Constraining the uncertainty of urbanization effect on surface air temperature change over the Beijing-Tianjin-Hebei region in China

被引:1
|
作者
He, Yuting [1 ,2 ]
Feng, Jinming [1 ,4 ]
Wang, Jun [1 ]
Cao, Lijuan [3 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia R, Beijing, Peoples R China
[2] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
[3] China Meteorol Adm, Natl Meteorol Informat Ctr, Beijing, Peoples R China
[4] Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia R, Beijing 100029, Peoples R China
来源
ATMOSPHERIC SCIENCE LETTERS | 2023年 / 24卷 / 07期
基金
中国国家自然科学基金;
关键词
contribution; fraction of urban build-up area; surface air temperature; urbanization effect; MAINLAND CHINA; URBAN BIAS; TRENDS; IMPACT;
D O I
10.1002/asl.1160
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Quantitative assessment of urbanization effect on surface air temperature (SAT) change provides crucial basis for formal detection and attribution analyses of climate change. However, debates about urbanization-related warming bias in documented regional SAT trend still persist, mainly due to different determination of rural stations. Here the urbanization effect on SAT change over the Beijing-Tianjin-Hebei region in China during 1980-2019 is estimated through three kinds of ways (i.e., comparisons between urban and rural stations [arithmetically station-averaged], urban-dominated and rural-dominated patches [patch-weighted mean], and realistic urban and rural areas [area weighted mean]). The last method explicitly takes urban and rural land cover fractions into account when calculating urban/rural and regional mean SAT trends. Urbanization-induced warming in the annual mean SAT change of urban stations (areas) through the three ways are estimated as 0.159 degrees C, 0.195 degrees C, and 0.138 degrees C per decade, respectively. And urbanization effect on regional averaged annual mean SAT calculated by patch-weighted and area-weighted methods are 0.113 degrees C and 0.050 degrees C per decade, respectively, which account for 33.8% and 14.8% of the total regional warming. The urbanization effect on observed SAT change estimated by considering realistic urban/rural land cover proportions is much lower than traditional station-unweighted way.
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页数:9
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