On the Effect of Surface Heat-Flux Heterogeneities on the Mixed-Layer-Top Entrainment

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dc.identifier.uri http://dx.doi.org/10.15488/929
dc.identifier.uri http://www.repo.uni-hannover.de/handle/123456789/953
dc.contributor.author Sühring, Matthias
dc.contributor.author Maronga, Björn
dc.contributor.author Herbort, Florian
dc.contributor.author Raasch, Siegfried
dc.date.accessioned 2016-12-21T14:07:24Z
dc.date.available 2016-12-21T14:07:24Z
dc.date.issued 2014
dc.identifier.citation Sühring, M.; Maronga, B.; Herbort, F.; Raasch, S.: On the Effect of Surface Heat-Flux Heterogeneities on the Mixed-Layer-Top Entrainment. In: Boundary-Layer Meteorology 151 (2014), Nr. 3, S. 531-556. DOI: https://doi.org/10.1007/s10546-014-9913-7
dc.description.abstract We used a set of large-eddy simulations to investigate the effect of one-dimensional stripe-like surface heat-flux heterogeneities on mixed-layer top entrainment. The profiles of sensible heat flux and the temporal evolution of the boundary-layer depth revealed decreased entrainment for small heat-flux amplitudes and increased entrainment for large heat-flux amplitudes, compared to the homogeneously-heated mixed layer. For large heat-flux amplitudes the largest entrainment was observed for patch sizes in the order of the boundary-layer depth, while for significantly smaller or larger patch sizes entrainment was similar as in the homogeneous case. In order to understand the underlying physics of this impact, a new approach was developed to infer local information on entrainment by means of the local flux divergence. We found an entrainment maximum over the centre of the stronger heated surface patch, where thermal energy is accumulated by the secondary circulation (SC) that was induced by the surface heterogeneity. Furthermore, we observed an entrainment maximum over the less heated patch as well, which we suppose is to be linked to the SC-induced horizontal flow convergence at the top of the convective boundary layer (CBL). For small heat-flux amplitudes a counteracting effect dominates that decreases entrainment, which we suppose is the horizontal advection of cold air in the lower, and warm air in the upper, CBL by the SC, stabilizing the CBL and thus weakening thermal convection. Moreover, we found that a mean wind can reduce the heterogeneity-induced impact on entrainment. If the flow is aligned perpendicular to the border between the differentially-heated patches, the SC and thus its impact on entrainment vanishes due to increased horizontal mixing, even for moderate wind speeds. However, if the flow is directed parallel to the border between the differentially-heated patches, the SC and thus its impact on entrainment persists. eng
dc.description.sponsorship DFG/RA 617/21-1
dc.description.sponsorship DFG/RA 617/20-1
dc.description.sponsorship Niedersächsische Technische Hochschule (NTH)
dc.language.iso eng
dc.publisher Berlin : Kluwer Academic Publishers
dc.relation.ispartofseries Boundary-Layer Meteorology 151 (2014)
dc.rights CC BY 3.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/3.0/
dc.subject Encroachment eng
dc.subject Entrainment eng
dc.subject Surface heterogeneity eng
dc.subject Boundary layer flow eng
dc.subject Boundary layers eng
dc.subject Heat flux eng
dc.subject Large eddy simulation eng
dc.subject Surface properties eng
dc.subject Convective boundary layers eng
dc.subject Horizontal advection eng
dc.subject Secondary circulation eng
dc.subject Sensible heat flux eng
dc.subject Surface heterogeneities eng
dc.subject Temporal evolution eng
dc.subject Thermal convections eng
dc.subject Air entrainment eng
dc.subject atmospheric circulation eng
dc.subject heterogeneity eng
dc.subject large eddy simulation eng
dc.subject mixed layer eng
dc.subject mixing eng
dc.subject sensible heat flux eng
dc.subject temporal evolution eng
dc.subject thermal convection eng
dc.subject wind velocity eng
dc.subject.ddc 500 | Naturwissenschaften ger
dc.title On the Effect of Surface Heat-Flux Heterogeneities on the Mixed-Layer-Top Entrainment
dc.type Article
dc.type Text
dc.relation.issn 00068314
dc.relation.doi https://doi.org/10.1007/s10546-014-9913-7
dc.bibliographicCitation.issue 3
dc.bibliographicCitation.volume 151
dc.bibliographicCitation.firstPage 531
dc.bibliographicCitation.lastPage 556
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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