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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/46L4642
Repositóriosid.inpe.br/mtc-m21d/2022/04.04.13.48   (acesso restrito)
Última Atualização2022:04.04.13.48.16 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21d/2022/04.04.13.48.16
Última Atualização dos Metadados2023:01.03.16.46.03 (UTC) administrator
DOI10.1002/qj.4222
ISSN0035-9009
Chave de CitaçãoTangXGHKKKKKLPVWYDHJMNPRSTBMNZ:2022:LoSiMo
TítuloLong-term single-column model intercomparison of diurnal cycle of precipitation over midlatitude and tropical land
Ano2022
MêsJan.
Data de Acesso18 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho7672 KiB
2. Contextualização
Autor 1 Tang, Shuaiqi
 2 Xie, Shaocheng
 3 Guo, Zhun
 4 Hong, Song-You
 5 Khouider, Boualem
 6 Klocke, Daniel
 7 Köhler, Martin
 8 Koo, Myung-Seo
 9 Krishna, Phani Murali
10 Larson, Vincent E.
11 Park, Sungsu
12 Vaillancourt, Paul A.
13 Wang, Yi-Chi
14 Yang, Jing
15 Daleu, Chimene L.
16 Homeyer, Cameron R.
17 Jones, Todd R.
18 Malap, Neelam
19 Neggers, Roel
20 Prabhakaran, Thara
21 Ramirez Gutierrez, Enver Manuel Amador
22 Schumacher, Courtney
23 Tao, Cheng
24 Bechtold, Peter
25 Ma, Hsi-Yen
26 Neelin, J. David
27 Zeng, Xubin
ORCID 1 0000-0002-8946-9205
 2 0000-0001-8931-5145
Grupo 1
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21 DIMNT-CGCT-INPE-MCTI-GOV-BR
Afiliação 1 Pacific Northwest National Laboratory
 2 Lawrence Livermore National Laboratory
 3 Chinese Academy of Sciences
 4 University of Colorado
 5 University of Victoria
 6 Hans Ertel Centre for Weather Research
 7 Deutscher Wetterdienst
 8 Korea Institute of Atmospheric Prediction Systems
 9 Indian Institute of Tropical Meteorology
10 Pacific Northwest National Laboratory
11 Seoul National University
12 Environment and Climate Change Canada
13 Research Center for Environmental Changes
14 Climate Change Canada
15 University of Reading
16 University of Oklahoma
17 University of Reading
18 Indian Institute of Tropical Meteorology
19 University of Cologne
20 Indian Institute of Tropical Meteorology
21 Instituto Nacional de Pesquisas Espaciais (INPE)
22 Texas A&M University
23 Lawrence Livermore National Laboratory
24 European Centre for Medium-Range Weather Forecasts
25 Lawrence Livermore National Laboratory
26 University of California in Los Angeles
27 University of Arizona
Endereço de e-Mail do Autor 1
 2 xie2@llnl.gov
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21 enver.ramirez@gmail.com
RevistaQuarterly Journal of the Royal Meteorological Society
Volume148
Número743
Páginas641-669
Nota SecundáriaA1_GEOCIÊNCIAS A2_ENGENHARIAS_I
Histórico (UTC)2022-04-04 13:48:16 :: simone -> administrator ::
2022-04-04 13:48:17 :: administrator -> simone :: 2022
2022-04-04 13:53:33 :: simone -> administrator :: 2022
2023-01-03 16:46:03 :: administrator -> simone :: 2022
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chave3. Physical phenomenon
convection
diurnal cycle of precipitation
single-column model
ResumoGeneral Circulation Models (GCMs) have for decades exhibited difficulties in modelling the diurnal cycle of precipitation (DCP). This issue can be related to inappropriate representation of the processes controlling sub-diurnal phenomena like convection. In this study, 11 single-column versions of GCMs are used to investigate the interactions between convection and environmental conditions, processes that control nocturnal convections, and the transition from shallow to deep convection on a diurnal time-scale. Long-term simulations are performed over two continental land sites: the Southern Great Plains (SGP) in the USA for 12 summer months from 2004 to 2015 and the Manacapuru site at the central Amazon (MAO) in Brazil for two full years from 2014 to 2015. The analysis is done on two regimes: afternoon convective regime and nocturnal precipitation regime. Most models produce afternoon precipitation too early, likely due to the missing transition of shallow-to-deep convection in these models. At SGP, the unified convection schemes better simulate the onset time of precipitation. At MAO, models produce the heating peak in a much lower level compared with observation, indicating too shallow convection in the models. For nocturnal precipitation, models that produce most of nocturnal precipitation all allow convection to be triggered above the boundary layer. This indicates the importance of model capability to detect elevated convection for simulating nocturnal precipitation. Sensitivity studies indicate that (a) nudging environmental variables towards observations has a minor impact on DCP, (b) unified treatment of shallow and deep convection and the capability to capture mid-level convection can help models better capture DCP, and (c) the interactions of the atmosphere with other components in the climate system (e.g. land) are also important for DCP simulations in coupled models. These results provide long-term statistical insights on which physical processes are essential in climate models to simulate DCP.
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4. Condições de acesso e uso
Idiomaen
Arquivo AlvoQuart J Royal Meteoro Soc - 2021 - Tang - Long‐term single‐column model intercomparison of diurnal cycle of precipitation.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/46KUATE
DivulgaçãoWEBSCI
Acervo Hospedeirourlib.net/www/2021/06.04.03.40
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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