2003
DOI: 10.1016/s1352-2310(03)00383-2
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Analysis of transport patterns during an SCOS97-NARSTO episode

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Cited by 32 publications
(20 citation statements)
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“…The interaction between UHI circulation and the background flow has been examined in several studies [9,41,42]. For an urban area, there is generally a certain wind-speed threshold that determines the relative dominance and impacts of background versus UHI-induced flows.…”
Section: Uhi/uhii Reference Pointsmentioning
confidence: 99%
“…The interaction between UHI circulation and the background flow has been examined in several studies [9,41,42]. For an urban area, there is generally a certain wind-speed threshold that determines the relative dominance and impacts of background versus UHI-induced flows.…”
Section: Uhi/uhii Reference Pointsmentioning
confidence: 99%
“…This pressure gradient is controlled by the semi-permanent Pacific high, situated offshore central California, which diverts storms far to the north during summer. This pressure feature drives prevailing west-southwesterly winds at the regional scale in the California south coast air basins (Boucouvala and Bornstein, 2003).…”
Section: The Southern San Joaquin Valley Californiamentioning
confidence: 94%
“…In particular, subtropical high-pressure systems are known to coincide with episodes of ground-level O 3 pollution. 14,16,18,[25][26][27][28][29][30][31][32][33][34] High-pressure systems are synonymous with large-scale subsidence through the troposphere, coinciding with stagnant conditions at Earth's surface. High concentrations of O 3 have been associated with highpressure systems and attendant subsidence, particularly when the anti-cyclonic circulation surrounding the center of high pressure is weak, leading to calm winds, sunny skies, and warm temperatures at ground level.…”
Section: Background O 3 and Meteorologymentioning
confidence: 99%
“…27 Similar high-pressure regimes contribute to an O 3 increase on the Pacific Coast of the United States, where the Pacific High tends to dominate. 31 The presence of the Pacific High, a broad, anticyclonic circulation, promotes stagnation within the boundary layer in the Los Angeles metropolitan area. 31 The Pacific High is marked by strong subsidence through the troposphere.…”
Section: Background O 3 and Meteorologymentioning
confidence: 99%
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