Please use this identifier to cite or link to this item: http://repositorio.ufc.br/handle/riufc/68825
Type: Artigo de Periódico
Title: Radar-observed spatial and temporal rainfall variability near the Tapajós-Amazon confluence
Other Titles: Variabilidade espacial e temporal da precipitação observada com o radar na confluência do Tapajós e Amazonas
Authors: Cohen, Julia Clarinda Paiva
Fitzjarrald, David Roy
D’Oliveira, Flávio Augusto Farias
Saraiva, Ivan
Barbosa, Illelson Rafael Da Silva
Gandu, Adilson Wagner
Kuhn, Paulo Afonso
Keywords: Precipitation;River Breeze;Instability Lines;Precipitação;Rio - Brisa;Linhas de instabilidade
Issue Date: 2014
Publisher: Revista Brasileira de Meteorologia
Citation: COHEN, Julia Clarinda Paiva; FITZJARRALD, David Roy; D’OLIVEIRA, Flávio Augusto Farias; SAIRAVA, Ivan; BARBOSA, Illelson Rafael Da Silva; GANDU, Adilson Wagner KUHN, Paulo Afonso. Radar-observed spatial and temporal rainfall variability near the Tapajós-Amazon confluence. Revista Brasileira de Meteorologia, Rio de Janeiro, v. 29, p. 23-30, 2014.
Abstract: Standard Amazonian rainfall climatologies rely on stations preferentially located near river margins. River breeze circulations that tend to suppress afternoon rainfall near the river and enhance it inland are not typically considered when reporting results. Previous studies found surprising nocturnal rainfall maxima near the rivers in some locations. We examine spatial and temporal rainfall variability in the Santarém region of the Tapajós-Amazon confluence, seeking to describe the importance of breeze effects on afternoon precipitation and defining the areal extent of nocturnal rainfall maxima.We used three years of mean S band radar reflectivity from Santarém airport with a Z-R relationship appropriate for tropical convective conditions. These data were complemented by TRMM satellite rainfall estimates. Nocturnal rainfall was enhanced along the Amazon River, consistent with the hypothesis that these are associated with the passage of instability lines, perhaps enhanced by local channeling and by land breeze convergence. In the daytime, two rainfall bands appear in mean results, along the east bank of the Tapajós River and to the south of the Amazon River, respectively. Keywords :
URI: http://www.repositorio.ufc.br/handle/riufc/68825
ISSN: 0102-7786
Appears in Collections:LABOMAR - Artigos publicados em revistas científicas

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