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		<isbn>978-85-17-00088-1</isbn>
		<label>59827</label>
		<citationkey>PiresSouzJúni:2017:AvTeSu</citationkey>
		<title>Avaliação da temperatura de superfície noturna no Estado do Tocantins, a partir de dados do sensor MODIS</title>
		<format>Internet</format>
		<year>2017</year>
		<secondarytype>PRE CN</secondarytype>
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		<size>1019 KiB</size>
		<author>Pires, Erika Gonçalves,</author>
		<author>Souza, Jaila Raiane Barbosa de,</author>
		<author>Júnior, Laerte Guimarães Ferreira,</author>
		<electronicmailaddress>erikapires@ifto.edu.br</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>8102-8109</pages>
		<booktitle>Anais</booktitle>
		<organization>Instituto Nacional de Pesquisas Espaciais (INPE)</organization>
		<transferableflag>1</transferableflag>
		<abstract>The human is  currently causing changes in climate  through the transformation of nature, occupation  and  modeling space. As a result, it is important conducting studies to analyze the variations of temperature on the planet. In this direction, this study aims to analyze the Night Land Surface Temperature (LSTnight) in Tocantins, from using geotechnology, in order to understand the behavior of temperature in this region. The surface temperature was estimated from the thermal images of sensor MODIS (Moderate Resolution Imaging Spectroradiometer). The LST images allowed the visualization of the spatial and seasonal distribution of temperature in state of Tocantins, in 2001, 2005, 2010 and 2014. In May, lower temperatures prevailed in the region, whereas in October, temperatures tend to be higher, with variation of up to 8 ° C in some regions, between the two months. In May, the minimum and maximum temperature values were lower in the Jalapão microregion, while the Dianopólis microregion had the highest minimum and maximum temperature values during all analyzed years. There were no large discrepancies between the night surface temperature values and the air temperature, obtained at INMET stations during the analyzed period. There is a correlation between the presence of vegetation cover and the variation of the surface temperature, that is, the higher the vegetation presence, the lower the surface temperatures tend to be.</abstract>
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