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Enhanced drought resistance of vegetation growth in cities due to urban heat, CO 2 domes and O 3 troughs

Dados Bibliográficos

ID15545265
AutoresPeng Fu (0009-0009-6501-1556, University of Illinois Urbana-Champaign, autor correspondente), Leiqiu Hu (0000-0002-1867-2521, University of Alabama in Huntsville), Elizabeth A Ainsworth (0000-0002-3199-8999, University of Illinois Urbana-Champaign), Xiaonan Tai (0000-0002-3040-3121, New Jersey Institute of Technology), Soe W Myint (0000-0001-7809-1211, Arizona State University), Wenfeng Zhan (0000-0001-7487-821X, Nanjing University), Bethany Blakely (0000-0001-9923-0794, University of Illinois Urbana-Champaign), Bethany J Blakely, Carl J Bernacchi (0000-0002-2397-425X, University of Illinois Urbana-Champaign)
Ano2021
Volume16
Fascículo12
Páginas124052-124052
Data de publicação2021-11-18
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoEnvironmental Research Letters (JOURNAL)
Identificadores do periódicoISSN: 1748-9326 • E-ISSN: 1748-9326
EditoraIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ac3b17
OpenAlexW3216482598
IdiomaEN
Citações recebidas1
Referências citadas48

Sustained increase in atmospheric CO 2 is strongly coupled with rising temperature and persistent droughts. While elevated CO 2 promotes photosynthesis and growth of vegetation, drier and warmer climate can potentially negate this benefit, complicating the prediction of future terrestrial carbon dynamics. Manipulative studies such as free air CO 2 enrichment (FACE) experiments have been useful for studying the joint effect of global change factors on vegetation growth; however, their results do not easily transfer to natural ecosystems partly due to their short-duration nature and limited consideration of climatic gradients and potential confounding factors, such as O 3 . Urban environments serve as a useful small-scale analogy of future climate at least in reference to CO 2 and temperature enhancements. Here, we develop a data-driven approach using urban environments as test beds for revealing the joint effect of changing temperature and CO 2 on vegetation response to drought. Using 75 urban-rural paired plots from three climate zones over the conterminous United States (CONUS), we find vegetation in urban areas exhibits a much stronger resistance to drought than in rural areas. Statistical analysis suggests the drought resistance enhancement of urban vegetation across CONUS is attributed to rising temperature (with a partial correlation coefficient of 0.36) and CO 2 (with a partial correlation coefficient of 0.31) and reduced O 3 concentration (with a partial correlation coefficient of −0.12) in cities. The controlling factor(s) responsible for urban-rural differences in drought resistance of vegetation vary across climate regions, such as surface O 3 gradients in the arid climate, and surface CO 2 and O 3 gradients in the temperate and continental climates. Thus, our study provides new observational insights on the impacts of competing factors on vegetation growth at a large scale, and ultimately, helps reduce uncertainties in understanding terrestrial carbon dynamics

Atmospheric sciences · Biology · Climate change · Climatology · Geography · Physical geography · Resistance (ecology · Urban climate · Urban heat island · Urbanization · Vegetation (pathology · Climate variability and models · Environmental Science · Plant responses to elevated CO2 · Urban Heat Island Mitigation · Ecology · Geology

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Obras citantes distintas1
Citações por ano1
Intervalo de citações2025 - 2025 (1)
Velocidade de citaçãorecent
Altamente citadoNão
Tipos de citaçãoNeutras: 1
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