Original paper

Finite-volume models with implicit subgrid-scale parameterization for the differentially heated rotating annulus

Borchert, Sebastian; Achatz, Ulrich; Remmler, Sebastian; Hickel, Stefan; Harlander, Uwe; Vincze, Miklos; Alexandrov, Kiril D.; Rieper, Felix; Heppelmann, Tobias; Dolaptchiev, Stamen I.

Meteorologische Zeitschrift Vol. 23 No. 6 (2015), p. 561 - 580

54 references

published: Jan 13, 2015
published online: Dec 10, 2014
manuscript accepted: Sep 16, 2014
manuscript revision received: Jun 26, 2014
manuscript revision requested: Jun 26, 2014
manuscript received: Nov 11, 2013

DOI: 10.1127/metz/2014/0548

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The differentially heated rotating annulus is a classical experiment for the investigation of baroclinic flows and can be regarded as a strongly simplified laboratory model of the atmosphere in mid-latitudes. Data of this experiment, measured at the BTU Cottbus-Senftenberg, are used to validate two numerical finite-volume models (INCA and cylFloit) which differ basically in their grid structure. Both models employ an implicit parameterization of the subgrid-scale turbulence by the Adaptive Local Deconvolution Method (ALDM). One part of the laboratory procedure, which is commonly neglected in simulations, is the annulus spin-up. During this phase the annulus is accelerated from a state of rest to a desired angular velocity. We use a simple modelling approach of the spin-up to investigate whether it increases the agreement between experiment and simulation. The model validation compares the azimuthal mode numbers of the baroclinic waves and does a principal component analysis of time series of the temperature field. The Eady model of baroclinic instability provides a guideline for the qualitative understanding of the observations.


differentially heated rotating annulusfinite-volume modelsimplicit subgrid-scale parameterizationbaroclinic wavesprincipal component analysis