DC FieldValueLanguage
dc.contributor.authorStevens, Bjorn-
dc.contributor.authorSatoh, Masaki-
dc.contributor.authorAuger, Ludovic-
dc.contributor.authorBiercamp, Joachim-
dc.contributor.authorBretherton, Christopher S.-
dc.contributor.authorChen, Xi-
dc.contributor.authorDüben, Peter-
dc.contributor.authorJudt, Falko-
dc.contributor.authorKhairoutdinov, Marat-
dc.contributor.authorKlocke, Daniel-
dc.contributor.authorKodama, Chihiro-
dc.contributor.authorKornblueh, Luis-
dc.contributor.authorLin, Shian Jiann-
dc.contributor.authorNeumann, Philipp-
dc.contributor.authorPutman, William M.-
dc.contributor.authorRöber, Niklas-
dc.contributor.authorShibuya, Ryosuke-
dc.contributor.authorVanniere, Benoit-
dc.contributor.authorVidale, Pier Luigi-
dc.contributor.authorWedi, Nils-
dc.contributor.authorZhou, Linjiong-
dc.date.accessioned2022-03-30T14:11:26Z-
dc.date.available2022-03-30T14:11:26Z-
dc.date.issued2019-
dc.identifier.issn2197-4284-
dc.description.abstractA 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.].de_DE
dc.description.sponsorshipGerman Climate Computing Center, DKRZde_DE
dc.language.isoende_DE
dc.relation.ispartofProgress in Earth and Planetary Sciencede_DE
dc.subject.ddcDDC::000 Informatik, Informationswissenschaft, allgemeine Werkede_DE
dc.subject.ddcDDC::500 Naturwissenschaften und Mathematikde_DE
dc.titleDYAMOND: the DYnamics of the Atmospheric general circulation Modeled On Non-hydrostatic Domainsde_DE
dc.typeArticlede_DE
dc.identifier.doi10.1186/s40645-019-0304-z-
dc.identifier.scopus2-s2.0-85066070118-
dcterms.bibliographicCitation.articlenumber61de_DE
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/85066070118-
local.submission.typeonly-metadatade_DE
dc.identifier.eissn21974284-
dc.description.peerReviewedYesde_DE
dc.type.articleScientific Articlede_DE
item.fulltext_sNo Fulltext-
item.openairetypeArticle-
item.grantfulltextnone-
item.languageiso639-1en-
item.fulltextNo Fulltext-
crisitem.author.deptHigh Performance Computing-
crisitem.author.parentorgFakultät für Maschinenbau und Bauingenieurwesen-
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