Open AccessEnhanced drought resistance of vegetation growth in cities due to urban heat, CO2 domes and O3 troughs
Author(s) -
Ping Fu,
Leiqiu Hu,
Elizabeth A. Ainsworth,
Xiaonan Tai,
Soe W. Myint,
Wenfeng Zhan,
B. Blakely,
Carl J. Bernacchi
Publication year - 2021
Publication title -
environmental research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.37
H-Index - 124
ISSN - 1748-9326
DOI - 10.1088/1748-9326/ac3b17
Subject(s) - vegetation (pathology) , environmental science , climate change , physical geography , urban climate , resistance (ecology) , atmospheric sciences , urban heat island , urbanization , ecology , climatology , geography , geology , biology , medicine , pathology
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.