bibo:abstract
  • This study is concerned with properties of a thermal convection in a stably stratified Boussinesq fluid caused by partial heating at the lower boundary. For thins purpose, two-dimensional, nonrotating system was employed. U the heating is very strong, convection takes the form of a turbulent plume. Otherwise, remains laminar. If the partial heating at the bottom boundary is symmetric. the convection takes the form of axisymmetric with respect to the z-axis. but heating form is not so significant as to alter the main features of the horizontal convection. The convective motion consists of two-cell with the convergence in the lower layer at the center of the partial heating area. The temperature perturbation is characterized by the temperature 'Cross-Over' over the partial heating area. These features are cleared according to the increase of temperature difference between the center and side part of the bottom boundary. (rdf:langString) (en)
nlon:biographicalNote
  • 김유근, 부산대학교 대기과학과 (xsd:string)
  • 김해동, 기상연구소 원격탐사연구실 (xsd:string)
  • 이화운, 부산대학교 대기과학과 (xsd:string)
  • 정우식, 부산대학교 대기과학과 (xsd:string)
nlon:classificationNumberOfNLK
  • 539.905 (xsd:string)
nlon:containedIn
dc:creator
  • 김유근 (xsd:string)
  • 김해동 (xsd:string)
  • 이화운 (xsd:string)
  • 정우식 (xsd:string)
dcterms:creator
nlon:datePublished
  • 2021-01-30T23:37:12 (xsd:dateTime)
dcterms:description
  • (A)numerical simulation of horizontal convection in mesoscale (xsd:string)
bibframe:extent
  • 26 cm (xsd:string)
  • p. 233-241 (xsd:string)
  • 삽도 (xsd:string)
dcterms:isPartOf
nlon:issuedYear
  • 1998 (xsd:string)
nlon:itemNumberOfNLK
  • 한648ㅎ (xsd:string)
rdfs:label
  • 중규모에서의 수평대류에 관한 수치모의 / 정우식, 이화운,김유근,김해동 (xsd:string)
dcterms:language
dc:subject
  • Horizontal convection (xsd:string)
  • Mesoscale (xsd:string)
  • Partial heating (xsd:string)
  • 수평대류 (xsd:string)
  • 중규모 (xsd:string)
dcterms:title
  • 중규모에서의 수평대류에 관한 수치모의 (xsd:string)
rdf:type
nlon:volumeOfNLK
  • 7(2) (xsd:string)