RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL

The fluvial plains or Parana River Unit constitutes an plan surface where thehood vegetable is the principal form of enhancement from the relief forms, sincethat the highlands has arboreal vegetation, middle lands are shrubs covered,low lands with fields and the shallows with hygrophytes forms. The...

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Main Authors: Paulo Cesar Rocha, João Lima Sant’Anna Neto
Format: Article
Language:Portuguese
Published: Associação Brasileira de Climatologa 2010-06-01
Series:Revista Brasileira de Climatologia
Subjects:
Online Access:https://revistas.ufpr.br/revistaabclima/article/view/25592
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spelling doaj-4e97f172414c4675b98886bb8979ae632020-11-25T01:01:57ZporAssociação Brasileira de ClimatologaRevista Brasileira de Climatologia1980-055X2237-86422010-06-016010.5380/abclima.v6i0.2559215677RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASILPaulo Cesar RochaJoão Lima Sant’Anna NetoThe fluvial plains or Parana River Unit constitutes an plan surface where thehood vegetable is the principal form of enhancement from the relief forms, sincethat the highlands has arboreal vegetation, middle lands are shrubs covered,low lands with fields and the shallows with hygrophytes forms. The most flangedparts constitute water bodies, on form of channels assets and lagoons. Thisstudy aims to discuss the influence from the variations on the atmospheric conditions what to anticipate field samplings of limnology variables in channelsthat compose aquatic environments of the high Parana River fluvial plains andits influence on the connectivity patterns among the aquatic environments of thestudy system, assisted by statistic treatment. The results indicate acharacterization by another type of aquatic environments homogenization, otherthan that caused by overflow from the main rivers. During the multi-skilled ofPolar air masses, since air and water temperatures decreases and dissolvedoxygen elevates allowing then the environments presented awhilehomogenization regarding the measurable variables.https://revistas.ufpr.br/revistaabclima/article/view/25592Ritmo ClimáticoDinâmica limnológicaRio Paraná
collection DOAJ
language Portuguese
format Article
sources DOAJ
author Paulo Cesar Rocha
João Lima Sant’Anna Neto
spellingShingle Paulo Cesar Rocha
João Lima Sant’Anna Neto
RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL
Revista Brasileira de Climatologia
Ritmo Climático
Dinâmica limnológica
Rio Paraná
author_facet Paulo Cesar Rocha
João Lima Sant’Anna Neto
author_sort Paulo Cesar Rocha
title RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL
title_short RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL
title_full RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL
title_fullStr RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL
title_full_unstemmed RITMO CLIMÁTICO E DINÂMICA LIMNOLÓGICA NA PLANÍCIE FLUVIAL DO ALTO RIO PARANÁ, CENTRO-SUL DO BRASIL
title_sort ritmo climático e dinâmica limnológica na planície fluvial do alto rio paraná, centro-sul do brasil
publisher Associação Brasileira de Climatologa
series Revista Brasileira de Climatologia
issn 1980-055X
2237-8642
publishDate 2010-06-01
description The fluvial plains or Parana River Unit constitutes an plan surface where thehood vegetable is the principal form of enhancement from the relief forms, sincethat the highlands has arboreal vegetation, middle lands are shrubs covered,low lands with fields and the shallows with hygrophytes forms. The most flangedparts constitute water bodies, on form of channels assets and lagoons. Thisstudy aims to discuss the influence from the variations on the atmospheric conditions what to anticipate field samplings of limnology variables in channelsthat compose aquatic environments of the high Parana River fluvial plains andits influence on the connectivity patterns among the aquatic environments of thestudy system, assisted by statistic treatment. The results indicate acharacterization by another type of aquatic environments homogenization, otherthan that caused by overflow from the main rivers. During the multi-skilled ofPolar air masses, since air and water temperatures decreases and dissolvedoxygen elevates allowing then the environments presented awhilehomogenization regarding the measurable variables.
topic Ritmo Climático
Dinâmica limnológica
Rio Paraná
url https://revistas.ufpr.br/revistaabclima/article/view/25592
work_keys_str_mv AT paulocesarrocha ritmoclimaticoedinamicalimnologicanaplaniciefluvialdoaltorioparanacentrosuldobrasil
AT joaolimasantannaneto ritmoclimaticoedinamicalimnologicanaplaniciefluvialdoaltorioparanacentrosuldobrasil
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