2015
DOI: 10.1016/j.jes.2014.12.022
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Ozone concentrations, flux and potential effect on yield during wheat growth in the Northwest-Shandong Plain of China

Abstract: exposure-response functions obtained from the USA, Europe, and China, the O 3 -induced wheat yield reduction in the district was estimated as 12.9% on average (5.5%-23.3%). Large uncertainties were related to the statistical methods and environmental conditions involved in deriving the exposure-response functions.

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Cited by 36 publications
(7 citation statements)
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References 52 publications
(93 reference statements)
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“…We further find a similar midday magnitude as Stella et al (2011a) found in April with wetter soils. Night-time ozone deposition velocity did not go lower than around 0.2 cm s −1 in our study, as also found by Zhu et al (2015) over a growing wheat in China, Stella et al (2011a) over bare soil in summer, and Lamaud et al (2009) over maize. These authors as well as Huang et al (2016) clearly show that this is due to non-stomatal deposition being primarily driven by u * which does not reach zero at night during these periods.…”
Section: Seasonal Dynamics Of No No 2 and O 3 Fluxessupporting
confidence: 88%
“…We further find a similar midday magnitude as Stella et al (2011a) found in April with wetter soils. Night-time ozone deposition velocity did not go lower than around 0.2 cm s −1 in our study, as also found by Zhu et al (2015) over a growing wheat in China, Stella et al (2011a) over bare soil in summer, and Lamaud et al (2009) over maize. These authors as well as Huang et al (2016) clearly show that this is due to non-stomatal deposition being primarily driven by u * which does not reach zero at night during these periods.…”
Section: Seasonal Dynamics Of No No 2 and O 3 Fluxessupporting
confidence: 88%
“…We further find a similar midday magnitude as Stella et al (2011) found in April with wetter soils. Night-time ozone deposition velocity does not go lower than around 0.2 cm s -1 in our study, as also found by Zhu et al (2015) over a growing wheat in China, Stella et al (2011) over bare soil in summer, and Lamaud et al (2009) over maize. These authors as well as Huang et al (2016) clearly show that this is due to non-stomatal deposition being primarily driven by u * which does not reach zero at night during these periods.…”
Section: S6 Seasonal Pattern Of O 3 Deposition Velocity and No Fluxessupporting
confidence: 87%
“…Specifically, the M7 indicator shows an average exposure of 7 h (from 9:00 a.m. to 3:59 p.m.) and the AOT40 index indicates the concentration of O 3 accumulated during daytime hours over a threshold of 40 ppbV [ 41 ]. AOT40 is an accumulated O 3 -exposure metric currently used as a standard in many regions worldwide to estimate the effects of ground-level O 3 pollution on crops, such as in China [ 18 , 69 , 70 ], India [ 15 , 71 ], Europe [ 72 , 73 ], and the United States [ 74 , 75 ]. Furthermore, the AOT40 index is strongly correlated with the relative yields of different crops [ [76] , [77] , [78] ].…”
Section: Methodsmentioning
confidence: 99%