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dc.contributor.authorCollier, Emily
dc.contributor.authorBan, Nikolina
dc.contributor.authorRichter, Niklas
dc.contributor.authorAhrens, Bodo
dc.contributor.authorChen, Deliang
dc.contributor.authorChen, Xingchao
dc.contributor.authorLai, Hui-Wen
dc.contributor.authorLeung, Ruby
dc.contributor.authorLi, Lu
dc.contributor.authorMedvedova, Alzbeta
dc.contributor.authorOu, Tinghai
dc.contributor.authorPothapakula, Praveen Kumar
dc.contributor.authorPotter, Emily
dc.contributor.authorPrein, Andreas F.
dc.contributor.authorSakaguchi, Koichi
dc.contributor.authorSchroeder, Marie
dc.contributor.authorSingh, Prashant
dc.contributor.authorSobolowski, Stefan Pieter
dc.contributor.authorSugimoto, Shiori
dc.contributor.authorTang, Jianping
dc.contributor.authorYu, Hongyong
dc.contributor.authorZiska, Catharina
dc.date.accessioned2024-07-03T14:17:54Z
dc.date.available2024-07-03T14:17:54Z
dc.date.created2024-06-18T14:48:35Z
dc.date.issued2024
dc.identifier.citationClimate Dynamics. 2024, .en_US
dc.identifier.issn0930-7575
dc.identifier.urihttps://hdl.handle.net/11250/3137740
dc.description.abstractAn accurate understanding of the current and future water cycle over the Third Pole is of great societal importance, given the role this region plays as a water tower for densely populated areas downstream. An emerging and promising approach for skillful climate assessments over regions of complex terrain is kilometer-scale climate modeling. As a foundational step towards such simulations over the Third Pole, we present a multi-model and multi-physics ensemble of kilometer-scale regional simulations for the hydrological year of October 2019 to September 2020. The ensemble consists of 13 simulations performed by an international consortium of 10 research groups, configured with a horizontal grid spacing ranging from 2.2 to 4 km covering all of the Third Pole region. These simulations are driven by ERA5 and are part of a Coordinated Regional Climate Downscaling EXperiment Flagship Pilot Study on Convection-Permitting Third Pole. The simulations are compared against available gridded and in-situ observations and remote-sensing data, to assess the performance and spread of the model ensemble compared to the driving reanalysis during the cold and warm seasons. Although ensemble evaluation is hindered by large differences between the gridded precipitation datasets used as a reference over this region, we show that the ensemble improves on many warm-season precipitation metrics compared with ERA5, including most wet-day and hour statistics, and also adds value in the representation of wet spells in both seasons. As such, the ensemble will provide an invaluable resource for future improvements in the process understanding of the hydroclimate of this remote but important region.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleThe first ensemble of kilometer-scale simulations of a hydrological year over the third poleen_US
dc.title.alternativeThe first ensemble of kilometer-scale simulations of a hydrological year over the third poleen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.rights.holder© The Author(s) 2024en_US
dc.description.versionpublishedVersionen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1007/s00382-024-07291-2
dc.identifier.cristin2277209
dc.source.journalClimate Dynamicsen_US
dc.source.pagenumber0en_US


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal