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Vertical grid spacing necessary for simulating tropical cirrus clouds with a high‐resolution atmospheric general circulation model
Author(s) -
Seiki Tatsuya,
Kodama Chihiro,
Satoh Masaki,
Hashino Tempei,
Hagihara Yuichiro,
Okamoto Hajime
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2015gl064282
Subject(s) - cirrus , environmental science , lidar , atmospheric sciences , atmospheric model , satellite , cloud fraction , longwave , liquid water content , cloud height , optical depth , cloud physics , ice cloud , meteorology , remote sensing , geology , aerosol , cloud cover , radiative transfer , cloud computing , physics , optics , astronomy , computer science , operating system
The distribution of simulated cirrus clouds over the tropics is affected by the particular model's vertical grid spacing. To examine this effect, we use a high‐resolution atmospheric general circulation model with 28 km and 14 km horizontal meshes. We show that a vertical grid spacing of 400 m or less is necessary to resolve the bulk structure of cirrus clouds. As one reduces the vertical grid spacing below about 1000 m, the visible cirrus cloud fraction decreases, the cloud thins (optically and geometrically), the cloud top height lowers, and consequently, the outgoing longwave radiation increases. These effects are stronger over the tropics. When using a vertical grid spacing of 400 m or less, the vertical profiles of effective radii and ice water content converge toward measurements (CloudSat satellite and Cloud‐Aerosol Lidar and Infrared Pathfinder Satellite Observation).