FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2523677473> ?p ?o ?g. }

• W2523677473 endingPage "5100" @default.
• W2523677473 startingPage "5081" @default.
• W2523677473 abstract "Abstract The vertical propagation and attenuation of mountain waves launched by New Zealand terrain during the Deep Propagating Gravity Wave Experiment (DEEPWAVE) field campaign are investigated. New Zealand mountain waves were frequently attenuated in a lower-stratospheric weak wind layer between z = 15 and 25 km. This layer is termed a “valve layer,” as conditions within this layer (primarily minimum wind speed) control mountain wave momentum flux through it, analogous to a valve controlling mass flux through a pipe. This valve layer is a climatological feature in the wintertime midlatitude lower stratosphere above the subtropical jet. Mountain wave dynamics within this valve layer are studied using realistic Weather Research and Forecasting (WRF) Model simulations that were extensively validated against research aircraft, radiosonde, and satellite observations. Locally, wave attenuation is horizontally and vertically inhomogeneous, evidenced by numerous regions with wave-induced low Richardson numbers and potential vorticity generation. WRF-simulated gravity wave drag (GWD) is peaked in the valve layer, and momentum flux transmitted through this layer is well approximated by a cubic function of minimum ambient wind speed within it, consistent with linear saturation theory. Valve-layer GWD within the well-validated WRF simulations was 3–6 times larger than that parameterized within MERRA. Previous research suggests increasing parameterized orographic GWD (performed in MERRA2) decreases the stratospheric polar vortex strength by altering planetary wave propagation and drag. The results reported here suggest carefully increasing orographic GWD is warranted, which may help to ameliorate the common cold-pole problem in chemistry–climate models." @default.
• W2523677473 created "2016-09-30" @default.
• W2523677473 creator A5044530866 @default.
• W2523677473 creator A5053108676 @default.
• W2523677473 creator A5060085491 @default.
• W2523677473 date "2016-12-01" @default.
• W2523677473 modified "2023-10-16" @default.
• W2523677473 title "The Midlatitude Lower-Stratospheric Mountain Wave “Valve Layer”" @default.
• W2523677473 cites W1544532437 @default.
• W2523677473 cites W1623656619 @default.
• W2523677473 cites W1853020041 @default.
• W2523677473 cites W1944878026 @default.
• W2523677473 cites W1949405806 @default.
• W2523677473 cites W1979601660 @default.
• W2523677473 cites W1985550815 @default.
• W2523677473 cites W1985591854 @default.
• W2523677473 cites W1988497189 @default.
• W2523677473 cites W1989788229 @default.
• W2523677473 cites W1996730960 @default.
• W2523677473 cites W1997132789 @default.
• W2523677473 cites W2019512707 @default.
• W2523677473 cites W2051416171 @default.
• W2523677473 cites W2057507785 @default.
• W2523677473 cites W2078720578 @default.
• W2523677473 cites W2099639803 @default.
• W2523677473 cites W2108896901 @default.
• W2523677473 cites W2124804734 @default.
• W2523677473 cites W2126532189 @default.
• W2523677473 cites W2139011662 @default.
• W2523677473 cites W2141319951 @default.
• W2523677473 cites W2144617861 @default.
• W2523677473 cites W2158993832 @default.
• W2523677473 cites W2171690040 @default.
• W2523677473 cites W2172622149 @default.
• W2523677473 cites W2192962990 @default.
• W2523677473 cites W2295260029 @default.
• W2523677473 cites W2549450207 @default.
• W2523677473 cites W4232473186 @default.
• W2523677473 cites W4236172704 @default.
• W2523677473 doi "https://doi.org/10.1175/jas-d-16-0173.1" @default.
• W2523677473 hasPublicationYear "2016" @default.
• W2523677473 type Work @default.
• W2523677473 sameAs 2523677473 @default.
• W2523677473 citedByCount "34" @default.
• W2523677473 countsByYear W25236774732017 @default.
• W2523677473 countsByYear W25236774732018 @default.
• W2523677473 countsByYear W25236774732019 @default.
• W2523677473 countsByYear W25236774732020 @default.
• W2523677473 countsByYear W25236774732021 @default.
• W2523677473 countsByYear W25236774732022 @default.
• W2523677473 countsByYear W25236774732023 @default.
• W2523677473 crossrefType "journal-article" @default.
• W2523677473 hasAuthorship W2523677473A5044530866 @default.
• W2523677473 hasAuthorship W2523677473A5053108676 @default.
• W2523677473 hasAuthorship W2523677473A5060085491 @default.
• W2523677473 hasBestOaLocation W25236774731 @default.
• W2523677473 hasConcept C11999413 @default.
• W2523677473 hasConcept C121332964 @default.
• W2523677473 hasConcept C127313418 @default.
• W2523677473 hasConcept C133204551 @default.
• W2523677473 hasConcept C153294291 @default.
• W2523677473 hasConcept C163861444 @default.
• W2523677473 hasConcept C18101618 @default.
• W2523677473 hasConcept C185975314 @default.
• W2523677473 hasConcept C190330329 @default.
• W2523677473 hasConcept C44870925 @default.
• W2523677473 hasConcept C49204034 @default.
• W2523677473 hasConcept C8058405 @default.
• W2523677473 hasConcept C91586092 @default.
• W2523677473 hasConceptScore W2523677473C11999413 @default.
• W2523677473 hasConceptScore W2523677473C121332964 @default.
• W2523677473 hasConceptScore W2523677473C127313418 @default.
• W2523677473 hasConceptScore W2523677473C133204551 @default.
• W2523677473 hasConceptScore W2523677473C153294291 @default.
• W2523677473 hasConceptScore W2523677473C163861444 @default.
• W2523677473 hasConceptScore W2523677473C18101618 @default.
• W2523677473 hasConceptScore W2523677473C185975314 @default.
• W2523677473 hasConceptScore W2523677473C190330329 @default.
• W2523677473 hasConceptScore W2523677473C44870925 @default.
• W2523677473 hasConceptScore W2523677473C49204034 @default.
• W2523677473 hasConceptScore W2523677473C8058405 @default.
• W2523677473 hasConceptScore W2523677473C91586092 @default.
• W2523677473 hasFunder F4320337402 @default.
• W2523677473 hasIssue "12" @default.
• W2523677473 hasLocation W25236774731 @default.
• W2523677473 hasOpenAccess W2523677473 @default.
• W2523677473 hasPrimaryLocation W25236774731 @default.
• W2523677473 hasRelatedWork W1538385640 @default.
• W2523677473 hasRelatedWork W2003484586 @default.
• W2523677473 hasRelatedWork W2007163268 @default.
• W2523677473 hasRelatedWork W2068704216 @default.
• W2523677473 hasRelatedWork W2078722141 @default.
• W2523677473 hasRelatedWork W2120142082 @default.
• W2523677473 hasRelatedWork W2143286209 @default.
• W2523677473 hasRelatedWork W2180331340 @default.
• W2523677473 hasRelatedWork W2576580918 @default.
• W2523677473 hasRelatedWork W2900860813 @default.
• W2523677473 hasVolume "73" @default.

• next