FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3203148128> ?p ?o ?g. }

• W3203148128 abstract "Abstract. Extreme convective events in the troposphere not only have immediate impacts on the surface, they can also influence the dynamics and composition of the lower stratosphere (LS). One major impact is the moistening of the LS by overshooting convection. This effect plays a crucial role in climate feedback as small changes of water vapor in the upper troposphere and lower stratosphere (UTLS) have a large impact on the radiation budget of the atmosphere. In this case study, we investigate water vapor injections into the LS by two consecutive convective events in the European mid-latitudes within the framework of the MOSES (Modular Observation Solutions for Earth Systems) measurement campaign during the early summer of 2019. Using balloon-borne instruments, rare measurements of the convective water vapor injection into the stratosphere were performed. The magnitude of the water vapor reached up to 12.1 ppmv with an estimated background value of 5 ppmv. Hence it is in the same order of magnitude as earlier reports of water vapor injection by convective overshooting above North America. However the overshooting took place in the extra-tropical stratosphere and has an impact on long-term water vapor mixing ratios in the stratosphere compared to the Monsoon-influenced region in North America. At the altitude of the measured injection, a sharp drop in a local ozone enhancement peak makes the observed composition of air very unique with high ozone up to 696 ppbv and high water vapor up to 12.1 ppmv. While ERA-Interim data does not show any signal of the convective overshoot, the measured values in the LS are underestimated by MLS satellite data and overestimated by ERA5 reanalysis data. Backward trajectories of the measured injected air masses reveal that the moistening of the LS took place several hours before the balloon launch. This is in good agreement with reanalyses and satellite data showing a strong change in the structure of isotherms, and a sudden and short-lived increase in potential vorticity at the altitude of the trajectory, as well as low cloud top brightness temperatures during the overshooting event." @default.
• W3203148128 created "2021-10-11" @default.
• W3203148128 creator A5029243561 @default.
• W3203148128 creator A5029366433 @default.
• W3203148128 creator A5036187203 @default.
• W3203148128 creator A5054025391 @default.
• W3203148128 creator A5060830810 @default.
• W3203148128 creator A5070306176 @default.
• W3203148128 creator A5076655435 @default.
• W3203148128 creator A5080245719 @default.
• W3203148128 date "2021-09-17" @default.
• W3203148128 modified "2023-09-23" @default.
• W3203148128 title "A case study on the impact of severe convective storms on the water vapor mixing ratio in the lower mid-latitude stratosphere observed in 2019 over Europe" @default.
• W3203148128 cites W2010142913 @default.
• W3203148128 cites W2011565179 @default.
• W3203148128 cites W2023874332 @default.
• W3203148128 cites W2033053636 @default.
• W3203148128 cites W2067513464 @default.
• W3203148128 cites W2071594560 @default.
• W3203148128 cites W2077730340 @default.
• W3203148128 cites W2081288537 @default.
• W3203148128 cites W2087262283 @default.
• W3203148128 cites W2088486052 @default.
• W3203148128 cites W2104718076 @default.
• W3203148128 cites W2115644419 @default.
• W3203148128 cites W2153559972 @default.
• W3203148128 cites W2156117950 @default.
• W3203148128 cites W2179767754 @default.
• W3203148128 cites W2747154523 @default.
• W3203148128 cites W2890344345 @default.
• W3203148128 cites W2980181288 @default.
• W3203148128 cites W3025949386 @default.
• W3203148128 cites W3035972944 @default.
• W3203148128 cites W3044868409 @default.
• W3203148128 cites W3048553107 @default.
• W3203148128 cites W2059027217 @default.
• W3203148128 doi "https://doi.org/10.5194/acp-2021-749" @default.
• W3203148128 hasPublicationYear "2021" @default.
• W3203148128 type Work @default.
• W3203148128 sameAs 3203148128 @default.
• W3203148128 citedByCount "0" @default.
• W3203148128 crossrefType "posted-content" @default.
• W3203148128 hasAuthorship W3203148128A5029243561 @default.
• W3203148128 hasAuthorship W3203148128A5029366433 @default.
• W3203148128 hasAuthorship W3203148128A5036187203 @default.
• W3203148128 hasAuthorship W3203148128A5054025391 @default.
• W3203148128 hasAuthorship W3203148128A5060830810 @default.
• W3203148128 hasAuthorship W3203148128A5070306176 @default.
• W3203148128 hasAuthorship W3203148128A5076655435 @default.
• W3203148128 hasAuthorship W3203148128A5080245719 @default.
• W3203148128 hasBestOaLocation W32031481281 @default.
• W3203148128 hasConcept C10899652 @default.
• W3203148128 hasConcept C122523270 @default.
• W3203148128 hasConcept C127313418 @default.
• W3203148128 hasConcept C13280743 @default.
• W3203148128 hasConcept C147534773 @default.
• W3203148128 hasConcept C153294291 @default.
• W3203148128 hasConcept C163861444 @default.
• W3203148128 hasConcept C18459110 @default.
• W3203148128 hasConcept C186816422 @default.
• W3203148128 hasConcept C192932206 @default.
• W3203148128 hasConcept C205649164 @default.
• W3203148128 hasConcept C2524010 @default.
• W3203148128 hasConcept C2776025126 @default.
• W3203148128 hasConcept C33923547 @default.
• W3203148128 hasConcept C39432304 @default.
• W3203148128 hasConcept C49204034 @default.
• W3203148128 hasConcept C6350597 @default.
• W3203148128 hasConcept C65440619 @default.
• W3203148128 hasConcept C9075549 @default.
• W3203148128 hasConcept C91586092 @default.
• W3203148128 hasConceptScore W3203148128C10899652 @default.
• W3203148128 hasConceptScore W3203148128C122523270 @default.
• W3203148128 hasConceptScore W3203148128C127313418 @default.
• W3203148128 hasConceptScore W3203148128C13280743 @default.
• W3203148128 hasConceptScore W3203148128C147534773 @default.
• W3203148128 hasConceptScore W3203148128C153294291 @default.
• W3203148128 hasConceptScore W3203148128C163861444 @default.
• W3203148128 hasConceptScore W3203148128C18459110 @default.
• W3203148128 hasConceptScore W3203148128C186816422 @default.
• W3203148128 hasConceptScore W3203148128C192932206 @default.
• W3203148128 hasConceptScore W3203148128C205649164 @default.
• W3203148128 hasConceptScore W3203148128C2524010 @default.
• W3203148128 hasConceptScore W3203148128C2776025126 @default.
• W3203148128 hasConceptScore W3203148128C33923547 @default.
• W3203148128 hasConceptScore W3203148128C39432304 @default.
• W3203148128 hasConceptScore W3203148128C49204034 @default.
• W3203148128 hasConceptScore W3203148128C6350597 @default.
• W3203148128 hasConceptScore W3203148128C65440619 @default.
• W3203148128 hasConceptScore W3203148128C9075549 @default.
• W3203148128 hasConceptScore W3203148128C91586092 @default.
• W3203148128 hasLocation W32031481281 @default.
• W3203148128 hasLocation W32031481282 @default.
• W3203148128 hasLocation W32031481283 @default.
• W3203148128 hasOpenAccess W3203148128 @default.
• W3203148128 hasPrimaryLocation W32031481281 @default.
• W3203148128 hasRelatedWork W1972065018 @default.
• W3203148128 hasRelatedWork W1990369235 @default.
• W3203148128 hasRelatedWork W2072648020 @default.
• W3203148128 hasRelatedWork W2349032817 @default.

• next