Rainfall distribution in the Atlantic Rainforest

Forest cover is of great importance in the context of water balance and may alter the mechanism of water absorption into the soil surface. The aim of this study was to evaluate the throughfall, stemflow, and surface runoff compared to rainfall in a fragment of the Atlantic Rainforest. Rainfall was m...

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Main Authors: João Paulo Oliveira de Freitas, Herly Carlos Teixeira Dias, Thiago Henrique Azevedo Barroso, Lucas Barros Quaresma Poyares
Format: Article
Language:English
Published: Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi) 2013-08-01
Series:Revista Ambiente & Água
Subjects:
Online Access:http://www.ambi-agua.net/seer/index.php/ambi-agua/article/view/1141
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spelling doaj-74b11c04a8cf45c7be645f3bd17abde22020-11-25T00:21:57ZengInstituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi)Revista Ambiente & Água1980-993X2013-08-018210010810.4136/ambi-agua.1141Rainfall distribution in the Atlantic RainforestJoão Paulo Oliveira de FreitasHerly Carlos Teixeira DiasThiago Henrique Azevedo BarrosoLucas Barros Quaresma PoyaresForest cover is of great importance in the context of water balance and may alter the mechanism of water absorption into the soil surface. The aim of this study was to evaluate the throughfall, stemflow, and surface runoff compared to rainfall in a fragment of the Atlantic Rainforest. Rainfall was measured through a rain gauge and a pluviograph installed on a tower above the forest canopy. To quantify the throughfall, six plots of 20 x20 m were laid, with 25 pluviometers five meters spaced from each other, for each plot. To measure the stemflow, collectors were adapted on the tree trunks having ≥ 15 cm circumference. For the runoff estimate, three plots were established with areas of 13.71 m², 14.79 m² and 14.86 m². The plots were demarcated with galvanized iron sheets. Based on the results, it can be concluded that forests play an important role in the hydrological cycle: from the total precipitation (1182.6 mm), one portion is intercepted by the tree canopy and evaporated back into the atmosphere; another portion (958.1 mm) corresponding to 81% of the total precipitation, passes through the canopy and hits the ground. The stemflow was 10.8 mm, corresponding to 0.9 % of the total rainfall. The runoff was 15.5 mm, which corresponds to 1.3% of the rainfall. The vegetation has an important role in reducing the runoff volume on the soil surface.http://www.ambi-agua.net/seer/index.php/ambi-agua/article/view/1141Precipitation, Forest Hydrology, Watershed Management
collection DOAJ
language English
format Article
sources DOAJ
author João Paulo Oliveira de Freitas
Herly Carlos Teixeira Dias
Thiago Henrique Azevedo Barroso
Lucas Barros Quaresma Poyares
spellingShingle João Paulo Oliveira de Freitas
Herly Carlos Teixeira Dias
Thiago Henrique Azevedo Barroso
Lucas Barros Quaresma Poyares
Rainfall distribution in the Atlantic Rainforest
Revista Ambiente & Água
Precipitation, Forest Hydrology, Watershed Management
author_facet João Paulo Oliveira de Freitas
Herly Carlos Teixeira Dias
Thiago Henrique Azevedo Barroso
Lucas Barros Quaresma Poyares
author_sort João Paulo Oliveira de Freitas
title Rainfall distribution in the Atlantic Rainforest
title_short Rainfall distribution in the Atlantic Rainforest
title_full Rainfall distribution in the Atlantic Rainforest
title_fullStr Rainfall distribution in the Atlantic Rainforest
title_full_unstemmed Rainfall distribution in the Atlantic Rainforest
title_sort rainfall distribution in the atlantic rainforest
publisher Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi)
series Revista Ambiente & Água
issn 1980-993X
publishDate 2013-08-01
description Forest cover is of great importance in the context of water balance and may alter the mechanism of water absorption into the soil surface. The aim of this study was to evaluate the throughfall, stemflow, and surface runoff compared to rainfall in a fragment of the Atlantic Rainforest. Rainfall was measured through a rain gauge and a pluviograph installed on a tower above the forest canopy. To quantify the throughfall, six plots of 20 x20 m were laid, with 25 pluviometers five meters spaced from each other, for each plot. To measure the stemflow, collectors were adapted on the tree trunks having ≥ 15 cm circumference. For the runoff estimate, three plots were established with areas of 13.71 m², 14.79 m² and 14.86 m². The plots were demarcated with galvanized iron sheets. Based on the results, it can be concluded that forests play an important role in the hydrological cycle: from the total precipitation (1182.6 mm), one portion is intercepted by the tree canopy and evaporated back into the atmosphere; another portion (958.1 mm) corresponding to 81% of the total precipitation, passes through the canopy and hits the ground. The stemflow was 10.8 mm, corresponding to 0.9 % of the total rainfall. The runoff was 15.5 mm, which corresponds to 1.3% of the rainfall. The vegetation has an important role in reducing the runoff volume on the soil surface.
topic Precipitation, Forest Hydrology, Watershed Management
url http://www.ambi-agua.net/seer/index.php/ambi-agua/article/view/1141
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