Articles | Volume 16, issue 6
https://doi.org/10.5194/acp-16-3881-2016
https://doi.org/10.5194/acp-16-3881-2016
Research article
 | 
23 Mar 2016
Research article |  | 23 Mar 2016

A modelling case study of a large-scale cirrus in the tropical tropopause layer

Aurélien Podglajen, Riwal Plougonven, Albert Hertzog, and Bernard Legras

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Cited articles

Bucholtz, A., Hlavka, D. L., McGill, M. J., Schmidt, K. S., Pilewskie, P., Davis, S. M., Reid, E. A., and Walker, A. L.: Directly measured heating rates of a tropical subvisible cirrus cloud, J. Geophys. Res., 115, D00J09, https://doi.org/10.1029/2009JD013128, 2010.
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Corti, T., Luo, B. P., Peter, T., Vömel, H., and Fu, Q.: Mean radiative energy balance and vertical mass fluxes in the equatorial upper troposphere and lower stratosphere, Geophys. Res. Lett., 32, L06802, https://doi.org/10.1029/2004GL021889, 2005.
Corti, T., Luo, B. P., Fu, Q., Vömel, H., and Peter, T.: The impact of cirrus clouds on tropical troposphere-to-stratosphere transport, Atmos. Chem. Phys., 6, 2539–2547, https://doi.org/10.5194/acp-6-2539-2006, 2006.
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Short summary
The Weather Research and Forecast model is used to simulate a large-scale tropical tropopause layer (TTL) cirrus. Validated with satellite observations, the simulation shows that several clouds successively form due to a large-scale uplift initiated by the intrusion of air from the midlatitudes. The simulated cloud field is found as sensitive to the initial condition as it is to the choice of the microphysics parametrisation. The cloud impacts on the radiative and water budgets are estimated.
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