2014
DOI: 10.1080/07055900.2014.910164
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Low Ozone Episodes at Amphitrite Point Marine Boundary Layer Observatory, British Columbia, Canada

Abstract: At Amphitrite Point, ozone (O 3) mixing ratios are observed to drop steadily to 5-15 ppb over a period of 12 hours or less with a frequency approaching one event per week (with highest frequencies occurring in summer and fall). Analysis of 47 such O 3 depletion events reveals that low O 3 episodes are a predominantly nocturnal phenomenon associated with anticyclonic conditions characterized by light onshore or alongshore winds and an absence of fog and mist. Back-trajectories show air carried to the Amphitrite… Show more

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Cited by 12 publications
(14 citation statements)
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References 29 publications
(37 reference statements)
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“…The main mode of winter and fall, and the second mode of summer monsoon season displayed similar concentrations, which comprised the primary mode of O 3 distributions observed at IORS. O 3 levels are known to exhibit lower variability at remote sites and rural areas (McKendry et al, 2014;Oltmans and Levy II, 1994). However, the results of this study challenge those of previous studies.…”
Section: Ozone Variationscontrasting
confidence: 57%
“…The main mode of winter and fall, and the second mode of summer monsoon season displayed similar concentrations, which comprised the primary mode of O 3 distributions observed at IORS. O 3 levels are known to exhibit lower variability at remote sites and rural areas (McKendry et al, 2014;Oltmans and Levy II, 1994). However, the results of this study challenge those of previous studies.…”
Section: Ozone Variationscontrasting
confidence: 57%
“…The back trajectories showed that ODEs were characterized by light onshore or alongshore winds and that the air masses generally originated in the MBL, i.e., had a marine origin. Overall, the evidence indicated that the ODEs at APO are caused by a non-photochemical coastal zone process that extends over a spatial scale of tens of kilometres (McKendry et al, 2014).…”
Section: Introductionmentioning
confidence: 93%
“…At a freezing temperature of −20 • C and for a diameter of 0.1 µm, approximately 1 in 10 5 particles acted as an INP, while for a diameter of 10 µm, approximately 1 in 100 particles acted as an INP. A study of residuals of mixed-phase clouds by Mertes et al (2007) found that 1 in 10 supermicron particles acted as an INP, while only 1 in 10 3 submicron particles acted as an INP. Huffman et al (2013) studied INPs collected at a semi-arid pine forest in Colorado, USA.…”
Section: Ice-nucleating Ability On a Per Number Basismentioning
confidence: 99%