DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE
| Autor(a) principal: | |
|---|---|
| Data de Publicação: | 2024 |
| Outros Autores: | , , , , , , , , |
| Tipo de documento: | Artigo |
| Idioma: | por |
| Título da fonte: | Nativa (Sinop) |
| Texto Completo: | https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/16528 |
Resumo: | The Brazilian Pantanal is a seasonally flooded biome, where microclimatic understanding is essential to understand the importance of this biome on a global scale. The main objective of this study was to analyze the dynamics of longwave radiation fluxes in the Pantanal, as well as the implications of their seasonal and interannual variations on the region's micrometeorology. The study was carried out in a seasonally floodable area in the Brazilian Pantanal in the state of Mato Grosso between 16°29'04" and 16°29'10" S; and between 56°25'25" and 56°25'36" at the site experimental located in the Natural Heritage Reserve (RPPN), assisted by the Social Service of Commerce, known as SESC-Pantanal, where the automatic meteorological station measures and stores solar radiation, air and soil temperature, wind speed and precipitation where evapotranspiration, aridity index, sensible and latent heat flux were calculated. There is a greater range of air temperature in the dry period (May to September) due to cold fronts, while in the rainy period the average temperature, Rn and ETo is greater due to the influence of surface water and greater incident radiation.The seasonality of water in the Pantanal directly influences temperature, energy balance, evapotranspiration and relative humidity. |
| id |
UFMT-2_71dcf7bc5449def4439097d59f3683b6 |
|---|---|
| oai_identifier_str |
oai:periodicoscientificos.ufmt.br:article/16528 |
| network_acronym_str |
UFMT-2 |
| network_name_str |
Nativa (Sinop) |
| repository_id_str |
|
| spelling |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSEmicrometeorology, energy flow, floodable area, Bowen Ratiomicrometeorología, flujo de energía, zona inundable, relación de Bowen.micrometeorologiafluxo de energiaárea inundávelRazão de BowenThe Brazilian Pantanal is a seasonally flooded biome, where microclimatic understanding is essential to understand the importance of this biome on a global scale. The main objective of this study was to analyze the dynamics of longwave radiation fluxes in the Pantanal, as well as the implications of their seasonal and interannual variations on the region's micrometeorology. The study was carried out in a seasonally floodable area in the Brazilian Pantanal in the state of Mato Grosso between 16°29'04" and 16°29'10" S; and between 56°25'25" and 56°25'36" at the site experimental located in the Natural Heritage Reserve (RPPN), assisted by the Social Service of Commerce, known as SESC-Pantanal, where the automatic meteorological station measures and stores solar radiation, air and soil temperature, wind speed and precipitation where evapotranspiration, aridity index, sensible and latent heat flux were calculated. There is a greater range of air temperature in the dry period (May to September) due to cold fronts, while in the rainy period the average temperature, Rn and ETo is greater due to the influence of surface water and greater incident radiation.The seasonality of water in the Pantanal directly influences temperature, energy balance, evapotranspiration and relative humidity.El Pantanal brasileño es un bioma estacionalmente inundado, donde la comprensión microclimática es esencial para comprender la importancia de este bioma a escala global. El principal objetivo de este estudio fue analizar la dinámica de los flujos de radiación de onda larga en el Pantanal, así como las implicaciones de sus variaciones estacionales e interanuales en la micrometeorología de la región. El estudio se llevó a cabo en una zona estacionalmente inundable del Pantanal brasileño en el estado de Mato Grosso entre 16°29'04" y 16°29'10" S; y entre 56°25'25" y 56°25'36 " en el sitio experimental ubicado en la Reserva del Patrimonio Natural (RPPN), asistido por el Servicio Social de Comercio, conocido como SESC-Pantanal, donde la estación meteorológica automática mide y almacena la radiación solar, la temperatura del aire y del suelo, la velocidad del viento y las precipitaciones donde Se calculó la evapotranspiración, índice de aridez, flujo de calor sensible y latente, existiendo un mayor rango de temperatura del aire en el período seco (mayo a septiembre) debido a frentes fríos, mientras que en el período lluvioso la temperatura promedio, Rn y ETo es mayor debido a a la influencia de las aguas superficiales y a una mayor radiación incidente. La estacionalidad del agua en el Pantanal influye directamente en la temperatura, el balance energético, la evapotranspiración y la humedad relativa.O Pantanal brasileiro é um bioma sazonalmente inundável, onde a compreensão microclimática é indispensável para compreender a importância desse bioma em escala global. O objetivo principal deste estudo foi analisar a dinâmica dos fluxos de radiação de onda longa no Pantanal, bem como as implicações de suas variações sazonais e interanuais na micrometeorologia da região. O estudo foi realizado em uma área sazonalmente inundável no Pantanal brasileiro no estado de Mato Grosso entre 16°29’04"e 16°29’10” S; e entre 56°25’25 "e 56°25’36" no sítio experimental localizado na Reserva do Patrimônio Natural (RPPN), assistido pelo Serviço Social do Comércio, conhecido como SESC-Pantanal, local no qual a estação meteorológica automática mensura e armazena a radiação solar, temperatura do ar e do solo, velocidade do vento e precipitação onde foi calculado a evapotranspiração, índice de aridez, fluxo de calor sensível e latente. Há uma maior amplitude da temperatura do ar no período seco (maio a setembro) em função de frentes frias, já no período chuvoso a média de temperatura, Rn e ETo é maior devido a influência da água superficial e maior radiação incidente. A sazonalidade das águas no Pantanal influencia diretamente na temperatura, balanço de energia, evapotranspiração e umidade relativa. Palavras-chave: micrometeorologia; fluxo de energia; área inundável; Razão de Bowen. Dynamics of long-wave radiation flows in the Pantanal Mato-Grossense ABSTRACT: The Brazilian Pantanal is a seasonally flooded biome, where microclimatic understanding is essential to understand the importance of this biome on a global scale. The main objective of this study was to analyze the dynamics of longwave radiation fluxes in the Pantanal, as well as the implications of their seasonal and interannual variations on the region's micrometeorology. The study was carried out in a seasonally floodable area in the Brazilian Pantanal in the state of Mato Grosso between 16°29'04" and 16°29'10" S; and between 56°25'25" and 56°25'36" at the site experimental located in the Natural Heritage Reserve (RPPN), assisted by the Social Service of Commerce, known as SESC-Pantanal, where the automatic meteorological station measures and stores solar radiation, air and soil temperature, wind speed and precipitation where evapotranspiration, aridity index, sensible and latent heat flux were calculated. There is a greater range of air temperature in the dry period (May to September) due to cold fronts, while in the rainy period the average temperature, Rn and ETo is greater due to the influence of surface water and greater incident radiation. The seasonality of water in the Pantanal directly influences temperature, energy balance, evapotranspiration and relative humidity. Keywords: micrometeorology; energy flow; floodable area; Bowen Ratio.Universidade Federal de Mato Grosso2024-03-31info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/1652810.31413/nat.v12i1.16528Nativa; v. 12 n. 1 (2024); 184-190Nativa; Vol. 12 Núm. 1 (2024); 184-190Nativa; Vol. 12 No. 1 (2024); 184-1902318-7670reponame:Nativa (Sinop)instname:Universidade Federal de Mato Grosso (UFMT)instacron:UFMTporhttps://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/16528/13508NacionalCopyright (c) 2024 Nativahttps://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccessSantos, Thamiris Amorim dosJosefa Araujo da Silva, HalineRoberto de Paulo , Sergio Jorge Cabral de Paulo , Iramaia Silva Palácios , Rafael Gomes Duarte , Leilane Santana, Valdicleia GonçalvesSilva, Jaqueline Pereira daBasso Marques , João Francisco Amorim Curado , Leone 2024-02-26T11:12:07Zoai:periodicoscientificos.ufmt.br:article/16528Revistahttps://periodicoscientificos.ufmt.br/ojs/index.php/nativaPUBhttps://periodicoscientificos.ufmt.br/ojs/index.php/nativa/oai||rrmelo2@yahoo.com.br2318-76702318-7670opendoar:2024-02-26T11:12:07Nativa (Sinop) - Universidade Federal de Mato Grosso (UFMT)false |
| dc.title.none.fl_str_mv |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| title |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| spellingShingle |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE Santos, Thamiris Amorim dos micrometeorology, energy flow, floodable area, Bowen Ratio micrometeorología, flujo de energía, zona inundable, relación de Bowen. micrometeorologia fluxo de energia área inundável Razão de Bowen |
| title_short |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| title_full |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| title_fullStr |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| title_full_unstemmed |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| title_sort |
DINÂMICA DOS FLUXOS DE RADIAÇÃO DE ONDA LONGA NO PANTANAL MATO-GROSSENSE |
| author |
Santos, Thamiris Amorim dos |
| author_facet |
Santos, Thamiris Amorim dos Josefa Araujo da Silva, Haline Roberto de Paulo , Sergio Jorge Cabral de Paulo , Iramaia Silva Palácios , Rafael Gomes Duarte , Leilane Santana, Valdicleia Gonçalves Silva, Jaqueline Pereira da Basso Marques , João Francisco Amorim Curado , Leone |
| author_role |
author |
| author2 |
Josefa Araujo da Silva, Haline Roberto de Paulo , Sergio Jorge Cabral de Paulo , Iramaia Silva Palácios , Rafael Gomes Duarte , Leilane Santana, Valdicleia Gonçalves Silva, Jaqueline Pereira da Basso Marques , João Francisco Amorim Curado , Leone |
| author2_role |
author author author author author author author author author |
| dc.contributor.author.fl_str_mv |
Santos, Thamiris Amorim dos Josefa Araujo da Silva, Haline Roberto de Paulo , Sergio Jorge Cabral de Paulo , Iramaia Silva Palácios , Rafael Gomes Duarte , Leilane Santana, Valdicleia Gonçalves Silva, Jaqueline Pereira da Basso Marques , João Francisco Amorim Curado , Leone |
| dc.subject.por.fl_str_mv |
micrometeorology, energy flow, floodable area, Bowen Ratio micrometeorología, flujo de energía, zona inundable, relación de Bowen. micrometeorologia fluxo de energia área inundável Razão de Bowen |
| topic |
micrometeorology, energy flow, floodable area, Bowen Ratio micrometeorología, flujo de energía, zona inundable, relación de Bowen. micrometeorologia fluxo de energia área inundável Razão de Bowen |
| description |
The Brazilian Pantanal is a seasonally flooded biome, where microclimatic understanding is essential to understand the importance of this biome on a global scale. The main objective of this study was to analyze the dynamics of longwave radiation fluxes in the Pantanal, as well as the implications of their seasonal and interannual variations on the region's micrometeorology. The study was carried out in a seasonally floodable area in the Brazilian Pantanal in the state of Mato Grosso between 16°29'04" and 16°29'10" S; and between 56°25'25" and 56°25'36" at the site experimental located in the Natural Heritage Reserve (RPPN), assisted by the Social Service of Commerce, known as SESC-Pantanal, where the automatic meteorological station measures and stores solar radiation, air and soil temperature, wind speed and precipitation where evapotranspiration, aridity index, sensible and latent heat flux were calculated. There is a greater range of air temperature in the dry period (May to September) due to cold fronts, while in the rainy period the average temperature, Rn and ETo is greater due to the influence of surface water and greater incident radiation.The seasonality of water in the Pantanal directly influences temperature, energy balance, evapotranspiration and relative humidity. |
| publishDate |
2024 |
| dc.date.none.fl_str_mv |
2024-03-31 |
| dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.uri.fl_str_mv |
https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/16528 10.31413/nat.v12i1.16528 |
| url |
https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/16528 |
| identifier_str_mv |
10.31413/nat.v12i1.16528 |
| dc.language.iso.fl_str_mv |
por |
| language |
por |
| dc.relation.none.fl_str_mv |
https://periodicoscientificos.ufmt.br/ojs/index.php/nativa/article/view/16528/13508 |
| dc.rights.driver.fl_str_mv |
Copyright (c) 2024 Nativa https://creativecommons.org/licenses/by-nc/4.0 info:eu-repo/semantics/openAccess |
| rights_invalid_str_mv |
Copyright (c) 2024 Nativa https://creativecommons.org/licenses/by-nc/4.0 |
| eu_rights_str_mv |
openAccess |
| dc.format.none.fl_str_mv |
application/pdf |
| dc.coverage.none.fl_str_mv |
Nacional |
| dc.publisher.none.fl_str_mv |
Universidade Federal de Mato Grosso |
| publisher.none.fl_str_mv |
Universidade Federal de Mato Grosso |
| dc.source.none.fl_str_mv |
Nativa; v. 12 n. 1 (2024); 184-190 Nativa; Vol. 12 Núm. 1 (2024); 184-190 Nativa; Vol. 12 No. 1 (2024); 184-190 2318-7670 reponame:Nativa (Sinop) instname:Universidade Federal de Mato Grosso (UFMT) instacron:UFMT |
| instname_str |
Universidade Federal de Mato Grosso (UFMT) |
| instacron_str |
UFMT |
| institution |
UFMT |
| reponame_str |
Nativa (Sinop) |
| collection |
Nativa (Sinop) |
| repository.name.fl_str_mv |
Nativa (Sinop) - Universidade Federal de Mato Grosso (UFMT) |
| repository.mail.fl_str_mv |
||rrmelo2@yahoo.com.br |
| _version_ |
1799711193575718912 |