Derivation of Structure Parameters of Temperature and Humidity in the Convective Boundary Layer from Large-Eddy Simulations and Implications for the Interpretation of Scintillometer Observations

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dc.identifier.uri http://dx.doi.org/10.15488/1739
dc.identifier.uri http://www.repo.uni-hannover.de/handle/123456789/1764
dc.contributor.author Maronga, Björn
dc.contributor.author Moene, Arnold F.
dc.contributor.author van Dinther, Danielle
dc.contributor.author Raasch, Siegfried
dc.contributor.author Bosveld, Fred C.
dc.contributor.author Gioli, Beniamino
dc.date.accessioned 2017-07-19T07:41:49Z
dc.date.available 2017-07-19T07:41:49Z
dc.date.issued 2013
dc.identifier.citation Maronga, B.; Moene, A.F.; van Dinther, D.; Raasch, S.; Bosveld, F.C. et al.: Derivation of Structure Parameters of Temperature and Humidity in the Convective Boundary Layer from Large-Eddy Simulations and Implications for the Interpretation of Scintillometer Observations. In: Boundary-Layer Meteorology 148 (2013), Nr. 1, S. 1-30. DOI: https://doi.org/10.1007/s10546-013-9801-6
dc.description.abstract We derive the turbulent structure parameters of temperature CT 2 and humidity Cq 2 from high-resolution large-eddy simulations (LES) of a homogeneously-heated convective boundary layer. Boundary conditions and model forcing were derived from measurements at Cabauw in The Netherlands. Three different methods to obtain the structure-parameters from LES are investigated. The shape of the vertical structure-parameter profiles from all three methods compare well with former experimental and LES results. Depending on the method, deviations in the magnitude up to a factor of two are found and traced back to the effects of discretization and numerical dissipation of the advection scheme. Furthermore, we validate the LES data with airborne and large-aperture scintillometer (LAS) measurements at Cabauw. Virtual path measurements are used to study the variability of CT 2 in the mixed layer and surface layer and its implications for airborne and LAS measurements. A high variability of CT 2 along a given horizontal path in the LES data is associated with plumes (high values) and downdrafts (low values). The path average of CT 2 varies rapidly in time due to the limited path length. The LES results suggest that measured path averages require sufficient temporal averaging and an adequate ratio of path length to height above the ground for the LAS in order to approach the domain average of CT 2. eng
dc.description.sponsorship DFG/RA 617/20-1
dc.language.iso eng
dc.publisher Heidelberg : Springer Verlag
dc.relation.ispartofseries Boundary-Layer Meteorology 148 (2013), Nr. 1
dc.rights CC BY 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/4.0/
dc.subject A1. largeeddy simulations (LES) eng
dc.subject Convective boundary layers eng
dc.subject Numerical dissipation eng
dc.subject Structure parameter eng
dc.subject Temperature and humidities eng
dc.subject Temporal averaging eng
dc.subject Turbulent structures eng
dc.subject Virtual scintillometer eng
dc.subject Scintillation eng
dc.subject Large eddy simulation eng
dc.subject advection eng
dc.subject air temperature eng
dc.subject atmospheric structure eng
dc.subject boundary condition eng
dc.subject convective boundary layer eng
dc.subject humidity eng
dc.subject large eddy simulation eng
dc.subject Cabauw eng
dc.subject Netherlands eng
dc.subject Utrecht [Netherlands] eng
dc.subject.ddc 550 | Geowissenschaften ger
dc.title Derivation of Structure Parameters of Temperature and Humidity in the Convective Boundary Layer from Large-Eddy Simulations and Implications for the Interpretation of Scintillometer Observations eng
dc.type Article
dc.type Text
dc.relation.issn 0006-8314
dc.relation.doi https://doi.org/10.1007/s10546-013-9801-6
dc.bibliographicCitation.issue 1
dc.bibliographicCitation.volume 148
dc.bibliographicCitation.firstPage 1
dc.bibliographicCitation.lastPage 30
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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