FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4238455331> ?p ?o ?g. }

• W4238455331 abstract "Abstract. We quantify the sources contributing to background surface ozone concentrations in the US Intermountain West by using the GEOS-Chem chemical transport model with 1/2° × 2/3° horizontal resolution to interpret CASTNet ozone monitoring data for 2006–2008. We isolate contributions from lightning, wildfires, the stratosphere, and California pollution. Lightning increases mean surface ozone in summer by 10 ppbv in the Intermountain West, with moderate variability; constraining the model source with flash rate observations is important. Using a daily wildfire inventory compiled from fire reports in the western US generates high-ozone events in excess of 80 ppbv in GEOS-Chem. The CASTNet observations show no evidence of such events. Models in general may overestimate ozone concentrations in fresh plumes because of inadequate fire plume chemistry. The highest ozone concentrations observed in the Intermountain West (>75 ppbv) in spring are associated with stratospheric intrusions. The model captures the timing of these intrusions but not their magnitude, reflecting numerical diffusion intrinsic to Eulerian models. This can be corrected statistically through a relationship between model bias and the model-diagnosed magnitude of stratospheric influence; with this correction, models may still be useful to forecast and interpret high-ozone events from stratospheric intrusions. We show that discrepancy between models in diagnosing stratospheric influence is due in part to differences in definition, i.e., whether stratospheric ozone is diagnosed as produced in the stratosphere (GEOS-Chem definition) or as transported from above the tropopause. The latter definition can double the diagnosed stratospheric influence in surface air by labeling as stratospheric any ozone produced in the troposphere and temporarily transported to the stratosphere. California pollution influence in the Intermountain West frequently exceeds 10 ppbv but is generally not correlated with the highest ozone events." @default.
• W4238455331 created "2022-05-12" @default.
• W4238455331 creator A5002048745 @default.
• W4238455331 creator A5004391411 @default.
• W4238455331 creator A5013271600 @default.
• W4238455331 creator A5014475118 @default.
• W4238455331 creator A5017874207 @default.
• W4238455331 creator A5076412395 @default.
• W4238455331 date "2013-10-08" @default.
• W4238455331 modified "2023-10-15" @default.
• W4238455331 title "Sources contributing to background surface ozone in the US Intermountain West" @default.
• W4238455331 cites W1627199030 @default.
• W4238455331 cites W1660571612 @default.
• W4238455331 cites W1835320847 @default.
• W4238455331 cites W1862105058 @default.
• W4238455331 cites W1903012642 @default.
• W4238455331 cites W1966195308 @default.
• W4238455331 cites W1971279984 @default.
• W4238455331 cites W1972358138 @default.
• W4238455331 cites W1978186098 @default.
• W4238455331 cites W1984910766 @default.
• W4238455331 cites W1995408610 @default.
• W4238455331 cites W1998652360 @default.
• W4238455331 cites W2014931100 @default.
• W4238455331 cites W2016055872 @default.
• W4238455331 cites W2018604209 @default.
• W4238455331 cites W2019708954 @default.
• W4238455331 cites W2024421777 @default.
• W4238455331 cites W2028245216 @default.
• W4238455331 cites W2030195284 @default.
• W4238455331 cites W2031601832 @default.
• W4238455331 cites W2033170862 @default.
• W4238455331 cites W2045083972 @default.
• W4238455331 cites W2052164035 @default.
• W4238455331 cites W2057103665 @default.
• W4238455331 cites W2061755621 @default.
• W4238455331 cites W2066595000 @default.
• W4238455331 cites W2090138698 @default.
• W4238455331 cites W2092159787 @default.
• W4238455331 cites W2095479710 @default.
• W4238455331 cites W2095981332 @default.
• W4238455331 cites W2097202844 @default.
• W4238455331 cites W2100121820 @default.
• W4238455331 cites W2101462621 @default.
• W4238455331 cites W2105791725 @default.
• W4238455331 cites W2119834746 @default.
• W4238455331 cites W2128738304 @default.
• W4238455331 cites W2129706680 @default.
• W4238455331 cites W2130995416 @default.
• W4238455331 cites W2134927874 @default.
• W4238455331 cites W2144304061 @default.
• W4238455331 cites W2157265468 @default.
• W4238455331 cites W2157422123 @default.
• W4238455331 cites W2157591818 @default.
• W4238455331 cites W2159639772 @default.
• W4238455331 cites W2165708514 @default.
• W4238455331 cites W2165977355 @default.
• W4238455331 cites W2166593303 @default.
• W4238455331 cites W2167475648 @default.
• W4238455331 cites W2169477247 @default.
• W4238455331 cites W2171688174 @default.
• W4238455331 cites W2321556814 @default.
• W4238455331 cites W2329080388 @default.
• W4238455331 cites W4297845603 @default.
• W4238455331 doi "https://doi.org/10.5194/acpd-13-25871-2013" @default.
• W4238455331 hasPublicationYear "2013" @default.
• W4238455331 type Work @default.
• W4238455331 citedByCount "0" @default.
• W4238455331 crossrefType "posted-content" @default.
• W4238455331 hasAuthorship W4238455331A5002048745 @default.
• W4238455331 hasAuthorship W4238455331A5004391411 @default.
• W4238455331 hasAuthorship W4238455331A5013271600 @default.
• W4238455331 hasAuthorship W4238455331A5014475118 @default.
• W4238455331 hasAuthorship W4238455331A5017874207 @default.
• W4238455331 hasAuthorship W4238455331A5076412395 @default.
• W4238455331 hasBestOaLocation W42384553311 @default.
• W4238455331 hasConcept C115719804 @default.
• W4238455331 hasConcept C127313418 @default.
• W4238455331 hasConcept C153294291 @default.
• W4238455331 hasConcept C163861444 @default.
• W4238455331 hasConcept C171420983 @default.
• W4238455331 hasConcept C205649164 @default.
• W4238455331 hasConcept C2775840915 @default.
• W4238455331 hasConcept C2777517185 @default.
• W4238455331 hasConcept C39432304 @default.
• W4238455331 hasConcept C49204034 @default.
• W4238455331 hasConcept C49999975 @default.
• W4238455331 hasConcept C508106653 @default.
• W4238455331 hasConcept C9075549 @default.
• W4238455331 hasConcept C91586092 @default.
• W4238455331 hasConceptScore W4238455331C115719804 @default.
• W4238455331 hasConceptScore W4238455331C127313418 @default.
• W4238455331 hasConceptScore W4238455331C153294291 @default.
• W4238455331 hasConceptScore W4238455331C163861444 @default.
• W4238455331 hasConceptScore W4238455331C171420983 @default.
• W4238455331 hasConceptScore W4238455331C205649164 @default.
• W4238455331 hasConceptScore W4238455331C2775840915 @default.
• W4238455331 hasConceptScore W4238455331C2777517185 @default.
• W4238455331 hasConceptScore W4238455331C39432304 @default.
• W4238455331 hasConceptScore W4238455331C49204034 @default.

• next