FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2123149383> ?p ?o ?g. }

• W2123149383 endingPage "11,507" @default.
• W2123149383 startingPage "11,493" @default.
• W2123149383 abstract "[1] The proportion of polar stratospheric clouds due to orographic gravity wave (OGW) forcing is quantified during four Antarctic (2007–2010) and four Arctic (2006/2007 to 2009/2010) winter seasons. OGW‒active days are defined as those days above major polar mountain ranges which have wave‒ice polar stratospheric clouds (PSCs), tropospheric wind conditions appropriate for orographic wave generation and propagation, and stratospheric temperatures below the frost point: 37% of Antarctic days and 12% of Arctic days are OGW‒active. Regions downstream of these mountain ranges are defined using a forward‒trajectory model which follows particle movement from ridge lines for 24 h periods. In both hemispheres in these mountain regions, more than 75% of H2O ice PSCs and around 50% of a high number density liquid‒nitric acid trihydrate mixture class (Mix 2‒enh) are attributed to OGW activity, with the balances due to non‒orographic formation. For the whole Arctic (equatorward of 82°), 25% of Mix 2‒enh and 54% of H2O ice PSCs are attributed to OGWs, while for the whole Antarctic, 7% of Mix 2‒enh and 13% of H2O ice PSCs are attributed to OGWs. For all types of PSC, 5% in the whole Antarctic and 12% in the whole Arctic are attributed to OGW forcing. While gravity waves play a role in PSC formation in the Antarctic, overall it is minor compared with other forcing sources. However, in the synoptically warmer Arctic, much larger proportions of PSCs are due to OGW activity." @default.
• W2123149383 created "2016-06-24" @default.
• W2123149383 creator A5012009216 @default.
• W2123149383 creator A5021333128 @default.
• W2123149383 creator A5028139800 @default.
• W2123149383 creator A5079386365 @default.
• W2123149383 date "2013-10-21" @default.
• W2123149383 modified "2023-09-27" @default.
• W2123149383 title "Quantifying the role of orographic gravity waves on polar stratospheric cloud occurrence in the Antarctic and the Arctic" @default.
• W2123149383 cites W1484516884 @default.
• W2123149383 cites W1488824683 @default.
• W2123149383 cites W1964065357 @default.
• W2123149383 cites W1977072837 @default.
• W2123149383 cites W1979849154 @default.
• W2123149383 cites W1981434441 @default.
• W2123149383 cites W1983308350 @default.
• W2123149383 cites W1983437298 @default.
• W2123149383 cites W1996422817 @default.
• W2123149383 cites W1997089932 @default.
• W2123149383 cites W1998099478 @default.
• W2123149383 cites W2000780733 @default.
• W2123149383 cites W2002348323 @default.
• W2123149383 cites W2005192947 @default.
• W2123149383 cites W2008277100 @default.
• W2123149383 cites W2013541067 @default.
• W2123149383 cites W2014885181 @default.
• W2123149383 cites W2017795014 @default.
• W2123149383 cites W2017965425 @default.
• W2123149383 cites W2020505699 @default.
• W2123149383 cites W2021959819 @default.
• W2123149383 cites W2031043891 @default.
• W2123149383 cites W2046534941 @default.
• W2123149383 cites W2047638950 @default.
• W2123149383 cites W2050066456 @default.
• W2123149383 cites W2050680567 @default.
• W2123149383 cites W2063477709 @default.
• W2123149383 cites W2069698589 @default.
• W2123149383 cites W2070758248 @default.
• W2123149383 cites W2076533338 @default.
• W2123149383 cites W2076785672 @default.
• W2123149383 cites W2088857912 @default.
• W2123149383 cites W2089444803 @default.
• W2123149383 cites W2092792319 @default.
• W2123149383 cites W2093808168 @default.
• W2123149383 cites W2096084973 @default.
• W2123149383 cites W2101972656 @default.
• W2123149383 cites W2104718076 @default.
• W2123149383 cites W2120653142 @default.
• W2123149383 cites W2121745948 @default.
• W2123149383 cites W2126341582 @default.
• W2123149383 cites W2151676805 @default.
• W2123149383 cites W2152219023 @default.
• W2123149383 cites W2154037629 @default.
• W2123149383 cites W2155191729 @default.
• W2123149383 cites W2169229194 @default.
• W2123149383 cites W2169993534 @default.
• W2123149383 cites W2172077960 @default.
• W2123149383 cites W3102820010 @default.
• W2123149383 cites W4242144118 @default.
• W2123149383 cites W4250266685 @default.
• W2123149383 doi "https://doi.org/10.1002/2013jd020122" @default.
• W2123149383 hasPublicationYear "2013" @default.
• W2123149383 type Work @default.
• W2123149383 sameAs 2123149383 @default.
• W2123149383 citedByCount "32" @default.
• W2123149383 countsByYear W21231493832014 @default.
• W2123149383 countsByYear W21231493832015 @default.
• W2123149383 countsByYear W21231493832016 @default.
• W2123149383 countsByYear W21231493832017 @default.
• W2123149383 countsByYear W21231493832018 @default.
• W2123149383 countsByYear W21231493832019 @default.
• W2123149383 countsByYear W21231493832020 @default.
• W2123149383 countsByYear W21231493832021 @default.
• W2123149383 countsByYear W21231493832023 @default.
• W2123149383 crossrefType "journal-article" @default.
• W2123149383 hasAuthorship W2123149383A5012009216 @default.
• W2123149383 hasAuthorship W2123149383A5021333128 @default.
• W2123149383 hasAuthorship W2123149383A5028139800 @default.
• W2123149383 hasAuthorship W2123149383A5079386365 @default.
• W2123149383 hasBestOaLocation W21231493831 @default.
• W2123149383 hasConcept C107054158 @default.
• W2123149383 hasConcept C111368507 @default.
• W2123149383 hasConcept C121332964 @default.
• W2123149383 hasConcept C127313418 @default.
• W2123149383 hasConcept C1276947 @default.
• W2123149383 hasConcept C134295995 @default.
• W2123149383 hasConcept C153294291 @default.
• W2123149383 hasConcept C163861444 @default.
• W2123149383 hasConcept C194507410 @default.
• W2123149383 hasConcept C197115733 @default.
• W2123149383 hasConcept C29705727 @default.
• W2123149383 hasConcept C39432304 @default.
• W2123149383 hasConcept C49204034 @default.
• W2123149383 hasConcept C518008717 @default.
• W2123149383 hasConcept C91586092 @default.
• W2123149383 hasConceptScore W2123149383C107054158 @default.
• W2123149383 hasConceptScore W2123149383C111368507 @default.
• W2123149383 hasConceptScore W2123149383C121332964 @default.

• next