FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2075310878> ?p ?o ?g. }

• W2075310878 endingPage "19681" @default.
• W2075310878 startingPage "19665" @default.
• W2075310878 abstract "This paper examines the high degree of linear dependence between multiwavelength extinction measurements of stratospheric aerosols and applies this to the problem of separating aerosol and gas contributions to the total measured extinction in the Stratospheric Aerosol and Gas Experiment (SAGE) II and Halogen Occultation Experiment (HALOE) satellite systems. Solar extinction recorded at wavelengths employed primarily for measuring gas densities inevitably includes a contribution from aerosols, whose spectral scattering behaviour depends on their unknown size distribution. Here linear relationships are determined to extract the aerosol contribution from the total extinction at the centers of the SAGE II ozone channel and the HALOE nitrogen dioxide and ozone broadband channels. The derived relationships are applied to both background and volcanic conditions. For the HALOE system we show how the currently employed two‐wavelength ratio gives accurate results for most commonly encountered particles sizes in the stratosphere. Although the use of multiple channels can improve the accuracy to which aerosols can be removed from HALOE gas channels, the sensitivity of the relationships to aerosol composition makes them impractical for routine processing. For the SAGE II experiment we show how inaccuracies in aerosol removal have affected the retrieved ozone concentration in the lower stratosphere. Under background conditions, SAGE II ozone concentrations are shown to be biased low by several percent, whereas in postvolcanic periods they are biased high. Prior to the eruption of Mount Pinatubo, SAGE II ozone concentrations below 20 km should be adjusted upward by up to 15% as too much of the measured 0.6 μm extinction has been attributed to aerosol. This change would exacerbate the discrepancy between SAGE II and ozonesonde data in the lower stratosphere throughout the 1980s. In the aftermath of Pinatubo the SAGE II ozone concentrations need to be adjusted downward by up to 15% as too little aerosol extinction was removed from the ozone channel. This shifting bias in the removal of aerosols by the SAGE II retrieval algorithm introduces an apparent downward trend in lower stratospheric ozone concentrations throughout the 1980s and early 1990s as the aerosol size distribution evolves during postvolcanic recovery periods. Trends as large as −2% per year have previously been reported from SAGE II data below 20 km. We show how a significant proportion of this could be explained by the incorrect aerosol removal." @default.
• W2075310878 created "2016-06-24" @default.
• W2075310878 creator A5025806674 @default.
• W2075310878 creator A5042275274 @default.
• W2075310878 date "1997-08-01" @default.
• W2075310878 modified "2023-09-26" @default.
• W2075310878 title "Separation of aerosol and gas components in the Halogen Occultation Experiment and the Stratospheric Aerosol and Gas Experiment (SAGE) II extinction measurements: Implications for SAGE II ozone concentrations and trends" @default.
• W2075310878 cites W1964625810 @default.
• W2075310878 cites W1976803590 @default.
• W2075310878 cites W1979041041 @default.
• W2075310878 cites W1987917766 @default.
• W2075310878 cites W1994653329 @default.
• W2075310878 cites W1999971203 @default.
• W2075310878 cites W2000464111 @default.
• W2075310878 cites W2005140191 @default.
• W2075310878 cites W2010598328 @default.
• W2075310878 cites W2014277569 @default.
• W2075310878 cites W2019428746 @default.
• W2075310878 cites W2019911081 @default.
• W2075310878 cites W2030054815 @default.
• W2075310878 cites W2034125765 @default.
• W2075310878 cites W2038424754 @default.
• W2075310878 cites W2039702279 @default.
• W2075310878 cites W2040623864 @default.
• W2075310878 cites W2044499513 @default.
• W2075310878 cites W2045623892 @default.
• W2075310878 cites W2046919106 @default.
• W2075310878 cites W2046926410 @default.
• W2075310878 cites W2047935199 @default.
• W2075310878 cites W2070411050 @default.
• W2075310878 cites W2071026014 @default.
• W2075310878 cites W2075501990 @default.
• W2075310878 cites W2078419246 @default.
• W2075310878 cites W2085191177 @default.
• W2075310878 cites W2086893237 @default.
• W2075310878 cites W2099685668 @default.
• W2075310878 cites W2100018797 @default.
• W2075310878 cites W2103800060 @default.
• W2075310878 cites W2122886072 @default.
• W2075310878 cites W2123592518 @default.
• W2075310878 cites W2142324838 @default.
• W2075310878 cites W2164896232 @default.
• W2075310878 doi "https://doi.org/10.1029/97jd01263" @default.
• W2075310878 hasPublicationYear "1997" @default.
• W2075310878 type Work @default.
• W2075310878 sameAs 2075310878 @default.
• W2075310878 citedByCount "35" @default.
• W2075310878 countsByYear W20753108782013 @default.
• W2075310878 countsByYear W20753108782015 @default.
• W2075310878 countsByYear W20753108782020 @default.
• W2075310878 countsByYear W20753108782022 @default.
• W2075310878 crossrefType "journal-article" @default.
• W2075310878 hasAuthorship W2075310878A5025806674 @default.
• W2075310878 hasAuthorship W2075310878A5042275274 @default.
• W2075310878 hasBestOaLocation W20753108781 @default.
• W2075310878 hasConcept C101991246 @default.
• W2075310878 hasConcept C115719804 @default.
• W2075310878 hasConcept C120665830 @default.
• W2075310878 hasConcept C121332964 @default.
• W2075310878 hasConcept C130047971 @default.
• W2075310878 hasConcept C131040042 @default.
• W2075310878 hasConcept C153294291 @default.
• W2075310878 hasConcept C163861444 @default.
• W2075310878 hasConcept C185592680 @default.
• W2075310878 hasConcept C199289684 @default.
• W2075310878 hasConcept C2779345167 @default.
• W2075310878 hasConcept C2779681926 @default.
• W2075310878 hasConcept C2780723490 @default.
• W2075310878 hasConcept C39432304 @default.
• W2075310878 hasConcept C44870925 @default.
• W2075310878 hasConcept C508106653 @default.
• W2075310878 hasConcept C6260449 @default.
• W2075310878 hasConcept C91586092 @default.
• W2075310878 hasConceptScore W2075310878C101991246 @default.
• W2075310878 hasConceptScore W2075310878C115719804 @default.
• W2075310878 hasConceptScore W2075310878C120665830 @default.
• W2075310878 hasConceptScore W2075310878C121332964 @default.
• W2075310878 hasConceptScore W2075310878C130047971 @default.
• W2075310878 hasConceptScore W2075310878C131040042 @default.
• W2075310878 hasConceptScore W2075310878C153294291 @default.
• W2075310878 hasConceptScore W2075310878C163861444 @default.
• W2075310878 hasConceptScore W2075310878C185592680 @default.
• W2075310878 hasConceptScore W2075310878C199289684 @default.
• W2075310878 hasConceptScore W2075310878C2779345167 @default.
• W2075310878 hasConceptScore W2075310878C2779681926 @default.
• W2075310878 hasConceptScore W2075310878C2780723490 @default.
• W2075310878 hasConceptScore W2075310878C39432304 @default.
• W2075310878 hasConceptScore W2075310878C44870925 @default.
• W2075310878 hasConceptScore W2075310878C508106653 @default.
• W2075310878 hasConceptScore W2075310878C6260449 @default.
• W2075310878 hasConceptScore W2075310878C91586092 @default.
• W2075310878 hasIssue "D16" @default.
• W2075310878 hasLocation W20753108781 @default.
• W2075310878 hasOpenAccess W2075310878 @default.
• W2075310878 hasPrimaryLocation W20753108781 @default.
• W2075310878 hasRelatedWork W2047411924 @default.
• W2075310878 hasRelatedWork W2062108531 @default.
• W2075310878 hasRelatedWork W2076470551 @default.

• next