Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America

Detalhes bibliográficos
Autor(a) principal: Gonzalo Andrés Guajardo Ferrada
Data de Publicação: 2016
Tipo de documento: Dissertação
Idioma: eng
Título da fonte: Biblioteca Digital de Teses e Dissertações do INPE
Texto Completo: http://urlib.net/sid.inpe.br/mtc-m21b/2016/07.04.16.18
Resumo: This study had the aim to evaluate the new developments on the Plume Rise Model (PRM), embedded into the BRAMS model. PRM computes the biomass burning plume injection heights and returns that information to the host model. Then, the atmospheric model releases all the fire emissions at this height. New developments are based on the initialization data used by the PRM, using fire size and fire radiative power (FRP) from remote sensing. The main difference between the two new versions is the conversion parameter ($\beta$) used to convert from FRP to the plume convective flux. In addition, a new scheme to generate daily fire emission fluxes is implemented, using the fire radiative energy (computed from remote sensing) in the Brazilian Biomass Burning Emission Model (3BEM-FRE). Model results using the three versions of the PRM are compared with observed airborne CO and O$_{3}$ data from the South American Biomass Burning Analysis (SAMBBA) campaign, which took place in southern Amazonia and Cerrado regions in September 2012. Results show that improvements in both 3BEM-FRE and PRM models, have a better performance in the vertical and horizontal reproduction of CO and O$-{3}$ than the original versions of both models, especially in the middle and upper troposphere, specially, reproducing fires over the Cerrado region. Nevertheless, new versions of both models have some difficulty to reproduce the emissions by the end of the campaign, probably due to the cumulus parameterization used, which overestimated the precipitation in the region of study.
id INPE_915d0adb28ff17e93cc1b91b6041740d
oai_identifier_str oai:urlib.net:sid.inpe.br/mtc-m21b/2016/07.04.16.18.49-0
network_acronym_str INPE
network_name_str Biblioteca Digital de Teses e Dissertações do INPE
spelling info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisSensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South AmericaSensibilidade do modelo Plume Rise Model na estimativa da altura de injeção de plumas de queimadas na América do Sul2016-07-14Saulo Ribeiro de FreitasNilton Manuel Évora do RosárioGonzalo Andrés Guajardo FerradaInstituto Nacional de Pesquisas Espaciais (INPE)Programa de Pós-Graduação do INPE em MeteorologiaINPEBRbiomass burningemissionsplume injection heightsSAMBBAqueimadasemissõesaltura de injeçãoThis study had the aim to evaluate the new developments on the Plume Rise Model (PRM), embedded into the BRAMS model. PRM computes the biomass burning plume injection heights and returns that information to the host model. Then, the atmospheric model releases all the fire emissions at this height. New developments are based on the initialization data used by the PRM, using fire size and fire radiative power (FRP) from remote sensing. The main difference between the two new versions is the conversion parameter ($\beta$) used to convert from FRP to the plume convective flux. In addition, a new scheme to generate daily fire emission fluxes is implemented, using the fire radiative energy (computed from remote sensing) in the Brazilian Biomass Burning Emission Model (3BEM-FRE). Model results using the three versions of the PRM are compared with observed airborne CO and O$_{3}$ data from the South American Biomass Burning Analysis (SAMBBA) campaign, which took place in southern Amazonia and Cerrado regions in September 2012. Results show that improvements in both 3BEM-FRE and PRM models, have a better performance in the vertical and horizontal reproduction of CO and O$-{3}$ than the original versions of both models, especially in the middle and upper troposphere, specially, reproducing fires over the Cerrado region. Nevertheless, new versions of both models have some difficulty to reproduce the emissions by the end of the campaign, probably due to the cumulus parameterization used, which overestimated the precipitation in the region of study.Este estudo teve como objetivo avaliar os novos desenvolvimentos no modelo Plume Rise Model (PRM), inserido no modelo BRAMS. O modelo PRM calcula a altura de injeção das plumas das queimadas e devolve esse dado para o modelo atmosférico. Logo, o modelo BRAMS libera todas as emissões das queimadas nesta altura. Os novos desenvolvimentos, baseiam-se no uso da área do fogo e a potência radiativa do fogo (FRP), obtidos via sensoriamento remoto, que são usados para a inicialização do PRM. A diferença entre as duas novas versões está no parâmetro de conversão de FRP para o fluxo conectivo das plumas ($\beta$). Também, é implementado um esquema para gerar as emissões das queimadas no modelo 3BEM que usa a energia radiativa do fogo (calculada a partir da FRP) para estimar a emissões diárias dos fogos detectados (3BEM-FRE). Os resultados das simulações com as novas versões do PRM são comparados com dados de voos da campanha South American Biomass Burning Analysis (SAMBBA), que teve lugar no sul da Amazônia e Cerrado brasileiro em setembro de 2012. Os resultados mostram que os desenvolvimentos feitos no 3BEM-FRE e no PRM, tiveram melhor desempenho na reprodução vertical e horizontal do CO e O$_{3}$ emitido pelas queimadas, do que as versões originais destes modelos, especialmente na troposfera média e alta. Embora, haja dificuldade para reproduzir as emissões para o final da campanha, provávelmente devido à parametrização de cumulus utilizada, que superestimou a precipitação na região de estudo.http://urlib.net/sid.inpe.br/mtc-m21b/2016/07.04.16.18info:eu-repo/semantics/openAccessengreponame:Biblioteca Digital de Teses e Dissertações do INPEinstname:Instituto Nacional de Pesquisas Espaciais (INPE)instacron:INPE2021-07-31T06:55:08Zoai:urlib.net:sid.inpe.br/mtc-m21b/2016/07.04.16.18.49-0Biblioteca Digital de Teses e Dissertaçõeshttp://bibdigital.sid.inpe.br/PUBhttp://bibdigital.sid.inpe.br/col/iconet.com.br/banon/2003/11.21.21.08/doc/oai.cgiopendoar:32772021-07-31 06:55:09.554Biblioteca Digital de Teses e Dissertações do INPE - Instituto Nacional de Pesquisas Espaciais (INPE)false
dc.title.en.fl_str_mv Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
dc.title.alternative.pt.fl_str_mv Sensibilidade do modelo Plume Rise Model na estimativa da altura de injeção de plumas de queimadas na América do Sul
title Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
spellingShingle Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
Gonzalo Andrés Guajardo Ferrada
title_short Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
title_full Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
title_fullStr Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
title_full_unstemmed Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
title_sort Sensitivity of the Plume Rise Model in the estimation of biomass burning plume injection heights in South America
author Gonzalo Andrés Guajardo Ferrada
author_facet Gonzalo Andrés Guajardo Ferrada
author_role author
dc.contributor.advisor1.fl_str_mv Saulo Ribeiro de Freitas
dc.contributor.referee1.fl_str_mv Nilton Manuel Évora do Rosário
dc.contributor.author.fl_str_mv Gonzalo Andrés Guajardo Ferrada
contributor_str_mv Saulo Ribeiro de Freitas
Nilton Manuel Évora do Rosário
dc.description.abstract.por.fl_txt_mv This study had the aim to evaluate the new developments on the Plume Rise Model (PRM), embedded into the BRAMS model. PRM computes the biomass burning plume injection heights and returns that information to the host model. Then, the atmospheric model releases all the fire emissions at this height. New developments are based on the initialization data used by the PRM, using fire size and fire radiative power (FRP) from remote sensing. The main difference between the two new versions is the conversion parameter ($\beta$) used to convert from FRP to the plume convective flux. In addition, a new scheme to generate daily fire emission fluxes is implemented, using the fire radiative energy (computed from remote sensing) in the Brazilian Biomass Burning Emission Model (3BEM-FRE). Model results using the three versions of the PRM are compared with observed airborne CO and O$_{3}$ data from the South American Biomass Burning Analysis (SAMBBA) campaign, which took place in southern Amazonia and Cerrado regions in September 2012. Results show that improvements in both 3BEM-FRE and PRM models, have a better performance in the vertical and horizontal reproduction of CO and O$-{3}$ than the original versions of both models, especially in the middle and upper troposphere, specially, reproducing fires over the Cerrado region. Nevertheless, new versions of both models have some difficulty to reproduce the emissions by the end of the campaign, probably due to the cumulus parameterization used, which overestimated the precipitation in the region of study.
Este estudo teve como objetivo avaliar os novos desenvolvimentos no modelo Plume Rise Model (PRM), inserido no modelo BRAMS. O modelo PRM calcula a altura de injeção das plumas das queimadas e devolve esse dado para o modelo atmosférico. Logo, o modelo BRAMS libera todas as emissões das queimadas nesta altura. Os novos desenvolvimentos, baseiam-se no uso da área do fogo e a potência radiativa do fogo (FRP), obtidos via sensoriamento remoto, que são usados para a inicialização do PRM. A diferença entre as duas novas versões está no parâmetro de conversão de FRP para o fluxo conectivo das plumas ($\beta$). Também, é implementado um esquema para gerar as emissões das queimadas no modelo 3BEM que usa a energia radiativa do fogo (calculada a partir da FRP) para estimar a emissões diárias dos fogos detectados (3BEM-FRE). Os resultados das simulações com as novas versões do PRM são comparados com dados de voos da campanha South American Biomass Burning Analysis (SAMBBA), que teve lugar no sul da Amazônia e Cerrado brasileiro em setembro de 2012. Os resultados mostram que os desenvolvimentos feitos no 3BEM-FRE e no PRM, tiveram melhor desempenho na reprodução vertical e horizontal do CO e O$_{3}$ emitido pelas queimadas, do que as versões originais destes modelos, especialmente na troposfera média e alta. Embora, haja dificuldade para reproduzir as emissões para o final da campanha, provávelmente devido à parametrização de cumulus utilizada, que superestimou a precipitação na região de estudo.
description This study had the aim to evaluate the new developments on the Plume Rise Model (PRM), embedded into the BRAMS model. PRM computes the biomass burning plume injection heights and returns that information to the host model. Then, the atmospheric model releases all the fire emissions at this height. New developments are based on the initialization data used by the PRM, using fire size and fire radiative power (FRP) from remote sensing. The main difference between the two new versions is the conversion parameter ($\beta$) used to convert from FRP to the plume convective flux. In addition, a new scheme to generate daily fire emission fluxes is implemented, using the fire radiative energy (computed from remote sensing) in the Brazilian Biomass Burning Emission Model (3BEM-FRE). Model results using the three versions of the PRM are compared with observed airborne CO and O$_{3}$ data from the South American Biomass Burning Analysis (SAMBBA) campaign, which took place in southern Amazonia and Cerrado regions in September 2012. Results show that improvements in both 3BEM-FRE and PRM models, have a better performance in the vertical and horizontal reproduction of CO and O$-{3}$ than the original versions of both models, especially in the middle and upper troposphere, specially, reproducing fires over the Cerrado region. Nevertheless, new versions of both models have some difficulty to reproduce the emissions by the end of the campaign, probably due to the cumulus parameterization used, which overestimated the precipitation in the region of study.
publishDate 2016
dc.date.issued.fl_str_mv 2016-07-14
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
status_str publishedVersion
format masterThesis
dc.identifier.uri.fl_str_mv http://urlib.net/sid.inpe.br/mtc-m21b/2016/07.04.16.18
url http://urlib.net/sid.inpe.br/mtc-m21b/2016/07.04.16.18
dc.language.iso.fl_str_mv eng
language eng
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Instituto Nacional de Pesquisas Espaciais (INPE)
dc.publisher.program.fl_str_mv Programa de Pós-Graduação do INPE em Meteorologia
dc.publisher.initials.fl_str_mv INPE
dc.publisher.country.fl_str_mv BR
publisher.none.fl_str_mv Instituto Nacional de Pesquisas Espaciais (INPE)
dc.source.none.fl_str_mv reponame:Biblioteca Digital de Teses e Dissertações do INPE
instname:Instituto Nacional de Pesquisas Espaciais (INPE)
instacron:INPE
reponame_str Biblioteca Digital de Teses e Dissertações do INPE
collection Biblioteca Digital de Teses e Dissertações do INPE
instname_str Instituto Nacional de Pesquisas Espaciais (INPE)
instacron_str INPE
institution INPE
repository.name.fl_str_mv Biblioteca Digital de Teses e Dissertações do INPE - Instituto Nacional de Pesquisas Espaciais (INPE)
repository.mail.fl_str_mv
publisher_program_txtF_mv Programa de Pós-Graduação do INPE em Meteorologia
contributor_advisor1_txtF_mv Saulo Ribeiro de Freitas
_version_ 1706809358969470976