1999
DOI: 10.1016/s1352-2310(97)00328-2
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Synoptic conditions associated with high carbon monoxide episodes at a coastal station in Hong Kong

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Cited by 24 publications
(19 citation statements)
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“…Generally, when the northerly monsoons were enhanced, the CO levels were dramatically increased at both sites (for example, 30 October-1 November and 18-19 November). Chung et al (1999) investigated the relationship between high CO episodes and synoptic conditions at a coastal station in Hong Kong and found similar features as well. In contrast to CO, the O 3 levels had a decreasing trend with enhanced northerly monsoons at both sites (for example, 30 October-1 …”
Section: Day-to-day Variationsmentioning
confidence: 81%
“…Generally, when the northerly monsoons were enhanced, the CO levels were dramatically increased at both sites (for example, 30 October-1 November and 18-19 November). Chung et al (1999) investigated the relationship between high CO episodes and synoptic conditions at a coastal station in Hong Kong and found similar features as well. In contrast to CO, the O 3 levels had a decreasing trend with enhanced northerly monsoons at both sites (for example, 30 October-1 …”
Section: Day-to-day Variationsmentioning
confidence: 81%
“…Similar meteorological conditions are also responsible for the majority of CO episodes in Hong Kong. 4 Clusters 1W and 4W are associated with cyclonic circulation, cloudiness, and low minimum temperature. These conditions are responsible for enhanced needs of central heating as well as for the "cold start" of vehicles that leads to CO production.…”
Section: Cold Periodmentioning
confidence: 99%
“…[1][2][3][4][5] All these works mainly concentrate on air pollution episodic events, especially for O 3 and other gaseous pollutants. Chung et al 4 found IMPLICATIONS This study correlates objectively defined synoptic circulation types with air pollution levels in Athens. These synoptic types are correlated with pollutant concentrations in objectively defined zones that present homogeneous air quality characteristics.…”
Section: Introductionmentioning
confidence: 99%
“…Uplifted CO usually has a longer lifetime and can be transported fast by the upper layer winds over long distances through continents and between hemispheres in the troposphere (Stohl, 2001;Stohl et al, 2002;Damoah et al, 2004). Uplifting air mass from the surface to FT generally takes place by three processes: (1) frontal lifting, (2) orographic lifting, and (3) deep convection (Brown et al, 1984;Banic et al, 1986;Dickerson et al, 1987;Bethan et al, 1998;Pickering et al, 1998;Chung et al, 1999;Donnell et al, 2001;Kowol-Santen et al, 2001;Cooper et al, 2002;Liu et al, 2003;Miyazaki et al, 2003;Chan et al;Mari et al, 2004;Liu et al, 2006;Kar et al, 2008;Zhao et al, 2008;Ding et al, 2009;Randel et al, 2010;Chen et al, 2012).…”
Section: Introductionmentioning
confidence: 99%