Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia

Detalhes bibliográficos
Autor(a) principal: Rodrigues, Hernani José Brazão
Data de Publicação: 2006
Tipo de documento: Tese
Idioma: por
Título da fonte: LOCUS Repositório Institucional da UFV
Texto Completo: http://locus.ufv.br/handle/123456789/1515
Resumo: This work use the longest series of continuous meteorological data and fluxes measurements of CO2, sensible heat and latent heat made in Amazon mangrove ecosystem. The series used in this study corresponds to the period of November, 2002 to August, 2003. The meteorological data were collected using an EDISOL system based on the hedí covariance technique. The main objectives of the work were to evaluate the performance of empirical models in estimating the components of radiation and energy balance; quantify the magnitudes of daily and seasonal fluxes of CO2 and its dependence to meteorological variables to evaluate the seasonal variations; to estimate and analyze the temporal variation of stomatal conductance and establish dependence relationships with the micrometeorology of mangrove and to evaluate micrometeorological changes due to the mangrove degradation. In order to estimate the global solar radiation (Rg) models proposed by Hargreaves-Samani and Bristow-Campbell were used based an variations on daily extreme temperatures. Bristow-Campbell s model showed a satisfactory performance while the Hargreaves-Samani s model didn t work well when it rains, although showed good performance in the estimates of Rg under cloudless conditions. The best results for the longwave radiation (BOL) balance estimates were presented by Brutsaert and Bruin s model that account for 70% to 80% of the BOL daily variation. Brunt s model was the one that showed the greatest differences between measured and simulated values, always underestimating the longwave radiation balance. In order to estimate the sensible heat (H) and latent heat (LE) fluxes in the mangroves the models proposed by Shuttleworth, Bruin- Holtslag and Penman-Monteith were applied. The results for sensible heat estimates showed that Shuttleworth model and Bruin-Holtslag model were the best in comparison with measurements data, although it was evident some overestimation and underestimation respectively. Penman-Monteith model showed an overestimation of about 10% to 15% and it s best results were obtained in the rainy season. A lower performance was presented by the models in the estimation of latent heat flux, in comparison with the sensible heat flux estimates. However, the Penman-Monteith model was the one that showed a lower difference between measured and simulated values and thus in considered the more appropriate in estimating the latent heat flux in mangrove. In regard to the partition of net radiation, it was found that the main Exchange of energy in latent heat flux, with 56% of the available energy used in the process of evapotranspiration in the rainy period and 43% in the less rainy period. The energy used for heating the atmosphere by sensible heat did not change much between both periods, corresponding to 27% of the net radiation. The hourly pattern of the stomatal conductance was evaluated, presenting a mean value of 0,015 m.s-1 in the rainy period and 0,027 m.s-1 in the less rainy period it was found that the vapor pressure deficit was the variable that showed the best dependence relationship with the stomatal conductance in both seasonal periods of the year. The pattern of stomatal conductance was also influenced by the net radiation. The daily cycles of CO2 fluxes showed an mean diurnal assimilation of 7 to 15 μmol.m-2,s-1, and a mean nocturnal emission that corresponds to the ecossystem respiration of 5 μmol.m-2,s-1, suggesting that the mangrove is a sink of CO2. In regard to the changes due to the mangrove degradation, the results showed that the deforestation caused an increase in air and soil temperature. The mangrove degradation caused an increase in surface albedo and a decrease in the air humidity, due to reduction in evapotranspiration because of vegetation renoval. The amplitude of soil heat flux in the degraded mangrove was six times higher than in the natural mangrove due to the high rates of heating in the degraded area.
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spelling Rodrigues, Hernani José Brazãohttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4782574P8Ribeiro, João Batista Mirandahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4782574Z7Costa, Antônio Carlos Lola dahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4766650H5Costa, José Maria Nogueira dahttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783772Y3Ferreira, Williams Pinto Marqueshttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4799404E8Lima, Francisca Zenaide dehttp://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4763794Y62015-03-26T12:49:19Z2007-04-192015-03-26T12:49:19Z2006-08-14RODRIGUES, Hernani José Brazão. Radiation and energy balance and fluxes of CO2 in a Amazon mangrove ecosystem. 2006. 226 f. Tese (Doutorado em Agrometeorologia; Climatologia; Micrometeorologia) - Universidade Federal de Viçosa, Viçosa, 2006.http://locus.ufv.br/handle/123456789/1515This work use the longest series of continuous meteorological data and fluxes measurements of CO2, sensible heat and latent heat made in Amazon mangrove ecosystem. The series used in this study corresponds to the period of November, 2002 to August, 2003. The meteorological data were collected using an EDISOL system based on the hedí covariance technique. The main objectives of the work were to evaluate the performance of empirical models in estimating the components of radiation and energy balance; quantify the magnitudes of daily and seasonal fluxes of CO2 and its dependence to meteorological variables to evaluate the seasonal variations; to estimate and analyze the temporal variation of stomatal conductance and establish dependence relationships with the micrometeorology of mangrove and to evaluate micrometeorological changes due to the mangrove degradation. In order to estimate the global solar radiation (Rg) models proposed by Hargreaves-Samani and Bristow-Campbell were used based an variations on daily extreme temperatures. Bristow-Campbell s model showed a satisfactory performance while the Hargreaves-Samani s model didn t work well when it rains, although showed good performance in the estimates of Rg under cloudless conditions. The best results for the longwave radiation (BOL) balance estimates were presented by Brutsaert and Bruin s model that account for 70% to 80% of the BOL daily variation. Brunt s model was the one that showed the greatest differences between measured and simulated values, always underestimating the longwave radiation balance. In order to estimate the sensible heat (H) and latent heat (LE) fluxes in the mangroves the models proposed by Shuttleworth, Bruin- Holtslag and Penman-Monteith were applied. The results for sensible heat estimates showed that Shuttleworth model and Bruin-Holtslag model were the best in comparison with measurements data, although it was evident some overestimation and underestimation respectively. Penman-Monteith model showed an overestimation of about 10% to 15% and it s best results were obtained in the rainy season. A lower performance was presented by the models in the estimation of latent heat flux, in comparison with the sensible heat flux estimates. However, the Penman-Monteith model was the one that showed a lower difference between measured and simulated values and thus in considered the more appropriate in estimating the latent heat flux in mangrove. In regard to the partition of net radiation, it was found that the main Exchange of energy in latent heat flux, with 56% of the available energy used in the process of evapotranspiration in the rainy period and 43% in the less rainy period. The energy used for heating the atmosphere by sensible heat did not change much between both periods, corresponding to 27% of the net radiation. The hourly pattern of the stomatal conductance was evaluated, presenting a mean value of 0,015 m.s-1 in the rainy period and 0,027 m.s-1 in the less rainy period it was found that the vapor pressure deficit was the variable that showed the best dependence relationship with the stomatal conductance in both seasonal periods of the year. The pattern of stomatal conductance was also influenced by the net radiation. The daily cycles of CO2 fluxes showed an mean diurnal assimilation of 7 to 15 μmol.m-2,s-1, and a mean nocturnal emission that corresponds to the ecossystem respiration of 5 μmol.m-2,s-1, suggesting that the mangrove is a sink of CO2. In regard to the changes due to the mangrove degradation, the results showed that the deforestation caused an increase in air and soil temperature. The mangrove degradation caused an increase in surface albedo and a decrease in the air humidity, due to reduction in evapotranspiration because of vegetation renoval. The amplitude of soil heat flux in the degraded mangrove was six times higher than in the natural mangrove due to the high rates of heating in the degraded area.Este trabalho utiliza a mais longa série de dados meteorológicos contínuos e medições de fluxos de CO2, calor sensível e calor latente, obtidos em ecossistema de manguezal amazônico. A série utilizada neste estudo corresponde ao período de novembro de 2002 a agosto de 2003. Os dados meteorológicos foram coletados por uma estação meteorológica automática e os fluxos de CO2 e energia foram medidos com o sistema EDISOL que utiliza a técnica de covariância de vórtices turbulentos. Os principais objetivos do presente trabalho foram, avaliar o desempenho de modelos empíricos na estimativa dos componentes do balanço de radiação e energia; avaliar as variações sazonais da partição dos componentes do balanço de radiação e energia; quantificar as magnitudes diárias e sazonais dos fluxos de CO2 e suas relações de dependência com variáveis meteorológicas; estimar e analisar a variação temporal da condutância estomática e estabelecer relações de dependência com a micrometeorologia do manguezal e finalmente avaliar alterações micrometeorológicas decorrentes da degradação no manguezal. Na estimativa da radiação solar global (Rg), foram utilizados os modelos propostos por Hargreaves-Samani e Bristow-Campbell, que se baseiam nas variações de temperaturas extremas diárias. O modelo de Bristow-Campbell apresentou desempenho satisfatório e o modelo de Hargreaves-Samani se mostrou bastante sensível às ocorrências de precipitação mostrando, todavia bom desempenho nas estimativas de Rg para dias de céu claro. Nas simulações do balanço de radiação de onda longa (BOL), os melhores resultados são apresentados pelos modelos de Brutsaert e Bruin, que conseguem reproduzir entre 70% e 80% a variabilidade diária do BOL. O modelo baseado em Brunt foi o que mostrou as maiores diferenças entre valores medidos e simulados, apresentando sempre subestimativa do balanço de radiação de ondas longas. Para estimativa dos fluxos de calor sensível (H) e calor latente (LE) no manguezal, foram aplicados os modelos propostos por Shuttleworth, Bruin-Holtslag e Penman-Monteith. Nas estimativas do fluxo de calor sensível, os resultados mostraram que os modelos de Shuttleworth e Bruin-Holtslag são os que simulam mais próximos dos dados medidos, ressaltando que ambos fazem ligeira superestimativa e subestimativa respectivamente. O modelo de Penman- Monteith apresentou uma superestimativa da ordem de 10 a 15% e seus melhores resultados são obtidos na estação chuvosa. Na estimativa do fluxo de calor latente, os modelos apresentaram um menor desempenho, quando comparado com as simulações de H. Contudo, o modelo de Penman- Monteith foi o que apresentou menor diferença entre valores medidos e simulados, podendo ser considerado o mais apropriado nas estimativas de LE no manguezal. Em relação à partição do saldo de radiação, verificou-se que a troca de energia dá-se predominantemente sob a forma de calor latente, com 56% da energia disponível utilizada para o processo de evapotranspiração no período chuvoso e 43% no período menos chuvoso. A energia utilizada para aquecimento da atmosfera sob a forma de calor sensível, praticamente não diferiu entre os períodos e correspondeu a 27% do saldo de radiação. Foi avaliado o comportamento horário da condutância estomática que apresentou um valor médio de 0,015 m.s-¹ no período chuvoso e 0,027 m.s-¹ no período menos chuvoso. Constatou-se que o déficit de pressão de vapor foi a variável que apresentou melhor relação de dependência com a condutância estomática, independente da época do ano. O comportamento da condutância estomática também foi influenciado pelo saldo de radiação. O ciclo diário de fluxo de CO2 apresentou uma absorção média de 7 a 15 μmol m-2 s-1 e uma emissão média noturna que corresponde a respiração do ecossistema de 5 μmol m-2 s-1, indicando que o manguezal foi um sumidouro de CO2. Em relação às alterações decorrentes da degradação no manguezal, os resultados mostraram que o desmatamento proporcionou um aumento de temperatura, tanto do ar como do solo. A degradação do manguezal resultou em um aumento do albedo superficial e em termos de umidade no ar, esta sofre considerável diminuição, basicamente devido à ausência da vegetação que proporciona uma diminuição da evapotranspiração. Devido às altas taxas de aquecimento na área degradada, o fluxo de calor no solo apresentou uma amplitude seis vezes maior que a medida no manguezal natural.Coordenação de Aperfeiçoamento de Pessoal de Nível Superiorapplication/pdfporUniversidade Federal de ViçosaDoutorado em Meteorologia AgrícolaUFVBRAgrometeorologia; Climatologia; MicrometeorologiaManguezalModelos empíricosMedidas de fluxosMangroveEmpirical modelsMeasurements of flowCNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA::MICROMETEOROLOGIABalanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na AmazôniaRadiation and energy balance and fluxes of CO2 in a Amazon mangrove ecosysteminfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/doctoralThesisinfo:eu-repo/semantics/openAccessreponame:LOCUS Repositório Institucional da UFVinstname:Universidade Federal de Viçosa (UFV)instacron:UFVORIGINAL01 - capa_abstract.pdfapplication/pdf201389https://locus.ufv.br//bitstream/123456789/1515/1/01%20-%20capa_abstract.pdfaa5abeaf1078d1de4aed08a6b016bfbbMD5102 - introducao_materiais e metodos.pdf02 - introducao_materiais e metodos.pdfapplication/pdf668421https://locus.ufv.br//bitstream/123456789/1515/2/02%20-%20introducao_materiais%20e%20metodos.pdf2d09b919dd88150af6762e876064850fMD5203 - resultados_pag 124.pdf03 - resultados_pag 124.pdfapplication/pdf3061674https://locus.ufv.br//bitstream/123456789/1515/3/03%20-%20resultados_pag%20124.pdfa6c232eecaaf40f3380d9d28f991a762MD5304 - pag 125_conclusoes.pdf04 - pag 125_conclusoes.pdfapplication/pdf2610467https://locus.ufv.br//bitstream/123456789/1515/4/04%20-%20pag%20125_conclusoes.pdf6217e34af2ee4051a9b7613fc63c83c1MD5405 - referencias bibliograficas.pdf05 - referencias bibliograficas.pdfapplication/pdf136035https://locus.ufv.br//bitstream/123456789/1515/5/05%20-%20referencias%20bibliograficas.pdfa15ceaa3364679fd22092e56f2e565aaMD55TEXT01 - capa_abstract.pdf.txt01 - capa_abstract.pdf.txtExtracted texttext/plain41335https://locus.ufv.br//bitstream/123456789/1515/6/01%20-%20capa_abstract.pdf.txt486f8e27245dfce512ba30ac4f3cbe2aMD5602 - introducao_materiais e metodos.pdf.txt02 - introducao_materiais e metodos.pdf.txtExtracted texttext/plain124162https://locus.ufv.br//bitstream/123456789/1515/7/02%20-%20introducao_materiais%20e%20metodos.pdf.txt102f809d8532f1c0b0a294c277d2156cMD5703 - resultados_pag 124.pdf.txt03 - resultados_pag 124.pdf.txtExtracted texttext/plain92431https://locus.ufv.br//bitstream/123456789/1515/8/03%20-%20resultados_pag%20124.pdf.txt10a181c4050518285e344ea1a25d36b7MD5804 - pag 125_conclusoes.pdf.txt04 - pag 125_conclusoes.pdf.txtExtracted texttext/plain102967https://locus.ufv.br//bitstream/123456789/1515/9/04%20-%20pag%20125_conclusoes.pdf.txt0267f01b71d94eb58c79b08f0a6a12d5MD5905 - referencias bibliograficas.pdf.txt05 - referencias bibliograficas.pdf.txtExtracted texttext/plain20262https://locus.ufv.br//bitstream/123456789/1515/10/05%20-%20referencias%20bibliograficas.pdf.txt9c90267929f83cb7a8fc365c24a50ab4MD510THUMBNAIL01 - capa_abstract.pdf.jpg01 - capa_abstract.pdf.jpgIM Thumbnailimage/jpeg3629https://locus.ufv.br//bitstream/123456789/1515/11/01%20-%20capa_abstract.pdf.jpg203ec90ec17af116b2adda9848fcb382MD51102 - introducao_materiais e metodos.pdf.jpg02 - introducao_materiais e metodos.pdf.jpgIM Thumbnailimage/jpeg4411https://locus.ufv.br//bitstream/123456789/1515/12/02%20-%20introducao_materiais%20e%20metodos.pdf.jpg4417281a73afbe3d81ed9ff402d54195MD51203 - resultados_pag 124.pdf.jpg03 - resultados_pag 124.pdf.jpgIM Thumbnailimage/jpeg4520https://locus.ufv.br//bitstream/123456789/1515/13/03%20-%20resultados_pag%20124.pdf.jpgd618afff7d236f967524210d44c26229MD51304 - pag 125_conclusoes.pdf.jpg04 - pag 125_conclusoes.pdf.jpgIM Thumbnailimage/jpeg4539https://locus.ufv.br//bitstream/123456789/1515/14/04%20-%20pag%20125_conclusoes.pdf.jpgcd708fe85c4cebec1867af9763252789MD51405 - referencias bibliograficas.pdf.jpg05 - referencias bibliograficas.pdf.jpgIM Thumbnailimage/jpeg4385https://locus.ufv.br//bitstream/123456789/1515/15/05%20-%20referencias%20bibliograficas.pdf.jpg7aa5f5fa1c1def73a00f1d8cb6457126MD515123456789/15152016-04-07 23:10:29.005oai:locus.ufv.br:123456789/1515Repositório InstitucionalPUBhttps://www.locus.ufv.br/oai/requestfabiojreis@ufv.bropendoar:21452016-04-08T02:10:29LOCUS Repositório Institucional da UFV - Universidade Federal de Viçosa (UFV)false
dc.title.por.fl_str_mv Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
dc.title.alternative.eng.fl_str_mv Radiation and energy balance and fluxes of CO2 in a Amazon mangrove ecosystem
title Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
spellingShingle Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
Rodrigues, Hernani José Brazão
Manguezal
Modelos empíricos
Medidas de fluxos
Mangrove
Empirical models
Measurements of flow
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA::MICROMETEOROLOGIA
title_short Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
title_full Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
title_fullStr Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
title_full_unstemmed Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
title_sort Balanço de radiação, energia e fluxo de CO2 em ecossistema de manguezal na Amazônia
author Rodrigues, Hernani José Brazão
author_facet Rodrigues, Hernani José Brazão
author_role author
dc.contributor.authorLattes.por.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4782574P8
dc.contributor.author.fl_str_mv Rodrigues, Hernani José Brazão
dc.contributor.advisor-co1.fl_str_mv Ribeiro, João Batista Miranda
dc.contributor.advisor-co1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4782574Z7
dc.contributor.advisor-co2.fl_str_mv Costa, Antônio Carlos Lola da
dc.contributor.advisor-co2Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4766650H5
dc.contributor.advisor1.fl_str_mv Costa, José Maria Nogueira da
dc.contributor.advisor1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4783772Y3
dc.contributor.referee1.fl_str_mv Ferreira, Williams Pinto Marques
dc.contributor.referee1Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4799404E8
dc.contributor.referee2.fl_str_mv Lima, Francisca Zenaide de
dc.contributor.referee2Lattes.fl_str_mv http://buscatextual.cnpq.br/buscatextual/visualizacv.do?id=K4763794Y6
contributor_str_mv Ribeiro, João Batista Miranda
Costa, Antônio Carlos Lola da
Costa, José Maria Nogueira da
Ferreira, Williams Pinto Marques
Lima, Francisca Zenaide de
dc.subject.por.fl_str_mv Manguezal
Modelos empíricos
Medidas de fluxos
topic Manguezal
Modelos empíricos
Medidas de fluxos
Mangrove
Empirical models
Measurements of flow
CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA::MICROMETEOROLOGIA
dc.subject.eng.fl_str_mv Mangrove
Empirical models
Measurements of flow
dc.subject.cnpq.fl_str_mv CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::METEOROLOGIA::MICROMETEOROLOGIA
description This work use the longest series of continuous meteorological data and fluxes measurements of CO2, sensible heat and latent heat made in Amazon mangrove ecosystem. The series used in this study corresponds to the period of November, 2002 to August, 2003. The meteorological data were collected using an EDISOL system based on the hedí covariance technique. The main objectives of the work were to evaluate the performance of empirical models in estimating the components of radiation and energy balance; quantify the magnitudes of daily and seasonal fluxes of CO2 and its dependence to meteorological variables to evaluate the seasonal variations; to estimate and analyze the temporal variation of stomatal conductance and establish dependence relationships with the micrometeorology of mangrove and to evaluate micrometeorological changes due to the mangrove degradation. In order to estimate the global solar radiation (Rg) models proposed by Hargreaves-Samani and Bristow-Campbell were used based an variations on daily extreme temperatures. Bristow-Campbell s model showed a satisfactory performance while the Hargreaves-Samani s model didn t work well when it rains, although showed good performance in the estimates of Rg under cloudless conditions. The best results for the longwave radiation (BOL) balance estimates were presented by Brutsaert and Bruin s model that account for 70% to 80% of the BOL daily variation. Brunt s model was the one that showed the greatest differences between measured and simulated values, always underestimating the longwave radiation balance. In order to estimate the sensible heat (H) and latent heat (LE) fluxes in the mangroves the models proposed by Shuttleworth, Bruin- Holtslag and Penman-Monteith were applied. The results for sensible heat estimates showed that Shuttleworth model and Bruin-Holtslag model were the best in comparison with measurements data, although it was evident some overestimation and underestimation respectively. Penman-Monteith model showed an overestimation of about 10% to 15% and it s best results were obtained in the rainy season. A lower performance was presented by the models in the estimation of latent heat flux, in comparison with the sensible heat flux estimates. However, the Penman-Monteith model was the one that showed a lower difference between measured and simulated values and thus in considered the more appropriate in estimating the latent heat flux in mangrove. In regard to the partition of net radiation, it was found that the main Exchange of energy in latent heat flux, with 56% of the available energy used in the process of evapotranspiration in the rainy period and 43% in the less rainy period. The energy used for heating the atmosphere by sensible heat did not change much between both periods, corresponding to 27% of the net radiation. The hourly pattern of the stomatal conductance was evaluated, presenting a mean value of 0,015 m.s-1 in the rainy period and 0,027 m.s-1 in the less rainy period it was found that the vapor pressure deficit was the variable that showed the best dependence relationship with the stomatal conductance in both seasonal periods of the year. The pattern of stomatal conductance was also influenced by the net radiation. The daily cycles of CO2 fluxes showed an mean diurnal assimilation of 7 to 15 μmol.m-2,s-1, and a mean nocturnal emission that corresponds to the ecossystem respiration of 5 μmol.m-2,s-1, suggesting that the mangrove is a sink of CO2. In regard to the changes due to the mangrove degradation, the results showed that the deforestation caused an increase in air and soil temperature. The mangrove degradation caused an increase in surface albedo and a decrease in the air humidity, due to reduction in evapotranspiration because of vegetation renoval. The amplitude of soil heat flux in the degraded mangrove was six times higher than in the natural mangrove due to the high rates of heating in the degraded area.
publishDate 2006
dc.date.issued.fl_str_mv 2006-08-14
dc.date.available.fl_str_mv 2007-04-19
2015-03-26T12:49:19Z
dc.date.accessioned.fl_str_mv 2015-03-26T12:49:19Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/doctoralThesis
format doctoralThesis
status_str publishedVersion
dc.identifier.citation.fl_str_mv RODRIGUES, Hernani José Brazão. Radiation and energy balance and fluxes of CO2 in a Amazon mangrove ecosystem. 2006. 226 f. Tese (Doutorado em Agrometeorologia; Climatologia; Micrometeorologia) - Universidade Federal de Viçosa, Viçosa, 2006.
dc.identifier.uri.fl_str_mv http://locus.ufv.br/handle/123456789/1515
identifier_str_mv RODRIGUES, Hernani José Brazão. Radiation and energy balance and fluxes of CO2 in a Amazon mangrove ecosystem. 2006. 226 f. Tese (Doutorado em Agrometeorologia; Climatologia; Micrometeorologia) - Universidade Federal de Viçosa, Viçosa, 2006.
url http://locus.ufv.br/handle/123456789/1515
dc.language.iso.fl_str_mv por
language por
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal de Viçosa
dc.publisher.program.fl_str_mv Doutorado em Meteorologia Agrícola
dc.publisher.initials.fl_str_mv UFV
dc.publisher.country.fl_str_mv BR
dc.publisher.department.fl_str_mv Agrometeorologia; Climatologia; Micrometeorologia
publisher.none.fl_str_mv Universidade Federal de Viçosa
dc.source.none.fl_str_mv reponame:LOCUS Repositório Institucional da UFV
instname:Universidade Federal de Viçosa (UFV)
instacron:UFV
instname_str Universidade Federal de Viçosa (UFV)
instacron_str UFV
institution UFV
reponame_str LOCUS Repositório Institucional da UFV
collection LOCUS Repositório Institucional da UFV
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