Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus

The behavior of the ECHAM4 cloud and turbulence scheme is evaluated for an idealized case of Stratocumulus. It is shown that the E-l turbulence closure that is used is sensitive to instabilities. This is caused by the formulation of the turbulent length scale / in terms of the moist Richardson numbe...

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Main Authors: Geert Lenderink, van Meijgaard, Albert A.M. Holtslag
Format: Article
Language:English
Published: Borntraeger 2000-04-01
Series:Meteorologische Zeitschrift
Subjects:
Online Access:http://dx.doi.org/10.1127/metz/9/2000/41
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author Geert Lenderink
van Meijgaard
Albert A.M. Holtslag
author_facet Geert Lenderink
van Meijgaard
Albert A.M. Holtslag
author_sort Geert Lenderink
collection DOAJ
description The behavior of the ECHAM4 cloud and turbulence scheme is evaluated for an idealized case of Stratocumulus. It is shown that the E-l turbulence closure that is used is sensitive to instabilities. This is caused by the formulation of the turbulent length scale / in terms of the moist Richardson number, which gives unrealistic results in the case of low wind shear. It is further shown that the ECHAM4 condensation scheme is highly dependent on both spatial and temporal resolution. It is only in the limit of high vertical resolution (25 meters) and of small time steps (1 second) that the scheme is able to sustain a cloud cover of more than 90 %. At operational resolution the cloud cover decreases to typically 60-70 %. A modified version of the condensation scheme is presented which does not display this strong dependency on the resolution. A three dimensional simulation with this scheme for a low level Stratocumulus cloud deck shows a significant improvement compared to the standard ECHAM4 scheme.
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spelling doaj.art-3b3b2f4167044efdae6c34d20da97c952024-02-08T08:28:14ZengBorntraegerMeteorologische Zeitschrift0941-29482000-04-0191414710.1127/metz/9/2000/4188653Evaluation of the ECHAM4 cloud-turbulence scheme for StratocumulusGeert Lenderinkvan MeijgaardAlbert A.M. HoltslagThe behavior of the ECHAM4 cloud and turbulence scheme is evaluated for an idealized case of Stratocumulus. It is shown that the E-l turbulence closure that is used is sensitive to instabilities. This is caused by the formulation of the turbulent length scale / in terms of the moist Richardson number, which gives unrealistic results in the case of low wind shear. It is further shown that the ECHAM4 condensation scheme is highly dependent on both spatial and temporal resolution. It is only in the limit of high vertical resolution (25 meters) and of small time steps (1 second) that the scheme is able to sustain a cloud cover of more than 90 %. At operational resolution the cloud cover decreases to typically 60-70 %. A modified version of the condensation scheme is presented which does not display this strong dependency on the resolution. A three dimensional simulation with this scheme for a low level Stratocumulus cloud deck shows a significant improvement compared to the standard ECHAM4 scheme.http://dx.doi.org/10.1127/metz/9/2000/41cloud and turbulence schemestratocumuluswolken- und turbulenzschema
spellingShingle Geert Lenderink
van Meijgaard
Albert A.M. Holtslag
Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus
Meteorologische Zeitschrift
cloud and turbulence scheme
stratocumulus
wolken- und turbulenzschema
title Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus
title_full Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus
title_fullStr Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus
title_full_unstemmed Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus
title_short Evaluation of the ECHAM4 cloud-turbulence scheme for Stratocumulus
title_sort evaluation of the echam4 cloud turbulence scheme for stratocumulus
topic cloud and turbulence scheme
stratocumulus
wolken- und turbulenzschema
url http://dx.doi.org/10.1127/metz/9/2000/41
work_keys_str_mv AT geertlenderink evaluationoftheecham4cloudturbulenceschemeforstratocumulus
AT vanmeijgaard evaluationoftheecham4cloudturbulenceschemeforstratocumulus
AT albertamholtslag evaluationoftheecham4cloudturbulenceschemeforstratocumulus