FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2557248897> ?p ?o ?g. }

• W2557248897 abstract "Abstract. Observation and simulation of individual ozone streamers are important for the description and understanding of non-linear transport processes in the middle atmosphere. A sudden increase in mid-stratospheric ozone occurred above central Europe on 4 December 2015. The GROund-based Millimeter-wave Ozone Spectrometer (GROMOS) and the Stratospheric Ozone MOnitoring RAdiometer (SOMORA) in Switzerland measured an ozone enhancement of about 30 % at 34 km altitude (8.3 hPa) from 1 to 4 December. A similar ozone increase is simulated by the Specified Dynamics Whole Atmosphere Community Climate (SD-WACCM) model. Further, the global ozone fields at 34 km altitude (8.3 hPa) from SD-WACCM and the satellite experiment Aura/MLS show a remarkable agreement for the location and timing of an ozone streamer (large-scale tongue-like structure) extending from the subtropics in northern America over the Atlantic to central Europe. This agreement indicates that SD-WACCM can inform us about the wind inside the Atlantic ozone streamer. SD-WACCM shows an eastward wind of about 100 m s−1 inside the Atlantic streamer in the mid-stratosphere. SD-WACCM shows that the Atlantic streamer flows along the edge of the polar vortex. The Atlantic streamer turns southward at an erosion region of the polar vortex located above the Caspian Sea. The spatial distribution of stratospheric water vapour indicates a filament outgoing from this erosion region. The Atlantic streamer, the polar vortex erosion region and the water vapour filament belong to the process of planetary wave breaking in the so-called surf zone of the northern midlatitude winter stratosphere." @default.
• W2557248897 created "2016-12-08" @default.
• W2557248897 creator A5025235944 @default.
• W2557248897 creator A5037503840 @default.
• W2557248897 creator A5048575226 @default.
• W2557248897 creator A5057938268 @default.
• W2557248897 creator A5082279312 @default.
• W2557248897 date "2017-03-10" @default.
• W2557248897 modified "2023-10-17" @default.
• W2557248897 title "An Atlantic streamer in stratospheric ozone observations and SD-WACCM simulation data" @default.
• W2557248897 cites W1488621090 @default.
• W2557248897 cites W1826216157 @default.
• W2557248897 cites W1976353606 @default.
• W2557248897 cites W1979242650 @default.
• W2557248897 cites W1992480812 @default.
• W2557248897 cites W1996072029 @default.
• W2557248897 cites W2002348323 @default.
• W2557248897 cites W2006451550 @default.
• W2557248897 cites W2012196264 @default.
• W2557248897 cites W2021855984 @default.
• W2557248897 cites W2027317218 @default.
• W2557248897 cites W2029686238 @default.
• W2557248897 cites W2032657191 @default.
• W2557248897 cites W2035187320 @default.
• W2557248897 cites W2043273584 @default.
• W2557248897 cites W2073247131 @default.
• W2557248897 cites W2080449145 @default.
• W2557248897 cites W2087084815 @default.
• W2557248897 cites W2091100289 @default.
• W2557248897 cites W2104718076 @default.
• W2557248897 cites W2106475005 @default.
• W2557248897 cites W2120768943 @default.
• W2557248897 cites W2138350700 @default.
• W2557248897 cites W2164533140 @default.
• W2557248897 cites W2165563089 @default.
• W2557248897 doi "https://doi.org/10.5194/acp-17-3445-2017" @default.
• W2557248897 hasPublicationYear "2017" @default.
• W2557248897 type Work @default.
• W2557248897 sameAs 2557248897 @default.
• W2557248897 citedByCount "1" @default.
• W2557248897 countsByYear W25572488972019 @default.
• W2557248897 crossrefType "journal-article" @default.
• W2557248897 hasAuthorship W2557248897A5025235944 @default.
• W2557248897 hasAuthorship W2557248897A5037503840 @default.
• W2557248897 hasAuthorship W2557248897A5048575226 @default.
• W2557248897 hasAuthorship W2557248897A5057938268 @default.
• W2557248897 hasAuthorship W2557248897A5082279312 @default.
• W2557248897 hasBestOaLocation W25572488971 @default.
• W2557248897 hasConcept C108619276 @default.
• W2557248897 hasConcept C115719804 @default.
• W2557248897 hasConcept C125405218 @default.
• W2557248897 hasConcept C127313418 @default.
• W2557248897 hasConcept C134097258 @default.
• W2557248897 hasConcept C153294291 @default.
• W2557248897 hasConcept C163861444 @default.
• W2557248897 hasConcept C205649164 @default.
• W2557248897 hasConcept C2524010 @default.
• W2557248897 hasConcept C2779547961 @default.
• W2557248897 hasConcept C33923547 @default.
• W2557248897 hasConcept C39432304 @default.
• W2557248897 hasConcept C49204034 @default.
• W2557248897 hasConcept C508106653 @default.
• W2557248897 hasConcept C6350597 @default.
• W2557248897 hasConcept C65440619 @default.
• W2557248897 hasConcept C91586092 @default.
• W2557248897 hasConceptScore W2557248897C108619276 @default.
• W2557248897 hasConceptScore W2557248897C115719804 @default.
• W2557248897 hasConceptScore W2557248897C125405218 @default.
• W2557248897 hasConceptScore W2557248897C127313418 @default.
• W2557248897 hasConceptScore W2557248897C134097258 @default.
• W2557248897 hasConceptScore W2557248897C153294291 @default.
• W2557248897 hasConceptScore W2557248897C163861444 @default.
• W2557248897 hasConceptScore W2557248897C205649164 @default.
• W2557248897 hasConceptScore W2557248897C2524010 @default.
• W2557248897 hasConceptScore W2557248897C2779547961 @default.
• W2557248897 hasConceptScore W2557248897C33923547 @default.
• W2557248897 hasConceptScore W2557248897C39432304 @default.
• W2557248897 hasConceptScore W2557248897C49204034 @default.
• W2557248897 hasConceptScore W2557248897C508106653 @default.
• W2557248897 hasConceptScore W2557248897C6350597 @default.
• W2557248897 hasConceptScore W2557248897C65440619 @default.
• W2557248897 hasConceptScore W2557248897C91586092 @default.
• W2557248897 hasFunder F4320320924 @default.
• W2557248897 hasLocation W25572488971 @default.
• W2557248897 hasLocation W25572488972 @default.
• W2557248897 hasOpenAccess W2557248897 @default.
• W2557248897 hasPrimaryLocation W25572488971 @default.
• W2557248897 hasRelatedWork W1483603240 @default.
• W2557248897 hasRelatedWork W1489857386 @default.
• W2557248897 hasRelatedWork W180563958 @default.
• W2557248897 hasRelatedWork W2012108625 @default.
• W2557248897 hasRelatedWork W2072320772 @default.
• W2557248897 hasRelatedWork W2100550490 @default.
• W2557248897 hasRelatedWork W2106868533 @default.
• W2557248897 hasRelatedWork W2114025531 @default.
• W2557248897 hasRelatedWork W2288609308 @default.
• W2557248897 hasRelatedWork W2288691784 @default.
• W2557248897 hasRelatedWork W2302543561 @default.
• W2557248897 hasRelatedWork W2418236288 @default.
• W2557248897 hasRelatedWork W2516274472 @default.

• next