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Measurements of Ozone Precursors in the Lake Tahoe Basin, USA

机译:美国太浩湖盆地中臭氧前体的测量

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The results of this and the previous study indicate that the majority of O_3 precursors (VOC and NOx) are emitted in the urbanized areas of the Central Valley and possibly the San Francisco Bay Area. The concentrations of ozone precursors, VOC and NOx at all four sites are very low, therefore, substantial in-situ photochemical production of ozone is unlikely at most sites. The only site which showed slightly higher NOx and VOC concentrations is TRPA, which is located in South Lake Tahoe near the Kingsbury Grade Highway. South Lake Tahoe is the biggest city in the Tahoe Basin and experiences higher local traffic. Thus photochemical production of ozone may be non-negligible in this area. The Tahoe sites display great site-to-site variability in O_3 concentrations during the evening and pre-dawn hours of 1900 to 0700 PST, but consistent maxima of 50 to 60 ppb from 1000 to 1700 PST. The observation that all of the Tahoe sites tend to rapidly reach the same middle day maximum between the hours of 0600 and 1000 PST suggests that this rise in surface ozone is due primarily to the vigorous vertical mixing that occurs in the hours immediately after sunrise, when ozone-depleted air near the surface is warmed by solar heating of the surface, while cooler, ozone-rich air from aloft is simultaneously mixed downwards. These well-mixed conditions persist throughout the Tahoe Basin until approximately 1700 PST, when there is marked decrease in solar insolation. During the evening hours, those sites that have good exposure to ozone-rich air from aloft, which is being transported in via regional-scale and long-range transport, continue to exhibit high ozone concentrations. Sites that are more conducive to the formation of nocturnal temperature inversions see a decrease in surface level ozone, primarily via dry deposition. These observations likely indicate that much of the ozone measured at Lake Tahoe sites results from the transport of polluted background air into the Basin from upwind pollution source regions (e.g., Sacramento, San Joaquin Valley and San Francisco Bay Area).
机译:该研究和先前的研究结果表明,大多数O_3前体(VOC和NOx)排放到中央山谷的城市化地区,也可能是旧金山湾地区。在所有四个站点中,臭氧前体,VOC和NOx的浓度都非常低,因此,在大多数站点中不太可能发生大量的原位臭氧光化学生产。 TRPA唯一显示出较高NOx和VOC浓度的站点是TRPA,它位于金斯伯里等级高速公路附近的南太浩湖。南太浩湖是塔霍盆地最大的城市,当地人流量较高。因此,臭氧的光化学产生在这一领域可能是不可忽略的。 Tahoe站点在1900至0700 PST的傍晚和黎明前时段,O_3浓度的站点间差异很大,但从1000到1700 PST的最大值为50到60 ppb。所有Tahoe地点趋向于在0600和1000 PST的小时之间迅速达到同一中间天最大值的观察结果表明,表面臭氧的这种上升主要是由于日出后紧接几个小时内发生的剧烈垂直混合所致。地表附近的消耗臭氧的空气通过地表的太阳能加热而变暖,而来自高空的较冷的,富含臭氧的空气同时向下混合。这些充分混合的条件一直持续到整个塔霍盆地,直到大约1700 PST,此时日照量明显下降。在傍晚时分,那些通过区域规模和远距离运输而被运输的高空暴露于高空臭氧的空气中的地点仍表现出较高的臭氧浓度。更有利于夜间温度反转形成的地点,主要是通过干沉降,减少了表面臭氧水平。这些观察结果可能表明,在太浩湖站点测得的大部分臭氧是由上风污染源区域(例如,萨克拉曼多,圣华金河谷和旧金山湾区)向本盆地输送的被污染背景空气造成的。

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