2011
DOI: 10.1016/j.atmosenv.2011.07.038
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Nocturnal ozone enhancement in the lower troposphere observed by lidar

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Cited by 34 publications
(19 citation statements)
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“…GEOS-5 meteorological data indicates that a weak low level jet (LLJ) may have been occurring as the westerly wind component (U wind) below 2 km increased from <5 m·s −1 at 00 UTC (07pm CDT) to >10 m·s −1 at 09 UTC (04am CDT). LLJs occur frequently in the southeast US and can transport O3 and precursor species from urban regions to rural areas in the late afternoon and night-time hours resulting in nocturnal O3 enhancements (e.g., [17]). Long-range/stratospheric sources contributed O3 mixing ratios near the surface which were similar to monthly-averaged values (~20 nmol mol −1 ).…”
Section: June 2013mentioning
confidence: 99%
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“…GEOS-5 meteorological data indicates that a weak low level jet (LLJ) may have been occurring as the westerly wind component (U wind) below 2 km increased from <5 m·s −1 at 00 UTC (07pm CDT) to >10 m·s −1 at 09 UTC (04am CDT). LLJs occur frequently in the southeast US and can transport O3 and precursor species from urban regions to rural areas in the late afternoon and night-time hours resulting in nocturnal O3 enhancements (e.g., [17]). Long-range/stratospheric sources contributed O3 mixing ratios near the surface which were similar to monthly-averaged values (~20 nmol mol −1 ).…”
Section: June 2013mentioning
confidence: 99%
“…The accuracy of the system has been discussed in previous studies and Lidar measurement precision is estimated to be ±10% in the lower troposphere and ±20% in the upper troposphere [15,16]. Data from the UAH TOLNet lidar system is publically available [14] and has been used to examine atmospheric chemistry relevant topics such as air pollution transport, nocturnal O 3 enhancements, stratosphere-troposphere exchange, boundary layer pollution entrainment, wildfire impacts on O 3 , and lightning NO x generated O 3 (e.g., [17][18][19]). During this study we evaluated all UAH TOLNet observations for the month of June 2013 to identify anomalous O 3 lamina (see Section 3.1).…”
Section: Tolnet Ozone Lidar Measurementsmentioning
confidence: 99%
“…The lidar receiver configuration is similar to that reported by Kuang et al [12] except for the addition of a 2.5 cm mini-receiver and a beamsplitter in the 10 cm receiver. In 2008, a 10%-90% beamsplitter was integrated into the 10 cm receiver and extended the observations down to ∼500 m AGL using the 10% channel [20,21]. Modifying a design used in a previous National Aeronautics and Space Administration (NASA) airborne lidar campaign [22], a 2.5 cm diameter receiver was recently added to lower the lidar's minimum observable altitude.…”
Section: B Lidar Receivermentioning
confidence: 99%
“…High resolution and continuous observational capability make lidars ideal instruments to capture rapid variations in ozone distribution (Kuang et al, 2011a(Kuang et al, , 2012. This paper evaluates the tropospheric ozone variability associated with lightning events as measured by the Rocket-city O 3 Quality Evaluation in the Troposphere (RO 3 QET) lidar in Huntsville, AL, and simulated by the Weather Research and Forecasting (WRF) model coupled with Chemistry (WRF/Chem).…”
Section: Introductionmentioning
confidence: 99%