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Title: How Well Can We Represent the Spectrum of Convective Clouds in a Climate Model? Comparisons between Internal Parameterization Variables and Radar Observations

Authors:
 [1] ;  [1] ;  [1] ;  [2]
  1. Department of Physics, University of Oxford, Oxford, United Kingdom
  2. Bureau of Meteorology, Melbourne, Victoria, Australia
Publication Date:
Grant/Contract Number:
FG02-03ER63533; FG02-08ER64527
Type:
Published Article
Journal Name:
Journal of the Atmospheric Sciences
Additional Journal Information:
Journal Name: Journal of the Atmospheric Sciences Journal Volume: 75 Journal Issue: 5; Journal ID: ISSN 0022-4928
Publisher:
American Meteorological Society
Sponsoring Org:
USDOE
Country of Publication:
United States
Language:
English
OSTI Identifier:
1435391

Labbouz, Laurent, Kipling, Zak, Stier, Philip, and Protat, Alain. How Well Can We Represent the Spectrum of Convective Clouds in a Climate Model? Comparisons between Internal Parameterization Variables and Radar Observations. United States: N. p., Web. doi:10.1175/JAS-D-17-0191.1.
Labbouz, Laurent, Kipling, Zak, Stier, Philip, & Protat, Alain. How Well Can We Represent the Spectrum of Convective Clouds in a Climate Model? Comparisons between Internal Parameterization Variables and Radar Observations. United States. doi:10.1175/JAS-D-17-0191.1.
Labbouz, Laurent, Kipling, Zak, Stier, Philip, and Protat, Alain. 2018. "How Well Can We Represent the Spectrum of Convective Clouds in a Climate Model? Comparisons between Internal Parameterization Variables and Radar Observations". United States. doi:10.1175/JAS-D-17-0191.1.
@article{osti_1435391,
title = {How Well Can We Represent the Spectrum of Convective Clouds in a Climate Model? Comparisons between Internal Parameterization Variables and Radar Observations},
author = {Labbouz, Laurent and Kipling, Zak and Stier, Philip and Protat, Alain},
abstractNote = {},
doi = {10.1175/JAS-D-17-0191.1},
journal = {Journal of the Atmospheric Sciences},
number = 5,
volume = 75,
place = {United States},
year = {2018},
month = {5}
}