2016
DOI: 10.1590/0102-778631231420150035
|View full text |Cite
|
Sign up to set email alerts
|

Incluindo Funcionalidades no Modelo BRAMS para Simular o Transporte de Cinzas Vulcânicas: Descrição e Análise de Sensibilidade Aplicada ao Evento Eruptivo do Puyehue em 2011

Abstract: Resumo Este trabalho possui dois objetivos principais, o primeiro é apresentar uma descrição de como o modelo atmosférico BRAMS foi estruturado com o intuito de capacitá-lo a simular a emissão, dispersão e sedimentação de cinzas vulcânicas; o segundo é fazer uma análise de sensibilidade com relação a diversas configurações do modelo, com o intuito de obter uma configuração adequada para prever a concentração de cinzas vulcânicas após eventos eruptivos. Avaliando os resultados do modelo com dados observados, pr… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
3
0

Year Published

2017
2017
2024
2024

Publication Types

Select...
3

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(3 citation statements)
references
References 12 publications
0
3
0
Order By: Relevance
“…Cloud and drizzle number concentrations are computed from cloud condensation nuclei (CCN) and giant CCN (GCCN) concentrations, respectively. A lookup table (LUT) is used to obtain the CCN concentration that is activated as a function of aerosol size, concentration, and composition via hygroscopicity parameter (Petters and Kreidenweis, 2007), as well as updraft velocities, pressure, and temperature. On the other hand, GCCN activation does not depend on the environmental conditions, being completely used in the drizzle nucleation process.…”
Section: Two-moment Parameterization From Rams/csumentioning
confidence: 99%
See 1 more Smart Citation
“…Cloud and drizzle number concentrations are computed from cloud condensation nuclei (CCN) and giant CCN (GCCN) concentrations, respectively. A lookup table (LUT) is used to obtain the CCN concentration that is activated as a function of aerosol size, concentration, and composition via hygroscopicity parameter (Petters and Kreidenweis, 2007), as well as updraft velocities, pressure, and temperature. On the other hand, GCCN activation does not depend on the environmental conditions, being completely used in the drizzle nucleation process.…”
Section: Two-moment Parameterization From Rams/csumentioning
confidence: 99%
“…Aerosol activation also uses a LUT of activated fraction determined by temperature, vertical velocity, aerosol number concentration, and hygroscopicity parameter determined by the model. The LUT was built following Köhler activation theory within a parcel model from Feingold and Heymsfield (1992) with additional changes by Eidhammer et al (2009) to use the hygroscopicity parameter (Petters and Kreidenweis, 2007). This approach is similar to the one used by RAMS Figure 1.…”
Section: Thompson Cloud Microphysicsmentioning
confidence: 99%
“…During the event, GOES-12 was operating as GOES-East. Figure 8 GOES-12 images together with a chemical transport model [Coupled Aerosol and Tracer Transport Model within the Brazilian Developments on the Regional Atmospheric Modeling System (CATT-BRAMS); Freitas et al 2017] were used to monitor in real time the volcanic ash traces and predict possible risk areas (Costa et al 2012;Pavani et al 2016). The Argentinean Naval Hydrographic Service (SHN) in collaboration with the Argentinean National Meteorological Service also explored the GOES imagery coupled with an ash dispersion model to monitor this event (Collini et al 2015).…”
Section: Case Studies Cptec-inpe Has High Demandmentioning
confidence: 99%