Show simple item record

dc.contributor.authorMellado González, Juan Pedro
dc.contributor.authorStevens, Bjorn
dc.contributor.authorSchmidt, Heiko
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Física
dc.date.accessioned2020-06-02T16:43:08Z
dc.date.available2020-06-02T16:43:08Z
dc.date.issued2014-03-01
dc.identifier.citationMellado, J. P.; Stevens, B.; Schmidt, H. Wind Shear and Buoyancy Reversal at the Top of Stratocumulus. "Journal of the atmospheric sciences", 1 Març 2014, vol. 71, p. 1040-1057.
dc.identifier.issn0022-4928
dc.identifier.urihttp://hdl.handle.net/2117/189754
dc.description.abstractA numerical experiment is designed to study the interaction at the stratocumulus top between a mean vertical shear and the buoyancy reversal due to evaporative cooling, without radiative cooling. Direct numerical simulation is used to eliminate the uncertainty introduced by turbulence models. It is found that the enhancement by shear-induced mixing of the turbulence caused by buoyancy reversal can render buoyancy reversal comparable to other forcing mechanisms. However, it is also found that (i) the velocity jump across the capping inversion Du needs to be relatively large and values of about 1 m s21 that are typically associated with the convective motions inside the boundary layer are generally too small and (ii) there is no indication of cloud-top entrainment instability. To obtain these results, parameterizations of the mean entrainment velocity and the relevant time scales are derived from the study of the cloud-top vertical structure. Two overlapping layers can be identified: a background shear layer with a thickness (1/3)(Du) 2 /Db, where Db is the buoyancy increment across the capping inversion and a turbulence layer dominated by free convection inside the cloud and by shear production inside the relatively thin overlap region. As turbulence intensifies, the turbulence layer encroaches into the background shear layer and defines thereby the entrainment velocity. Particularized to the first research flight of the Second Dynamics and Chemistry of the Marine Stratocumulus (DYCOMS II) field campaign, the analysis predicts an entrainment velocity of about 3 mm s21 after 5–10 min—a velocity comparable to the measurements and thus indicative of the relevance of mean shear in that case.
dc.format.extent18 p.
dc.language.isoeng
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Spain
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subjectÀrees temàtiques de la UPC::Física
dc.subject.lcshClouds
dc.subject.lcshVertical wind shear
dc.subject.lcshCooling power (Meteorology)
dc.subject.lcshAtmospheric physics
dc.subject.otherEvaporative cooling: Radiative cooling
dc.subject.otherStratocumulus
dc.titleWind Shear and Buoyancy Reversal at the Top of Stratocumulus
dc.typeArticle
dc.subject.lemacNúvols
dc.subject.lemacFísica atmosfèrica
dc.identifier.doi10.1175/JAS-D-13-0189.1
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttps://journals.ametsoc.org/doi/full/10.1175/JAS-D-13-0189.1
dc.rights.accessOpen Access
local.identifier.drac27656126
dc.description.versionPostprint (published version)
local.citation.authorMellado, J. P.; Stevens, B.; Schmidt, H.
local.citation.publicationNameJournal of the atmospheric sciences
local.citation.volume71
local.citation.startingPage1040
local.citation.endingPage1057


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record

Attribution-NonCommercial-NoDerivs 3.0 Spain
Except where otherwise noted, content on this work is licensed under a Creative Commons license : Attribution-NonCommercial-NoDerivs 3.0 Spain