dc.contributor.author
Kostelecky, Jonathan
dc.contributor.author
Ansorge, Cedrick
dc.date.accessioned
2024-09-03T12:01:41Z
dc.date.available
2024-09-03T12:01:41Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/44776
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-44487
dc.description.abstract
Roughness of the surface underlying the atmospheric boundary layer causes departures of the near-surface scalar and momentum transport in comparison with aerodynamically smooth surfaces. Here, we investigate the effect of 56×56 homogeneously distributed roughness elements on bulk properties of a turbulent Ekman flow. Direct numerical simulation in combination with an immersed boundary method is performed for fully resolved, three-dimensional roughness elements. The packing density is approximately 10% and the roughness elements have a mean height in wall units of 10≲H+≲40. According to their roughness Reynolds numbers, the cases are transitionally rough, although the roughest case is on the verge of being fully rough. We derive the friction of velocity and of the passive scalar through vertical integration of the respective balances. Thereby, we quantify the enhancement of turbulent activity with increasing roughness height and find a scaling for the friction Reynolds number that is verified up to Reτ≈2700. The higher level of turbulent activity results in a deeper logarithmic layer for the rough cases and an increase of the near-surface wind veer in spite of higher Reτ. We estimate the von Kármán constant for the horizontal velocity κm=0.42 (offset A=5.44) and for the passive scalar κh=0.35 (offset A=4.2). We find an accurate collapse of the data under the rough-wall scaling in the logarithmic layer, which also yields a scaling for the roughness parameters z-nought for momentum (z0m) and the passive scalar (z0h).
en
dc.format.extent
33 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
Geophysical and Geological Flows: Topographic effects
en
dc.subject
Turbulent Flows: Turbulent boundary layers
en
dc.subject
Geophysical and Geological Flows: Meteorology
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::550 Geowissenschaften
dc.title
Simulation and scaling analysis of periodic surfaces with small-scale roughness in turbulent Ekman flow
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
A8
dcterms.bibliographicCitation.doi
10.1017/jfm.2024.542
dcterms.bibliographicCitation.journaltitle
Journal of Fluid Mechanics
dcterms.bibliographicCitation.volume
992
dcterms.bibliographicCitation.url
https://doi.org/10.1017/jfm.2024.542
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Meteorologie

refubium.funding
Cambridge
refubium.note.author
Die Publikation wurde aus Open Access Publikationsgeldern der Freien Universität Berlin gefördert.
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
1469-7645