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• W2028343812 abstract "Thermal gradient of a Central Amazonian lake was studied to establish a link between seasonal variations in the water level, temperature, suspended particulate matter (SPM) and thermal stratification. Bimonthly measurements of temperature and PAR radiation were made at 0.25 m intervals from the surface to bottom from February 2004 to July 2006. Daily occurs full vertical mixing of the water column, and classic thermal stratification was not observed in the period. The effect of the winds associated to flood-pulse and the penetrative convection, transported the turbulent kinetic energy (TKE) into the lake mixing the column of water. This phenomenon was more expressive in the rainfall seasons when is generally higher contributing to the circulation of the water. The limit of the euphotic zone ranged from 1.36 to 1.77 m in the period studied. The results of the transmission curves for the sampling sites showed that, in general, less than 0.01% of the surface light reached the bottom. The trend curve developed can facilitate the understanding of the limnological and ecological processes in lentic systems of whitewaters of the Central Amazonian." @default.
• W2028343812 created "2016-06-24" @default.
• W2028343812 creator A5029768157 @default.
• W2028343812 date "2011-05-17" @default.
• W2028343812 modified "2023-09-30" @default.
• W2028343812 title "Thermal structure of the Poraquê lake, Central Amazonian, Brazil" @default.
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• W2028343812 doi "https://doi.org/10.4025/actascibiolsci.v33i2.5150" @default.
• W2028343812 hasPublicationYear "2011" @default.
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