气候变化领域集成服务门户(CCPortal): Sensitivity of Ozone Dry Deposition to Ecosystem-Atmosphere Interactions: A Critical Appraisal of Observations and Simulations

CCPortal

DOI	10.1029/2018GB006157
	Sensitivity of Ozone Dry Deposition to Ecosystem-Atmosphere Interactions: A Critical Appraisal of Observations and Simulations
	Lin M.; Malyshev S.; Shevliakova E.; Paulot F.; Horowitz L.W.; Fares S.; Mikkelsen T.N.; Zhang L.
发表日期	2019
ISSN	0886-6236
EISSN	1944-9224
起始页码	1264
结束页码	1288
卷号	33 期号:10
英文摘要	The response of ozone (O3) dry deposition to ecosystem-atmosphere interactions is poorly understood but is central to determining the potential for extreme pollution events under current and future climate conditions. Using observations and an interactive dry deposition scheme within two dynamic vegetation land models (Geophysical Fluid Dynamics Laboratory LM3.0/LM4.0) driven by observation-based meteorological forcings over 1948–2014, we investigate the factors controlling seasonal and interannual variability (IAV) in O3 deposition velocities (Vd,O3). Stomatal activity in this scheme is determined mechanistically, depending on phenology, soil moisture, vapor pressure deficit, and CO2 concentration. Soil moisture plays a key role in modulating the observed and simulated Vd,O3 seasonal changes over evergreen forests in Mediterranean Europe, South Asia, and the Amazon. Analysis of multiyear observations at forest sites in Europe and North America reveals drought stress to reduce Vd,O3 by ~50%. Both LM3.0 and LM4.0 capture the observed Vd,O3 decreases due to drought; however, IAV is weaker by a factor of 2 in LM3.0 coupled to atmospheric models, particularly in regions with large precipitation biases. IAV in summertime Vd,O3 to forests, driven primarily by the stomatal pathway, is largest (15–35%) in semiarid regions of western Europe, eastern North America, and northeastern China. Monthly mean Vd,O3 for the highest year is 2 to 4 times that of the lowest, with significant implications for surface O3 variability and extreme events. Using Vd,O3 from LM4.0 in an atmospheric chemistry model improves the simulation of surface O3 abundance and spatial variability (reduces mean biases by ~10 ppb) relative to the widely used Wesely scheme. ©2019. American Geophysical Union. All Rights Reserved.
英文关键词	air quality; drought; ecosystem-atmosphere interactions; ozone deposition; stomatal conductance
语种	英语
来源期刊	Global Biogeochemical Cycles
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/129704
作者单位	Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ, United States; NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States; Council for Agricultural Research and Economics, Research Centre for Forestry and Wood, Rome, Italy; Department of Environmental Engineering, Technical University of Denmark, Lyngby, Denmark; Air Quality Research Division, Science and Technology Branch, Environment and Climate Change Canada, Toronto, ON, Canada
推荐引用方式 GB/T 7714	Lin M.,Malyshev S.,Shevliakova E.,et al. Sensitivity of Ozone Dry Deposition to Ecosystem-Atmosphere Interactions: A Critical Appraisal of Observations and Simulations[J],2019,33(10).
APA	Lin M..,Malyshev S..,Shevliakova E..,Paulot F..,Horowitz L.W..,...&Zhang L..(2019).Sensitivity of Ozone Dry Deposition to Ecosystem-Atmosphere Interactions: A Critical Appraisal of Observations and Simulations.Global Biogeochemical Cycles,33(10).
MLA	Lin M.,et al."Sensitivity of Ozone Dry Deposition to Ecosystem-Atmosphere Interactions: A Critical Appraisal of Observations and Simulations".Global Biogeochemical Cycles 33.10(2019).