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		<isbn>978-85-17-00088-1</isbn>
		<label>59566</label>
		<citationkey>OliveiraSilvVale:2017:CaClOn</citationkey>
		<title>Caracterização do clima de ondas da praia de Catuama (Goiana -PE) através do uso do Sistema de Modelagem Costeira (SMC-Brasil)</title>
		<format>Internet</format>
		<year>2017</year>
		<secondarytype>PRE CN</secondarytype>
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		<size>958 KiB</size>
		<author>Oliveira, Patricia Fernanda Passos de,</author>
		<author>Silva, Hewerton Alves da,</author>
		<author>Valença, Lúcia Maria Mafra,</author>
		<electronicmailaddress>patriciapassosoliveira@gmail.com</electronicmailaddress>
		<editor>Gherardi, Douglas Francisco Marcolino,</editor>
		<editor>Aragão, Luiz Eduardo Oliveira e Cruz de,</editor>
		<e-mailaddress>daniela.seki@inpe.br</e-mailaddress>
		<conferencename>Simpósio Brasileiro de Sensoriamento Remoto, 18 (SBSR)</conferencename>
		<conferencelocation>Santos</conferencelocation>
		<date>28-31 maio 2017</date>
		<publisher>Instituto Nacional de Pesquisas Espaciais (INPE)</publisher>
		<publisheraddress>São José dos Campos</publisheraddress>
		<pages>6551-6558</pages>
		<booktitle>Anais</booktitle>
		<organization>Instituto Nacional de Pesquisas Espaciais (INPE)</organization>
		<transferableflag>1</transferableflag>
		<abstract>The relevance of wave studies in specific regions of the coast lies in the establishment of precise physical parameters, which are fundamental subsidies to coastal and oceanic studies. The aim of this work was to understand the characteristics of the waves at Catuama beach through the numerical simulation of the SMC-Brazil wave data base. The Coastal Modeling System (SMC) is a numerical tool that integrates a series of numerical models, which are structured according to the temporal and spatial scales. The program''s database has two time series of sea states of 60 years, as well as methodologies and tools necessary to propagate waves, from deep waters to the beach. The wave directions of higher occurrence are waves coming from the ESE and SE direction, with 77% and 18% of the probability of occurrence. For the average conditions the wavelength varies between 0.9m and 1.45m and in the peak period there is variation between 6.9s and 8.9s. For storm conditions the waves reach between 1.32m and 2.56m peak periods ranged between 12.2s and 13.9s. ESE waves arriving in the region undergo the refraction / diffraction process due to the presence of beachrocks and the smooth topography of the shallow internal platform of Catuama beach. The reefs on the platform form a barrier preventing waves of greater height and energy from reaching the shoreline in the low tide and preamar.</abstract>
		<area>SRE</area>
		<type>Modelagem espacial</type>
		<language>pt</language>
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