The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study

Through their multiple interactions with radiation, clouds have an important impact on the climate. Nonetheless, the simulation of clouds in climate models is still coarse. The present evolution of modeling tends to a more realistic representation of the liquid water content; thus the problem of its...

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Main Authors: F. Parol, J. C. Buriez, D. Crétel, Y. Fouquart
Format: Article
Language:English
Published: Copernicus Publications
Series:Annales Geophysicae
Online Access:http://www.ann-geophys.net/12/240/1994/angeo-12-240-1994.html
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spelling doaj-a4f7cdc845dd428d9a890a8b221829bd2020-11-24T21:21:14ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-0576122/3240253The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case studyF. ParolJ. C. BuriezD. CrételY. FouquartThrough their multiple interactions with radiation, clouds have an important impact on the climate. Nonetheless, the simulation of clouds in climate models is still coarse. The present evolution of modeling tends to a more realistic representation of the liquid water content; thus the problem of its subgrid scale distribution is crucial. For a convective cloud field observed during ICE 89, Landsat TM data (resolution: 30m) have been analyzed in order to quantify the respective influences of both the horizontal distribution of liquid water content and cloud shape on the Earth radiation budget. The cloud field was found to be rather well-represented by a stochastic distribution of hemi-ellipsoidal clouds whose horizontal aspect ratio is close to 2 and whose vertical aspect ratio decreases as the cloud cell area increases. For that particular cloud field, neglecting the influence of the cloud shape leads to an over-estimate of the outgoing longwave flux; in the shortwave, it leads to an over-estimate of the reflected flux for high solar elevations but strongly depends on cloud cell orientations for low elevations. On the other hand, neglecting the influence of cloud size distribution leads to systematic over-estimate of their impact on the shortwave radiation whereas the effect is close to zero in the thermal range. The overall effect of the heterogeneities is estimated to be of the order of 10 W m<sup>-2</sup> for the conditions of that Landsat picture (solar zenith angle 65°, cloud cover 70%); it might reach 40 W m<sup>-2</sup> for an overhead sun and overcast cloud conditions. http://www.ann-geophys.net/12/240/1994/angeo-12-240-1994.html
collection DOAJ
language English
format Article
sources DOAJ
author F. Parol
J. C. Buriez
D. Crétel
Y. Fouquart
spellingShingle F. Parol
J. C. Buriez
D. Crétel
Y. Fouquart
The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study
Annales Geophysicae
author_facet F. Parol
J. C. Buriez
D. Crétel
Y. Fouquart
author_sort F. Parol
title The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study
title_short The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study
title_full The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study
title_fullStr The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study
title_full_unstemmed The impact of cloud inhomogeneities on the Earth radiation budget: the 14 October 1989 I.C.E. convective cloud case study
title_sort impact of cloud inhomogeneities on the earth radiation budget: the 14 october 1989 i.c.e. convective cloud case study
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
description Through their multiple interactions with radiation, clouds have an important impact on the climate. Nonetheless, the simulation of clouds in climate models is still coarse. The present evolution of modeling tends to a more realistic representation of the liquid water content; thus the problem of its subgrid scale distribution is crucial. For a convective cloud field observed during ICE 89, Landsat TM data (resolution: 30m) have been analyzed in order to quantify the respective influences of both the horizontal distribution of liquid water content and cloud shape on the Earth radiation budget. The cloud field was found to be rather well-represented by a stochastic distribution of hemi-ellipsoidal clouds whose horizontal aspect ratio is close to 2 and whose vertical aspect ratio decreases as the cloud cell area increases. For that particular cloud field, neglecting the influence of the cloud shape leads to an over-estimate of the outgoing longwave flux; in the shortwave, it leads to an over-estimate of the reflected flux for high solar elevations but strongly depends on cloud cell orientations for low elevations. On the other hand, neglecting the influence of cloud size distribution leads to systematic over-estimate of their impact on the shortwave radiation whereas the effect is close to zero in the thermal range. The overall effect of the heterogeneities is estimated to be of the order of 10 W m<sup>-2</sup> for the conditions of that Landsat picture (solar zenith angle 65°, cloud cover 70%); it might reach 40 W m<sup>-2</sup> for an overhead sun and overcast cloud conditions.
url http://www.ann-geophys.net/12/240/1994/angeo-12-240-1994.html
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