FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2004368876> ?p ?o ?g. }

• W2004368876 endingPage "1027" @default.
• W2004368876 startingPage "1007" @default.
• W2004368876 abstract "A simple, steady, moist, axisymmetric, constant-depth, slab model for the hurricane boundary layer is investigated. High-resolution solutions of the boundary-layer equations are obtained by integrating inwards from some large radius, at which it is assumed that geostrophic balance and convective–radiative balance exist. In all the solutions obtained, the tangential wind speed in the boundary layer approaches that above the boundary layer in the inner-core region and the maximum wind speed in the boundary layer is comparable with, or even marginally higher than that above. A new feature of one of the solutions described is the existence of spatial oscillations in vertical velocity at the top of the boundary layer, inside the radius of maximum tangential wind speed. These oscillations may be interpreted as frictionally damped inertial waves. They are accompanied by annular regions in which the tangential flow alternates between supergradient and subgradient. The existence of boundary-layer-induced oscillations in vertical velocity in reality would have implications for the organization of convection in the core region of a hurricane. It is shown that an approximation to determine the radial flow in the boundary layer suggested by Willoughby overestimates the vertical motion at the top of the boundary layer by a factor of about two, but the analysis leads us to question the utility of the approximation. We investigate also the thermodynamic structure of the boundary layer and the radial distribution of surface fluxes for vortices with the same maximum tangential wind speed above the boundary layer and the same radius of maximum wind (RMW), but having different widths. It is found that the equivalent potential temperature (θe) in the boundary layer continues to increase with decreasing radius inside the RMW. Moreover, the negative radial gradient of θe in the inner-core region, which is related to that of virtual temperature above the boundary layer in the eyewall region, is relatively insensitive to the vortex width, but the maximum values of θe increase with the width. The strength and radial distribution of the latent-heat flux is insensitive to the vortex width in the inner-core region, but varies markedly with width in the outer part of the vortex. Realistic radial distribution of relative humidity are obtained only when shallow convection is represented in the model. The inclusion of dissipative heating in the thermodynamic equation leads to an increase in θe of the order of 1.5 K in the inner-core region of the vortex and to a reduction in the boundary-layer relative humidity of 5%. Copyright © 2003 Royal Meteorological Society" @default.
• W2004368876 created "2016-06-24" @default.
• W2004368876 creator A5047527760 @default.
• W2004368876 date "2003-01-01" @default.
• W2004368876 modified "2023-10-02" @default.
• W2004368876 title "A simple model of the hurricane boundary layer" @default.
• W2004368876 cites W1975205672 @default.
• W2004368876 cites W1989638758 @default.
• W2004368876 cites W1993412011 @default.
• W2004368876 cites W1996418370 @default.
• W2004368876 cites W2001336149 @default.
• W2004368876 cites W2023490218 @default.
• W2004368876 cites W2025506259 @default.
• W2004368876 cites W2027921998 @default.
• W2004368876 cites W2036885847 @default.
• W2004368876 cites W2057708103 @default.
• W2004368876 cites W2058588889 @default.
• W2004368876 cites W2058740778 @default.
• W2004368876 cites W2069201694 @default.
• W2004368876 cites W2100924595 @default.
• W2004368876 cites W2112338325 @default.
• W2004368876 cites W2122559342 @default.
• W2004368876 cites W2129549246 @default.
• W2004368876 cites W2143187501 @default.
• W2004368876 cites W2172970791 @default.
• W2004368876 cites W2174096611 @default.
• W2004368876 cites W2177506136 @default.
• W2004368876 cites W2598575790 @default.
• W2004368876 cites W4235954819 @default.
• W2004368876 cites W627007294 @default.
• W2004368876 cites W86326337 @default.
• W2004368876 doi "https://doi.org/10.1256/qj.01.197" @default.
• W2004368876 hasPublicationYear "2003" @default.
• W2004368876 type Work @default.
• W2004368876 sameAs 2004368876 @default.
• W2004368876 citedByCount "68" @default.
• W2004368876 countsByYear W20043688762012 @default.
• W2004368876 countsByYear W20043688762013 @default.
• W2004368876 countsByYear W20043688762014 @default.
• W2004368876 countsByYear W20043688762015 @default.
• W2004368876 countsByYear W20043688762016 @default.
• W2004368876 countsByYear W20043688762017 @default.
• W2004368876 countsByYear W20043688762018 @default.
• W2004368876 countsByYear W20043688762019 @default.
• W2004368876 countsByYear W20043688762020 @default.
• W2004368876 countsByYear W20043688762021 @default.
• W2004368876 countsByYear W20043688762022 @default.
• W2004368876 countsByYear W20043688762023 @default.
• W2004368876 crossrefType "journal-article" @default.
• W2004368876 hasAuthorship W2004368876A5047527760 @default.
• W2004368876 hasBestOaLocation W20043688762 @default.
• W2004368876 hasConcept C111603439 @default.
• W2004368876 hasConcept C121332964 @default.
• W2004368876 hasConcept C133877212 @default.
• W2004368876 hasConcept C134306372 @default.
• W2004368876 hasConcept C151890184 @default.
• W2004368876 hasConcept C178635117 @default.
• W2004368876 hasConcept C2524010 @default.
• W2004368876 hasConcept C33923547 @default.
• W2004368876 hasConcept C38652104 @default.
• W2004368876 hasConcept C41008148 @default.
• W2004368876 hasConcept C49221354 @default.
• W2004368876 hasConcept C57879066 @default.
• W2004368876 hasConcept C62354387 @default.
• W2004368876 hasConcept C74650414 @default.
• W2004368876 hasConceptScore W2004368876C111603439 @default.
• W2004368876 hasConceptScore W2004368876C121332964 @default.
• W2004368876 hasConceptScore W2004368876C133877212 @default.
• W2004368876 hasConceptScore W2004368876C134306372 @default.
• W2004368876 hasConceptScore W2004368876C151890184 @default.
• W2004368876 hasConceptScore W2004368876C178635117 @default.
• W2004368876 hasConceptScore W2004368876C2524010 @default.
• W2004368876 hasConceptScore W2004368876C33923547 @default.
• W2004368876 hasConceptScore W2004368876C38652104 @default.
• W2004368876 hasConceptScore W2004368876C41008148 @default.
• W2004368876 hasConceptScore W2004368876C49221354 @default.
• W2004368876 hasConceptScore W2004368876C57879066 @default.
• W2004368876 hasConceptScore W2004368876C62354387 @default.
• W2004368876 hasConceptScore W2004368876C74650414 @default.
• W2004368876 hasIssue "589" @default.
• W2004368876 hasLocation W20043688761 @default.
• W2004368876 hasLocation W20043688762 @default.
• W2004368876 hasOpenAccess W2004368876 @default.
• W2004368876 hasPrimaryLocation W20043688761 @default.
• W2004368876 hasRelatedWork W1546435160 @default.
• W2004368876 hasRelatedWork W1577120718 @default.
• W2004368876 hasRelatedWork W1977499649 @default.
• W2004368876 hasRelatedWork W2002238875 @default.
• W2004368876 hasRelatedWork W2137493924 @default.
• W2004368876 hasRelatedWork W2510403086 @default.
• W2004368876 hasRelatedWork W2923872275 @default.
• W2004368876 hasRelatedWork W66197931 @default.
• W2004368876 hasRelatedWork W1586431784 @default.
• W2004368876 hasRelatedWork W227479670 @default.
• W2004368876 hasVolume "129" @default.
• W2004368876 isParatext "false" @default.
• W2004368876 isRetracted "false" @default.
• W2004368876 magId "2004368876" @default.

• next