Matches in SemOpenAlex for { <https://semopenalex.org/work/W2607045632> ?p ?o ?g. }
Showing items 1 to 84 of
84
with 100 items per page.
- W2607045632 endingPage "457" @default.
- W2607045632 startingPage "440" @default.
- W2607045632 abstract "This paper concerns with properties of a thermal convection in a stably stratified Boussinesq fluid caused by partial heating or cooling of the lower boundary. For infinitesimal heating (cooling) the convective motion can be described by a linear theory. Introducing a suitable scaling, it is shown that the convection is controlled mainly by a non-dimensional parameter, R=αgΓl4/κν where Gamma; is the vertical temperature gradient in the basic state, l is the half-width of the heated (cooled) area and the other symbols have conventional meanings. The convective motion is confined to the frictional depth introduced by Stommel and Veronis (1957). For a single slab-symmetric heating (cooling) the thickness (the lowest height at which the temperature perturbation vanishes) is given by hT=3.6 R-l/6 and the maximum horizontal velocity by u*max=0.25, √αg/PγGamma;|Th| where Pγ=ν/κ and Th is the temperature difference between the heated (cooled) area and the surrounding area. The width of the upward (downward) motion area is close to the horizontal scale of the forcing area.The convection patterns for the finite-amplitude heating (cooling) were investigated by means of laboratory and numerical experiments for |Th|_??__??_l. It was observed that increase of the thickness of the boundary layer with Th is small. As for the convection caused by heating, however, the width of the upward motion area decreases with the increase of Th until the magnitude of the upward motion becomes comparable with that of the horizontal motion. As for the convection caused by cooling, the width of the downward motion area increases with |Th|, but the essential features of the convection pattern are similar to those for the infinitesimal cooling.These results are compared with available data of the convection due to the urban heat island effect." @default.
- W2607045632 created "2017-04-28" @default.
- W2607045632 creator A5075720898 @default.
- W2607045632 date "1975-01-01" @default.
- W2607045632 modified "2023-10-03" @default.
- W2607045632 title "Dynamics of Steady Convections Over Heat and Cool Islands" @default.
- W2607045632 cites W1979730981 @default.
- W2607045632 cites W1980193825 @default.
- W2607045632 cites W1986870706 @default.
- W2607045632 cites W2034194999 @default.
- W2607045632 cites W2053575937 @default.
- W2607045632 cites W2070663058 @default.
- W2607045632 cites W2074133059 @default.
- W2607045632 cites W2087560317 @default.
- W2607045632 cites W2105615138 @default.
- W2607045632 cites W2147418088 @default.
- W2607045632 cites W4210980582 @default.
- W2607045632 cites W4233502935 @default.
- W2607045632 cites W4248649832 @default.
- W2607045632 doi "https://doi.org/10.2151/jmsj1965.53.6_440" @default.
- W2607045632 hasPublicationYear "1975" @default.
- W2607045632 type Work @default.
- W2607045632 sameAs 2607045632 @default.
- W2607045632 citedByCount "41" @default.
- W2607045632 countsByYear W26070456322013 @default.
- W2607045632 countsByYear W26070456322016 @default.
- W2607045632 countsByYear W26070456322018 @default.
- W2607045632 countsByYear W26070456322020 @default.
- W2607045632 countsByYear W26070456322021 @default.
- W2607045632 countsByYear W26070456322023 @default.
- W2607045632 crossrefType "journal-article" @default.
- W2607045632 hasAuthorship W2607045632A5075720898 @default.
- W2607045632 hasBestOaLocation W26070456321 @default.
- W2607045632 hasConcept C10899652 @default.
- W2607045632 hasConcept C111603439 @default.
- W2607045632 hasConcept C113740112 @default.
- W2607045632 hasConcept C121332964 @default.
- W2607045632 hasConcept C127313418 @default.
- W2607045632 hasConcept C137109543 @default.
- W2607045632 hasConcept C153294291 @default.
- W2607045632 hasConcept C192562407 @default.
- W2607045632 hasConcept C204530211 @default.
- W2607045632 hasConcept C2524010 @default.
- W2607045632 hasConcept C33923547 @default.
- W2607045632 hasConcept C54791560 @default.
- W2607045632 hasConcept C57879066 @default.
- W2607045632 hasConcept C8058405 @default.
- W2607045632 hasConcept C99844830 @default.
- W2607045632 hasConceptScore W2607045632C10899652 @default.
- W2607045632 hasConceptScore W2607045632C111603439 @default.
- W2607045632 hasConceptScore W2607045632C113740112 @default.
- W2607045632 hasConceptScore W2607045632C121332964 @default.
- W2607045632 hasConceptScore W2607045632C127313418 @default.
- W2607045632 hasConceptScore W2607045632C137109543 @default.
- W2607045632 hasConceptScore W2607045632C153294291 @default.
- W2607045632 hasConceptScore W2607045632C192562407 @default.
- W2607045632 hasConceptScore W2607045632C204530211 @default.
- W2607045632 hasConceptScore W2607045632C2524010 @default.
- W2607045632 hasConceptScore W2607045632C33923547 @default.
- W2607045632 hasConceptScore W2607045632C54791560 @default.
- W2607045632 hasConceptScore W2607045632C57879066 @default.
- W2607045632 hasConceptScore W2607045632C8058405 @default.
- W2607045632 hasConceptScore W2607045632C99844830 @default.
- W2607045632 hasIssue "6" @default.
- W2607045632 hasLocation W26070456321 @default.
- W2607045632 hasOpenAccess W2607045632 @default.
- W2607045632 hasPrimaryLocation W26070456321 @default.
- W2607045632 hasRelatedWork W1969582476 @default.
- W2607045632 hasRelatedWork W1987480428 @default.
- W2607045632 hasRelatedWork W1991205155 @default.
- W2607045632 hasRelatedWork W2051277406 @default.
- W2607045632 hasRelatedWork W2053205414 @default.
- W2607045632 hasRelatedWork W2065907555 @default.
- W2607045632 hasRelatedWork W2132672914 @default.
- W2607045632 hasRelatedWork W2761755253 @default.
- W2607045632 hasRelatedWork W84742024 @default.
- W2607045632 hasRelatedWork W2426487851 @default.
- W2607045632 hasVolume "53" @default.
- W2607045632 isParatext "false" @default.
- W2607045632 isRetracted "false" @default.
- W2607045632 magId "2607045632" @default.
- W2607045632 workType "article" @default.