Spatiotemporal effects of urban ecological land transitions to thermal environment change in mega-urban agglomeration

被引:9
|
作者
Feng, Rundong [1 ,2 ]
Wang, Fuyuan [1 ]
Zhou, Meijing [3 ,4 ]
Liu, Shenghe [1 ]
Qi, Wei [1 ]
Li, Li [1 ,2 ]
机构
[1] Inst Geog Sci & Nat Resources Res, Chinese Acad Sci, Key Lab Reg Sustainable Dev Modeling, Beijing 100101, Peoples R China
[2] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
[3] Cent South Univ, Sch Business, Changsha 410083, Peoples R China
[4] Fraunhofer Inst Syst & Innovat Res, Competence Ctr Sustainabil & Infrastruct Syst, D-76139 Karlsruhe, Germany
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Urban ecological land transition; Land surface temperature; Spatiotemporal patterns; Interaction effects; Mega-urban agglomeration; SURFACE TEMPERATURE; HEAT ISLANDS; MITIGATION; GREENSPACE; DYNAMICS; PATTERNS; REGION;
D O I
10.1016/j.scitotenv.2022.156158
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Urban ecological land transitions (UELTs) have far-reaching effects on the thermal environment, but their dynamic ef-fects in urban agglomerations remain poorly understood. This study defines the UELTs concept and quantifies its spa-tiotemporal effects and driving mechanisms on land surface temperature interdecadal variations (LSTIVs) in the Guangdong-Hong Kong-Macao Greater Bay Area using remote sensing, fuzzy overlay, shape-weighted landscape evo-lution index, and Geodetector methods. The results showed that UELTs shifted from degradation, increasing pressure, and decreasing vegetation proportion in the central city to scattered restoration, pressure relief, and increasing vege-tation proportion in 2010-2020. LSTIVs simultaneously transitioned from rapid growth and contiguous expansion to reduction and dispersion. Moreover, the contribution of UELTs to LSTIVs increased by 19.49% from 2000 to 2020, and gradually shifted from being driven by dominant transition (isolating and adjacent degradation) (mean q = 0.58) to recessive transition (increased population and construction land pressure) (mean q = 0.62), where q is the determi-nant power. Interactions between edge-expansion and infilling restoration with the blue-green ratio (BGR; i.e., ratio of waterbodies to vegetation), habitat quality, and population layout had significant effects on LSTIVs. In addition, the relative magnitude of the effect of UEL restoration-degradation and BGR on LSTIVs was not fixed, but rather re-lated to their interaction effect and the urban agglomeration development stage. Therefore, in addition to promoting an increase in UEL, optimizing the landscape structure of UEL (e.g., increasing aggregation and connectivity, adjusting BGR) and UEL distribution with other human factors are also crucial to reduce the urban thermal environment.
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页数:12
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