The impact of land use/cover change on extreme temperatures on the Yangtze River Delta, China

被引:1
|
作者
Zhu, Nina [1 ,2 ]
Yang, Haiqing [3 ,4 ]
Zhu, Mengyu [5 ]
Li, Dahui [6 ]
机构
[1] East China Normal University, Ctr Modern Chinese City Studies, Shanghai 200062, Peoples R China
[2] East China Normal Univ, Inst Urban Dev, Shanghai 200062, Peoples R China
[3] China West Normal Univ, Sch Geograph Sci, Nanchong 637009, Peoples R China
[4] China West Normal Univ, Sichuan Prov Engn Lab Monitoring & Control Soil Er, Nanchong 637009, Peoples R China
[5] Fuzhou Univ, Coll Chem Engn, Fuzhou 350108, Peoples R China
[6] Sun Yat Sen Univ, Sch Geospatial Engn & Sci, Zhuhai 519082, Peoples R China
来源
ERDE | 2022年 / 153卷 / 04期
关键词
Yangtze River Delta; extreme temperature; land use; cover change; contribution rate; ensemble empirical mode decomposition; observation minus reanalysis; CLIMATE-CHANGE; HOT EXTREMES; COVER CHANGE; URBANIZATION; HEAT; INDEXES;
D O I
10.12854/erde-2022-590
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
The contribution from land use/cover change (LUCC) toward temperature in recent decades is of great concern across the globe. Although there have been many studies, most of them focus on the discussion of average temperature and lack a discussion of extreme temperatures. In this study, we first investigated the spatio-temporal changes in extreme temperatures in the Yangtze River Delta during 1980-2020 using the ensemble empirical mode decomposition (EEMD) method. Then, we explored the impact of LUCC on extreme temperatures using the observation minus reanalysis (OMR) method. Finally, the relationship between the normalized difference vegetation index (NDVI) and extreme tempera-tures was analyzed using the correlation analysis method. We found that: (1) extreme temperatures have a nonlinear variation characteristics on different time scales. Extremely high temperatures (EHT) clearly exhibited a monthly time scale (quasi-3-month), an interannual time scale (quasi-1-year, quasi-2-year, quasi-3-year and quasi-5-year), and an in-terdecadal time scale (quasi-10-year and quasi-35-year). Extremely low temperatures (ELT) also clearly exhibited a monthly time scale (quasi-3-month), an interannual scale (quasi-1-year, quasi-2-year, quasi-3-year and quasi-6-year), and an interdecadal scale (quasi-10-year and quasi-20-year). (2) EHT showed an east-middle-west staggered phase and ELT showed a southeast-northwest anti-phase characteristic in spatial distribution. (3) The contribution rates of LUCC on EHT and ELT are 53.6% and 92.4%, respectively, which are higher than for the average temperature (40%). (4) The monthly time scale response of the NDVI to extreme temperatures is more regionally concentrated and significant than that on the interannual time scale in spatial distribution. This paper makes up for the insufficiency of the impact of land use/cover changes on extreme temperature changes at multiple time scales and enriches our understanding of climate change.
引用
收藏
页码:219 / 238
页数:20
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