The urban heat island in Rio de Janeiro, Brazil, in the last 30 years using remote sensing data

被引:92
|
作者
Peres, Leonardo de Faria [1 ]
de Lucena, Andrews Jose [2 ]
Rotunno Filho, Otto Correa [3 ]
de Almeida Franca, Jose Ricardo [1 ]
机构
[1] Fed Univ Rio de Janeiro UFRJ, Dept Meteorol, Campus Ilha Fundao Cidade Univ, BR-21949900 Rio De Janeiro, RJ, Brazil
[2] Fed Rural Univ Rio de Janeiro UFRRJ, Agron Inst, Dept Geosci, BR-465,Km 7, BR-23890000 Seropedica, RJ, Brazil
[3] Fed Univ Rio de Janeiro UFRJ, COPPE, Civil Engn Program, BR-21945970 Rio De Janeiro, RJ, Brazil
关键词
Urban heat island; Remote sensing; Land-surface temperature; Land-use; Urban planning; LAND-SURFACE TEMPERATURE; SCALE COMMON FEATURES; BAIU FRONTAL ZONE; CLIMATE RESEARCH; TM; EMISSIVITY; RETRIEVAL; IMPACT; MICROCLIMATE; VEGETATION;
D O I
10.1016/j.jag.2017.08.012
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
The aim of this work is to study urban heat island (UHI) in Metropolitan Area of Rio de Janeiro (MARJ) based on the analysis of land-surface temperature (LST) and land-use patterns retrieved from Landsat-5/Thematic Mapper (TM), Landsat-7/Enhanced Thematic Mapper Plus (ETM +) and Landsat-8/Operational Land Imager (011) and Thermal Infrared Sensors (TIRS) data covering a 32-year period between 1984 and 2015. LST temporal evolution is assessed by comparing the average LST composites for 1984-1999 and 2000-2015 where the parametric Student t-test was conducted at 5% significance level to map the pixels where LST for the more recent period is statistically significantly greater than the previous one. The non-parametric Mann-Whitney-Wilcoxon rank sum test has also confirmed at the same 5% significance level that the more recent period (2000-2015) has higher LST values. UHI intensity between "urban" and "rural/urban low density" ("vegetation") areas for 1984-1999 and 2000-2015 was established and confirmed by both parametric and non-parametric tests at 1% significance level as 3.3 degrees C (5.1 degrees C) and 4.4 degrees C (7.1 degrees C), respectively. LST has statistically significantly (p-value < 0.01) increased over time in two of three land cover classes ("urban" and "urban low density"), respectively by 1.9 degrees C and 0.9 degrees C, except in "vegetation" class. A spatial analysis was also performed to identify the urban pixels within MARJ where UHI is more intense by subtracting the LST of these pixels from the LST mean value of "vegetation" land-use class.
引用
收藏
页码:104 / 116
页数:13
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