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  5. DYAMOND: the DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domains
 
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DYAMOND: the DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domains

Publication date
2019
Document type
Research article
Author
Stevens, Bjorn
Satoh, Masaki
Auger, Ludovic
Biercamp, Joachim
Bretherton, Christopher S.
Chen, Xi
Düben, Peter
Judt, Falko
Khairoutdinov, Marat
Klocke, Daniel
Kodama, Chihiro
Kornblueh, Luis
Lin, Shian Jiann
Neumann, Philipp 
Putman, William M.
Röber, Niklas
Shibuya, Ryosuke
Vanniere, Benoit
Vidale, Pier Luigi
Wedi, Nils
Zhou, Linjiong
Organisational unit
German Climate Computing Center, DKRZ
DOI
10.1186/s40645-019-0304-z
URI
https://openhsu.ub.hsu-hh.de/handle/10.24405/14223
Scopus ID
2-s2.0-85066070118
Series or journal
Progress in Earth and Planetary Science
ISSN
2197-4284
2197-4284
Peer-reviewed
✅
Part of the university bibliography
Nein
  • Additional Information
Language
English
Abstract
A review of the experimental protocol and motivation for DYAMOND, the first intercomparison project of global storm-resolving models, is presented. Nine models submitted simulation output for a 40-day (1 August–10 September 2016) intercomparison period. Eight of these employed a tiling of the sphere that was uniformly less than 5 km. By resolving the transient dynamics of convective storms in the tropics, global storm-resolving models remove the need to parameterize tropical deep convection, providing a fundamentally more sound representation of the climate system and a more natural link to commensurately high-resolution data from satellite-borne sensors. The models and some basic characteristics of their output are described in more detail, as is the availability and planned use of this output for future scientific study. Tropically and zonally averaged energy budgets, precipitable water distributions, and precipitation from the model ensemble are evaluated, as is their representation of tropical cyclones and the predictability of column water vapor, the latter being important for tropical weather. [Figure not available: see fulltext.].
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