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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/3892P38
Repositóriosid.inpe.br/mtc-m19/2010/09.14.17.16
Última Atualização2010:10.07.17.58.31 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19/2010/09.14.17.16.59
Última Atualização dos Metadados2020:04.28.18.34.19 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoDoyleToma:2010:ExUsNe
TítuloExperiments Using New Initial Soil Moisture Conditions and Soil Map in the Eta Model Over La Plata Basin
Ano2010
Data de Acesso18 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho277 KiB
2. Contextualização
Autor1 Doyle, M E
2 Tomasella, Javier
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHE3
Grupo1
2 CST-CST-INPE-MCT-BR
Afiliação1 CIMA- UBA/CONICET, Buenos Aires, Argentina
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 doyle@cima.fcen.uba.ar
2 javier@cptec.inpe.br
Nome do EventoThe Meeting of the Americas.
Localização do EventoFoz do Iguaçu, BR
Data08-12 aug 2010
Título do LivroProceedings
Tipo TerciárioPapers
Histórico (UTC)2010-10-07 17:58:31 :: valdirene -> administrator :: 2010
2020-04-28 18:34:19 :: administrator -> simone :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveLand/atmosphere interactions
Soil Moisture
atmospheric Eta model
ResumoAB: Strong interactions between soil moisture and the atmospheric processes take place in all spatial and temporal scales. The effects of soil moisture on rainfall can be associated with dynamical modifications of atmospheric systems as well as the generation of mesoscale circulations through the formation of spatial sensible heat flux gradients. A new effort towards a more realistic representation of soil moisture and its impact on the modeling of weather systems is presented. The Eta model is chosen to perform numerical simulations over South America testing the sensitivity of precipitation to soil and soil moisture changes. In this sense, the meteorological situation analyzed is a cold front crossing southeastern South America which is followed by the development of a mesoscale convective complex over northern Argentina in October 2006. The ETA model was configured to run on a 40km grid resolution and 38 vertical levels on a domain which includes all of South America north of 40°S. Initial conditions used to force the Eta Model experiments are taken from the CPTEC global model (Bonatti 1996), as well as the lateral boundary conditions which are updated every 6 hours. The control run (CTRL) uses the NOAH land surface model, with a 4 layer soil model and 9 different types of soil. Three other experiments were performed in order to test the sensibility to modifications of a) initial soil moisture conditions (MOIST), b) a new soil map (MAP) and c) both initial soil mositure conditions and new soil map (M&M). Modified initial soil moisture conditions for the ETA simulations were obtained from a hydrological balance model developed and running operational at CPTEC. The model uses integrated daily precipitation obtained from TRMM product 3B42 version 6 on a 0.25° x 0.25° grid, and rain gauge observed precipitation collected by different institutions in Brazil and by the National Weather Services of Argentina, Uruguay and Paraguay. A new soil map was elaborated using the available soil profile information in the CPTEC/INPE soil data base. It includes information on soil profiles for Brazil, Paraguay, Uruguay and Argentina. Each profile includes basic information such as soil types, texture classes, horizon depths, amount of organic carbon, etc. The different hydrological parameters defining each soil were obtained applying pedotransfer functions. The new soil map includes 16 different soil types. Results indicate that modifying inicial soil moisture conditions and incorporating a new soil map with hydraulic parameters, more representative of South American soils, improves rainfall forecasting both through a better spatial representation of precipitation and a daily total precipitation values. Although both CTRL and M&M overestimate the total precipitation of the MCC, M&M maximum precipitation is located closer to Presidente Roque Saenz Peña where the most intense precipitation was registered and the difference with the observed value is smaller.
ÁreaMET
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP7W/3892P38
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP7W/3892P38
Idiomaen
Arquivo Alvodoyle_experiments.pdf
Grupo de Usuáriosadministrator
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5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/3F3T29H
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.19.20.40 3
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosarchivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor format isbn issn label lineage mark nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark type url versiontype volume
7. Controle da descrição
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