Tesis
Estudo da inter-sazonalidade dos fluxos de calor latente e sensível no Cerrado e Pantanal de Mato Grosso
Fecha
2013-06-21Registro en:
CURADO, Leone Francisco Amorim. Estudo da inter-sazonalidade dos fluxos de calor latente e sensível no Cerrado e Pantanal de Mato Grosso. 2013. 104 f. Tese (Doutorado em Física Ambiental) - Universidade Federal de Mato Grosso, Instituto de Física, Cuiabá, 2013.
Autor
Nogueira, José de Souza
Sanches, Luciana
http://lattes.cnpq.br/2358137001200356
http://lattes.cnpq.br/5893185001802390
Nogueira, José de Souza
072.278.841-04
http://lattes.cnpq.br/5893185001802390
Sanches, Luciana
773.270.980-00
http://lattes.cnpq.br/2358137001200356
072.278.841-04
773.270.980-00
Dalmagro, Higo José
089.683.367-41
http://lattes.cnpq.br/2968364807067338
Silva, Tonny José Araújo da
781.203.064-49
http://lattes.cnpq.br/0651075688988405
Dallacort, Rivanildo
022.933.519-55
http://lattes.cnpq.br/1292986021348016
Institución
Resumen
In recent years has intensified the environmental research in the Cerrado and Pantanal regions in order to understand the interrelationships micrometeorological these biomes. This study set out to study the inter-seasonal flows of latent and sensible heat in the Cerrado and the Pantanal of Mato Grosso. Such fluxes were estimated from the Bowen ratio method following the correction of Perez et al. (1999 and 2008) were made and analysis of seasonal and inter-seasonal of latent and sensible heat fluxes from the Bootstrap resampling technique and did the analysis of the relationships between energy flows and system variables through the Pearson correlation. According to the results, the flow of latent and sensible heat present in seasonal differences (between rainy and dry seasons) and inter-seasonal (between the rainy and dry with wet and dry seasons in different years) in virtually all periods . As for interrelations, the fluxes of latent and sensible exhibit complex behavior influencing and being influenced by a group of up to 8 variables among these variables have: the emission of energy by the atmosphere and the clearness index variables that are external to micrometeorology, indicating that there is an influence of micrometeorological and macrometeorológical phenomena the dynamics of the region.