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Abstract
The decorrelation length (Lcf) has been widely used to describe the behavior of vertical overlap of clouds in gene-ral circulation models (GCMs); however, it has been a challenge to associate Lcf with the large-scale meteorological conditions during cloud evolution. This study explored the relationship between Lcf and the strength of atmospheric convection in the tropics based on output from a global cloud-resolving model. Lcf tends to increase with vertical velocity in the mid-troposphere (w500) at locations of ascent, but shows little or no dependency on w500 at locations of descent. A representation of Lcf as a function of vertical velocity is obtained, with a linear regression in ascending regions and a constant value in descending regions. This simple and dynamic-related representation of Lcf leads to a significant improvement in simulation of both cloud cover and radiation fields compared with traditional overlap treatments. This work presents a physically justifiable approach to depicting cloud overlap in the tropics in GCMs.
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Citation
Jing, X. W., H. Zhang, M. Satoh, et al., 2018: Improving representation of tropical cloud overlap in GCMs based on cloud-resolving model data. J. Meteor. Res., 32(2), 233–245, doi: 10.1007/s13351-018-7095-9..
Jing, X. W., H. Zhang, M. Satoh, et al., 2018: Improving representation of tropical cloud overlap in GCMs based on cloud-resolving model data. J. Meteor. Res., 32(2), 233–245, doi: 10.1007/s13351-018-7095-9..
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Jing, X. W., H. Zhang, M. Satoh, et al., 2018: Improving representation of tropical cloud overlap in GCMs based on cloud-resolving model data. J. Meteor. Res., 32(2), 233–245, doi: 10.1007/s13351-018-7095-9..
Jing, X. W., H. Zhang, M. Satoh, et al., 2018: Improving representation of tropical cloud overlap in GCMs based on cloud-resolving model data. J. Meteor. Res., 32(2), 233–245, doi: 10.1007/s13351-018-7095-9..
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