Inter-model Variability in Convection-Resolving Simulations of Subtropical Marine Low Clouds
Author:
Affiliation:
1. Institute for Atmospheric and Climate Science, ETH Zürich, Switzerland
2. Department of Atmospheric and Cryospheric Sciences, Universität Innsbruck, Austria
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj/99/5/99_2021-062/_pdf
Reference83 articles.
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2. Arnold, N. P., W. M. Putman, and S. R. Freitas, 2020: Impact of resolution and parameterized convection on the diurnal cycle of precipitation in a global non-hydrostatic model. J. Meteor. Soc. Japan, 98, 1279-1304.
3. Baldauf, M., and G. Zängl, 2012: Horizontal nonlinear Smagorinsky diffusion. COSMO Newsl., 2, 3-7.
4. Ban, N., J. Schmidli, and C. Schär, 2014: Evaluation of the convection-resolving regional climate modeling approach in decade-long simulations. J. Geophys. Res.: Atmos., 119, 7889-7907.
5. Bony, S., and J.-L. Dufresne, 2005: Marine boundary layer clouds at the heart of tropical cloud feedback uncertainties in climate models. Geophys. Res. Lett., 32, L20806, doi:10.1029/2005GL023851.
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