Matches in SemOpenAlex for { <https://semopenalex.org/work/W4236049891> ?p ?o ?g. }
- W4236049891 abstract "Abstract. Ten different approaches for applying lateral and top climatological boundary conditions for ozone have been evaluated using the off-line regional air-quality model AURAMS. All ten approaches employ the same climatological ozone profiles, but differ in the manner in which they are applied, via the inclusion or exclusion of (i) a dynamic adjustment of the climatological ozone profile in response to the model-predicted tropopause height, (ii) a sponge zone for ozone on the model top, (iii) upward extrapolation of the climatological ozone profile, and (iv) different mass consistency corrections. The model performance for each approach was evaluated against North American surface ozone and ozonesonde observations from the BAQS-Met field study period in the summer of 2007. The original daily one-hour maximum surface ozone biases of about +15 ppbv were greatly reduced (halved) in some simulations using alternative methodologies. However, comparisons to ozonesonde observations showed that the reduction in surface ozone bias sometimes came at the cost of significant positive biases in ozone concentrations in the free troposphere and upper troposphere. The best overall performance throughout the troposphere was achieved using a methodology that included dynamic tropopause height adjustment, no sponge zone at the model top, extrapolation of ozone when required above the limit of the climatology, and no mass consistency corrections (global mass conservation was still enforced). The simulation using this model version had a one-hour daily maximum surface ozone bias of +8.6 ppbv, with small reductions in model correlation, and the best comparison to ozonesonde profiles. This recommended and original methodologies were compared for two further case studies: a high-resolution simulation of the BAQS-Met measurement intensive, and a study of the downwind region of the Canadian Rockies. Significant improvements were noted for the high resolution simulations during the BAQS-Met measurement intensive period, both in formal statistical comparisons and time series comparisons of events at surface stations. The tests for the downwind-Rockies region showed that the coupling between vertical transport associated with troposphere/stratosphere exchange, and that associated with boundary layer turbulent mixing, may contribute to ozone positive biases." @default.
- W4236049891 created "2022-05-12" @default.
- W4236049891 creator A5002510778 @default.
- W4236049891 creator A5023595627 @default.
- W4236049891 creator A5038479277 @default.
- W4236049891 creator A5041835402 @default.
- W4236049891 creator A5048516418 @default.
- W4236049891 creator A5063819107 @default.
- W4236049891 creator A5065750553 @default.
- W4236049891 creator A5067499882 @default.
- W4236049891 creator A5073429517 @default.
- W4236049891 creator A5081753548 @default.
- W4236049891 creator A5087210606 @default.
- W4236049891 date "2010-06-01" @default.
- W4236049891 modified "2023-10-17" @default.
- W4236049891 title "Dynamic Adjustment of Climatological Ozone Boundary Conditions for Air-Quality Forecasts" @default.
- W4236049891 cites W1506955444 @default.
- W4236049891 cites W1964250365 @default.
- W4236049891 cites W1965736430 @default.
- W4236049891 cites W1971171207 @default.
- W4236049891 cites W1978474657 @default.
- W4236049891 cites W1980865383 @default.
- W4236049891 cites W1985550815 @default.
- W4236049891 cites W1986127040 @default.
- W4236049891 cites W1987849640 @default.
- W4236049891 cites W1989825589 @default.
- W4236049891 cites W1993076417 @default.
- W4236049891 cites W2002185921 @default.
- W4236049891 cites W2023223991 @default.
- W4236049891 cites W2027292790 @default.
- W4236049891 cites W2041860261 @default.
- W4236049891 cites W2045080642 @default.
- W4236049891 cites W2052372798 @default.
- W4236049891 cites W2053881040 @default.
- W4236049891 cites W2061589304 @default.
- W4236049891 cites W2065321126 @default.
- W4236049891 cites W2066072680 @default.
- W4236049891 cites W2071272121 @default.
- W4236049891 cites W2071783577 @default.
- W4236049891 cites W2077946087 @default.
- W4236049891 cites W2079261398 @default.
- W4236049891 cites W2106595238 @default.
- W4236049891 cites W2122607663 @default.
- W4236049891 cites W2409576224 @default.
- W4236049891 cites W3081975057 @default.
- W4236049891 doi "https://doi.org/10.5194/acpd-10-13643-2010" @default.
- W4236049891 hasPublicationYear "2010" @default.
- W4236049891 type Work @default.
- W4236049891 citedByCount "4" @default.
- W4236049891 countsByYear W42360498912016 @default.
- W4236049891 crossrefType "posted-content" @default.
- W4236049891 hasAuthorship W4236049891A5002510778 @default.
- W4236049891 hasAuthorship W4236049891A5023595627 @default.
- W4236049891 hasAuthorship W4236049891A5038479277 @default.
- W4236049891 hasAuthorship W4236049891A5041835402 @default.
- W4236049891 hasAuthorship W4236049891A5048516418 @default.
- W4236049891 hasAuthorship W4236049891A5063819107 @default.
- W4236049891 hasAuthorship W4236049891A5065750553 @default.
- W4236049891 hasAuthorship W4236049891A5067499882 @default.
- W4236049891 hasAuthorship W4236049891A5073429517 @default.
- W4236049891 hasAuthorship W4236049891A5081753548 @default.
- W4236049891 hasAuthorship W4236049891A5087210606 @default.
- W4236049891 hasBestOaLocation W42360498911 @default.
- W4236049891 hasConcept C105795698 @default.
- W4236049891 hasConcept C126314574 @default.
- W4236049891 hasConcept C127313418 @default.
- W4236049891 hasConcept C132459708 @default.
- W4236049891 hasConcept C153294291 @default.
- W4236049891 hasConcept C171420983 @default.
- W4236049891 hasConcept C205649164 @default.
- W4236049891 hasConcept C2776349674 @default.
- W4236049891 hasConcept C33923547 @default.
- W4236049891 hasConcept C39432304 @default.
- W4236049891 hasConcept C49204034 @default.
- W4236049891 hasConcept C508106653 @default.
- W4236049891 hasConcept C9075549 @default.
- W4236049891 hasConcept C91586092 @default.
- W4236049891 hasConceptScore W4236049891C105795698 @default.
- W4236049891 hasConceptScore W4236049891C126314574 @default.
- W4236049891 hasConceptScore W4236049891C127313418 @default.
- W4236049891 hasConceptScore W4236049891C132459708 @default.
- W4236049891 hasConceptScore W4236049891C153294291 @default.
- W4236049891 hasConceptScore W4236049891C171420983 @default.
- W4236049891 hasConceptScore W4236049891C205649164 @default.
- W4236049891 hasConceptScore W4236049891C2776349674 @default.
- W4236049891 hasConceptScore W4236049891C33923547 @default.
- W4236049891 hasConceptScore W4236049891C39432304 @default.
- W4236049891 hasConceptScore W4236049891C49204034 @default.
- W4236049891 hasConceptScore W4236049891C508106653 @default.
- W4236049891 hasConceptScore W4236049891C9075549 @default.
- W4236049891 hasConceptScore W4236049891C91586092 @default.
- W4236049891 hasLocation W42360498911 @default.
- W4236049891 hasLocation W42360498912 @default.
- W4236049891 hasOpenAccess W4236049891 @default.
- W4236049891 hasPrimaryLocation W42360498911 @default.
- W4236049891 hasRelatedWork W12744974 @default.
- W4236049891 hasRelatedWork W16993394 @default.
- W4236049891 hasRelatedWork W23468020 @default.
- W4236049891 hasRelatedWork W23608737 @default.
- W4236049891 hasRelatedWork W32802341 @default.