensities, on the quantitative studies of SUHIs. To bridge this research gap, this study eliminates the interference of atmospheric attenuation and daily temperature variation factors, in quantifying the TRD based on land surface temperature (LST), from MODIS data and station air temperature data for Hefei (China) from 2010–2020. The influence of TRD on SUHI intensity quantification was evaluated by comparing the TRD under different land-use intensities in Hefei. The results show that: (1) daytime and nighttime directionality can reach up to 4.7 K and 2.6 K, and occur in areas with the highest and medium urban land-use intensity, respectively. (2) There are two significant TRD hotspots for daytime urban surfaces, where the sensor zenith angle is approximately the same as the forenoon solar zenith angle, and where the sensor zenith angle is near its nadir in the afternoon. (3) The TRD can contribute up to 2.0 K to the results of assessing the SUHI intensity based on satellite data, which is approximately 31–44% of the total SUHI in Hefei.

show abstract