A refined statistical cloud closure using double-Gaussian probability density functions

We introduce a probability density function (PDF)-based scheme to parameterize cloud fraction, average liquid water and liquid water flux in large-scale models, that is developed from and tested against large-eddy simulations and observational data. Because the tails of the PDFs are crucial for an a...

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Main Authors: A. K. Naumann, A. Seifert, J. P. Mellado
Format: Article
Language:English
Published: Copernicus Publications 2013-10-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/6/1641/2013/gmd-6-1641-2013.pdf
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spelling doaj-c901eb210d4e460e9299540ea0e40caf2020-11-24T22:14:27ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032013-10-01651641165710.5194/gmd-6-1641-2013A refined statistical cloud closure using double-Gaussian probability density functionsA. K. NaumannA. SeifertJ. P. MelladoWe introduce a probability density function (PDF)-based scheme to parameterize cloud fraction, average liquid water and liquid water flux in large-scale models, that is developed from and tested against large-eddy simulations and observational data. Because the tails of the PDFs are crucial for an appropriate parameterization of cloud properties, we use a double-Gaussian distribution that is able to represent the observed, skewed PDFs properly. Introducing two closure equations, the resulting parameterization relies on the first three moments of the subgrid variability of temperature and moisture as input parameters. The parameterization is found to be superior to a single-Gaussian approach in diagnosing the cloud fraction and average liquid water profiles. A priori testing also suggests improved accuracy compared to existing double-Gaussian closures. Furthermore, we find that the error of the new parameterization is smallest for a horizontal resolution of about 5–20 km and also depends on the appearance of mesoscale structures that are accompanied by higher rain rates. In combination with simple autoconversion schemes that only depend on the liquid water, the error introduced by the new parameterization is orders of magnitude smaller than the difference between various autoconversion schemes. For the liquid water flux, we introduce a parameterization that is depending on the skewness of the subgrid variability of temperature and moisture and that reproduces the profiles of the liquid water flux well.http://www.geosci-model-dev.net/6/1641/2013/gmd-6-1641-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. K. Naumann
A. Seifert
J. P. Mellado
spellingShingle A. K. Naumann
A. Seifert
J. P. Mellado
A refined statistical cloud closure using double-Gaussian probability density functions
Geoscientific Model Development
author_facet A. K. Naumann
A. Seifert
J. P. Mellado
author_sort A. K. Naumann
title A refined statistical cloud closure using double-Gaussian probability density functions
title_short A refined statistical cloud closure using double-Gaussian probability density functions
title_full A refined statistical cloud closure using double-Gaussian probability density functions
title_fullStr A refined statistical cloud closure using double-Gaussian probability density functions
title_full_unstemmed A refined statistical cloud closure using double-Gaussian probability density functions
title_sort refined statistical cloud closure using double-gaussian probability density functions
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2013-10-01
description We introduce a probability density function (PDF)-based scheme to parameterize cloud fraction, average liquid water and liquid water flux in large-scale models, that is developed from and tested against large-eddy simulations and observational data. Because the tails of the PDFs are crucial for an appropriate parameterization of cloud properties, we use a double-Gaussian distribution that is able to represent the observed, skewed PDFs properly. Introducing two closure equations, the resulting parameterization relies on the first three moments of the subgrid variability of temperature and moisture as input parameters. The parameterization is found to be superior to a single-Gaussian approach in diagnosing the cloud fraction and average liquid water profiles. A priori testing also suggests improved accuracy compared to existing double-Gaussian closures. Furthermore, we find that the error of the new parameterization is smallest for a horizontal resolution of about 5–20 km and also depends on the appearance of mesoscale structures that are accompanied by higher rain rates. In combination with simple autoconversion schemes that only depend on the liquid water, the error introduced by the new parameterization is orders of magnitude smaller than the difference between various autoconversion schemes. For the liquid water flux, we introduce a parameterization that is depending on the skewness of the subgrid variability of temperature and moisture and that reproduces the profiles of the liquid water flux well.
url http://www.geosci-model-dev.net/6/1641/2013/gmd-6-1641-2013.pdf
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