2019
DOI: 10.3390/atmos10010025
|View full text |Cite
|
Sign up to set email alerts
|

Skill-Testing Chemical Transport Models across Contrasting Atmospheric Mixing States Using Radon-222

Abstract: We propose a new technique to prepare statistically-robust benchmarking data for evaluating chemical transport model meteorology and air quality parameters within the urban boundary layer. The approach employs atmospheric class-typing, using nocturnal radon measurements to assign atmospheric mixing classes, and can be applied temporally (across the diurnal cycle), or spatially (to create angular distributions of pollutants as a top-down constraint on emissions inventories). In this study only a short (<1-mo… Show more

Help me understand this report
View preprint versions

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

2
29
0

Year Published

2019
2019
2023
2023

Publication Types

Select...
9
1

Relationship

3
7

Authors

Journals

citations
Cited by 30 publications
(33 citation statements)
references
References 69 publications
2
29
0
Order By: Relevance
“…The underpredictions are attributed to underestimated CO emissions, inaccurate chemical boundary conditions, and possible overestimated atmospheric mixing in the PBL either during daytime or nighttime. The convective boundary-layer height determined by the lidar backscatter measurements at Westmead is 900 m during daytime on 8 May 2012 [29] and between 500-1700 m during daytime and between 100-250 m at night during the whole SPS2 period [104]. WRF/Chem-ROMS gives good agreement for nocturnal mixing depth but tends to underpredict daytime PBLH at this site.…”
Section: Evaluation Of Column Gas Abundancesmentioning
confidence: 80%
“…The underpredictions are attributed to underestimated CO emissions, inaccurate chemical boundary conditions, and possible overestimated atmospheric mixing in the PBL either during daytime or nighttime. The convective boundary-layer height determined by the lidar backscatter measurements at Westmead is 900 m during daytime on 8 May 2012 [29] and between 500-1700 m during daytime and between 100-250 m at night during the whole SPS2 period [104]. WRF/Chem-ROMS gives good agreement for nocturnal mixing depth but tends to underpredict daytime PBLH at this site.…”
Section: Evaluation Of Column Gas Abundancesmentioning
confidence: 80%
“…The loss decay parameter (λ), is defined as a piece-wise polynomial function based on the rain rate such that pollen has a half-life on the plant of 2 d Fig. 3) and the grass pollen record in Melbourne (red); the full sequence of data is shown as circles, with a locally weighted polynomial regression overlaid (Cleveland, 1979). The EVI data are 16 d composites.…”
Section: Pollen Production-loss Modelmentioning
confidence: 99%
“…The temperate coastal basin geography of Sydney means it is influenced by both synoptic and meso-scale meteorological phenomena [4]. In particular, cold air drainage into the basin during the cooler part of the year and afternoon sea breezes in the warmer months are frequent, persistent meso-scale processes that impact the city's air quality [5,6].…”
Section: Air Quality In Sydneymentioning
confidence: 99%