| Title: | Measurement-based investigation of ozone deposition to vegetation under the effects of coastal and photochemical air pollution in the Eastern Mediterranean |
| Author(s): | Li Q; Gabay M; Rubin Y; Fredj E; Tas E; |
| Address: | "The Robert H. Smith Faculty of Agriculture, Food & Environment, Department of Soil and Water Sciences, The Hebrew University of Jerusalem, Rehovot, Israel. Department of Computer Science, Jerusalem College of Technology, Jerusalem, Israel. Electronic address: fredj@jct.ac.il. The Robert H. Smith Faculty of Agriculture, Food & Environment, Department of Soil and Water Sciences, The Hebrew University of Jerusalem, Rehovot, Israel. Electronic address: eran.tas@mail.huji.ac.il" |
| DOI: | 10.1016/j.scitotenv.2018.07.037 |
| ISSN/ISBN: | 1879-1026 (Electronic) 0048-9697 (Linking) |
| Abstract: | "Dry deposition of ozone (O(3)) to vegetation is an important pathway for its removal from the troposphere, and it can lead to adverse effects in plants and changes in climate. However, our mechanistic understanding of O(3) dry deposition is insufficient to adequately account for it in global and regional models, primarily because this process is highly complicated by feedback mechanisms and sensitivity to specific characteristics of vegetative environment and atmospheric dynamics and composition. We hypothesized that measuring dry deposition of O(3) to vegetation near the Eastern Mediterranean (EM) coast, where large variations in meteorological conditions and photochemical air pollution frequently occur, would enable identifying the mechanisms controlling O(3) deposition to vegetation. Moreover, we have only limited knowledge of O(3) deposition to vegetation occurring near a coastline, under air pollution, or in the EM. This study investigated O(3) deposition to mixed Mediterranean vegetation between the summers of 2015 and 2017, 3.6?ª+km away from the EM coast, using the eddy covariance technique to quantify vertical flux of O(3) and its partitioning to stomatal and non-stomatal flux, concurrent with nitrogen oxide (NO(x)), sulfur dioxide and carbon monoxide. Surprisingly, nighttime O(3)-deposition velocity (V(d)) was smaller than daytime V(d) by only ~20-37% on average for all measurement periods, primarily related to moderate nighttime atmospheric stability due to proximity to the seashore. We provide evidence for the role of sea-salt aerosols in enhancing O(3) deposition via surface-wetness buildup at low relative humidity near the coast, and for daytime enhancement of O(3) deposition by the combined effects of biogenic volatile organic compound emission and surface-wetness buildup. We further show that NO(x) emitted from elevated emission sources can reduce O(3) deposition, and even lead to a positive O(3) flux, demonstrating the importance of adequately taking into account the impact of air pollution on O(3) deposition to vegetation" |
| Keywords: | Air Pollutants/*analysis Air Pollution/statistics & numerical data Climate *Environmental Monitoring Ozone/*analysis Sulfur Dioxide Bvoc Eddy covariance Flux NO(x) Sea-salt aerosol Sea-land breeze; |
| Notes: | "MedlineLi, Qian Gabay, Maor Rubin, Yoav Fredj, Erick Tas, Eran eng Netherlands 2018/09/27 Sci Total Environ. 2018 Dec 15; 645:1579-1597. doi: 10.1016/j.scitotenv.2018.07.037. Epub 2018 Jul 25" |
