FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1996138929> ?p ?o ?g. }

• W1996138929 endingPage "10845" @default.
• W1996138929 startingPage "10809" @default.
• W1996138929 abstract "In order to better understand the photochemical and meteorological processes controlling regional scale air quality problems such as ozone formation, we have developed a three‐dimensional Eulerian model and applied this model to a high‐pressure period (July 4 to July 7, 1986) over the eastern United States. Meteorological and physical variables from a three‐dimensional primitive‐equation model are used to drive the transport parameters over a grid with 60×60 km 2 horizontal resolution, and 15 unequally spaced vertical layers extending from the ground to roughly 15 km. The treatment and incorporation of the dynamic model, the transport model, surface deposition, emission of anthropogenic and natural O 3 precursors, the chemical mechanism for 35 individual species, solar radiation and the numerical methods are discussed in detail. Model performance is tested by comparing model predicted O 3 concentrations with observations from the U.S. Environmental Protection Agency ozone‐monitoring network. Although a significant correlation between model and observed O 3 is found, systematic discrepancies also exist and are discussed in relation to the basic model formulation, and variability in the observed O 3 . Additionally, a comparison of time‐averaged NO x and anthropogenic nonmethane hydrocarbon (NMHC) concentrations to relatively long term observations provides a qualitative assessment of the model's ability to simulate certain aspects of these O 3 precursors from the few available observations. The model is used as a diagnostic tool to analyze various aspects of regional scale O 3 formation and the budgets of the primary O 3 precursors. Ozone formation over much of the continental model domain is shown to be NO x . limited. On the other hand, for midday NO x levels greater than about 4 or 5 ppbv, O 3 formation is generally suppressed because of the low NMHC to NO x ratios (1 to 7) that are characteristic of the emissions inventory. Regional‐scale budget analyses show that very Hide NO x or NMHC is transported to the free troposphere for the high‐pressure conditions of this study and in the absence of a significant subgrid‐scale vertical mixing process (i.e., efficient cumulus transport). We calculate a net turnover time of about 1.5 days for continental O 3 below 1800 m with in situ photochemical formation being balanced by photochemical loss and transport off the American continent. The results of this work are intended to serve as a baseline for further model development." @default.
• W1996138929 created "2016-06-24" @default.
• W1996138929 creator A5043824280 @default.
• W1996138929 creator A5046676389 @default.
• W1996138929 creator A5056787173 @default.
• W1996138929 creator A5071159939 @default.
• W1996138929 creator A5074416915 @default.
• W1996138929 date "1991-06-20" @default.
• W1996138929 modified "2023-10-14" @default.
• W1996138929 title "A regional model study of the ozone budget in the eastern United States" @default.
• W1996138929 cites W1500508824 @default.
• W1996138929 cites W1592514828 @default.
• W1996138929 cites W1623924183 @default.
• W1996138929 cites W1964375160 @default.
• W1996138929 cites W1964915634 @default.
• W1996138929 cites W1965736430 @default.
• W1996138929 cites W1973108140 @default.
• W1996138929 cites W1974529166 @default.
• W1996138929 cites W1975585929 @default.
• W1996138929 cites W1976391619 @default.
• W1996138929 cites W1977611960 @default.
• W1996138929 cites W1978153810 @default.
• W1996138929 cites W1978855535 @default.
• W1996138929 cites W1978873159 @default.
• W1996138929 cites W1978961072 @default.
• W1996138929 cites W1979058380 @default.
• W1996138929 cites W1981367411 @default.
• W1996138929 cites W1990877036 @default.
• W1996138929 cites W1991852877 @default.
• W1996138929 cites W1993773161 @default.
• W1996138929 cites W1994029151 @default.
• W1996138929 cites W1994274844 @default.
• W1996138929 cites W1994628644 @default.
• W1996138929 cites W1996563514 @default.
• W1996138929 cites W1996931441 @default.
• W1996138929 cites W1997956060 @default.
• W1996138929 cites W1998350080 @default.
• W1996138929 cites W2001838540 @default.
• W1996138929 cites W2002801763 @default.
• W1996138929 cites W2004327715 @default.
• W1996138929 cites W2004771924 @default.
• W1996138929 cites W2005887670 @default.
• W1996138929 cites W2006412860 @default.
• W1996138929 cites W2007403062 @default.
• W1996138929 cites W2008558786 @default.
• W1996138929 cites W2009470133 @default.
• W1996138929 cites W2010192261 @default.
• W1996138929 cites W2014298861 @default.
• W1996138929 cites W2016737365 @default.
• W1996138929 cites W2018337903 @default.
• W1996138929 cites W2020147105 @default.
• W1996138929 cites W2024765523 @default.
• W1996138929 cites W2024999252 @default.
• W1996138929 cites W2025171076 @default.
• W1996138929 cites W2026123903 @default.
• W1996138929 cites W2027349663 @default.
• W1996138929 cites W2031980749 @default.
• W1996138929 cites W2034862870 @default.
• W1996138929 cites W2041499204 @default.
• W1996138929 cites W2047451389 @default.
• W1996138929 cites W2047734533 @default.
• W1996138929 cites W2057899290 @default.
• W1996138929 cites W2058464886 @default.
• W1996138929 cites W2059006576 @default.
• W1996138929 cites W2059205508 @default.
• W1996138929 cites W2063981797 @default.
• W1996138929 cites W2067184883 @default.
• W1996138929 cites W2067418767 @default.
• W1996138929 cites W2071848641 @default.
• W1996138929 cites W2072270610 @default.
• W1996138929 cites W2076526537 @default.
• W1996138929 cites W2076702827 @default.
• W1996138929 cites W2078357352 @default.
• W1996138929 cites W2079591728 @default.
• W1996138929 cites W2081518068 @default.
• W1996138929 cites W2081917368 @default.
• W1996138929 cites W2082262515 @default.
• W1996138929 cites W2083604125 @default.
• W1996138929 cites W2084765781 @default.
• W1996138929 cites W2087489447 @default.
• W1996138929 cites W2093634354 @default.
• W1996138929 cites W2095059645 @default.
• W1996138929 cites W2117270435 @default.
• W1996138929 cites W2118350199 @default.
• W1996138929 cites W2120477378 @default.
• W1996138929 cites W2124827694 @default.
• W1996138929 cites W2127703393 @default.
• W1996138929 cites W2137741627 @default.
• W1996138929 cites W2143468207 @default.
• W1996138929 cites W2147677219 @default.
• W1996138929 cites W2151457357 @default.
• W1996138929 cites W2153162078 @default.
• W1996138929 cites W2156219496 @default.
• W1996138929 cites W2156380621 @default.
• W1996138929 cites W2157424290 @default.
• W1996138929 cites W2158184352 @default.
• W1996138929 cites W2164050692 @default.
• W1996138929 cites W2166537477 @default.

• next