R
Richard Neale
Researcher at National Center for Atmospheric Research
Publications - 67
Citations - 14978
Richard Neale is an academic researcher from National Center for Atmospheric Research. The author has contributed to research in topics: Climate model & Madden–Julian oscillation. The author has an hindex of 36, co-authored 67 publications receiving 11502 citations. Previous affiliations of Richard Neale include University of Reading.
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The role of convective gustiness in reducing seasonal precipitation biases in the Tropical West Pacific
TL;DR: In this paper, a Normalized Gross Moist Stability (NGMS) framework is used to explore the processes responsible for the precipitation bias, and the impact of the gustiness parameterization in reducing that bias.
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Simulation of the intraseasonal variability over the Eastern Pacific ITCZ in climate models
Xianan Jiang,Xianan Jiang,Duane E. Waliser,Daehyun Kim,Ming Zhao,Kenneth R. Sperber,W. Stern,Siegfried D. Schubert,Guang J. Zhang,Wanqiu Wang,Marat Khairoutdinov,Richard Neale,Myong-In Lee +12 more
TL;DR: In this paper, the model fidelity in representing these two dominant ISV modes over the EPAC is assessed by analyzing six atmospheric and three coupled general circulation models (GCMs), including one superparameterized GCM (SPCAM) and one recently developed high-resolution GCM with horizontal resolution of about 50 km.
Posted ContentDOI
A new ensemble-based consistency test for the Community Earth System Model
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Deep Convective Transition Characteristics in the Community Climate System Model and Changes under Global Warming
TL;DR: In this article, the authors analyzed tropical deep convective transition characteristics using uncoupled and coupled versions of the Community Climate System Model (CCSM) under present-day and global warming conditions.
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Evolution of the Double‐ITCZ Bias Through CESM2 Development
TL;DR: The Community Earth System Model version 2 (CESM2) is greatly improved as compared to its previous version, CESM version 1 as discussed by the authors, which is attributed to increases in low cloud cover and the associated shortwave cloud forcing over the southeast.