Detection of surface temperature from LANDSAT-7/ETM+

被引:27
作者
Suga, Y
Ogawa, H
Ohno, K
Yamada, K
机构
[1] Hiroshima Inst Technol, Saeki Ku, Hiroshima 7315193, Japan
[2] Hiroshima Earth Environm Informat Ctr, Saeki Ku, Hiroshima 7315193, Japan
来源
CALIBRATION, CHARACTERIZATION OF SATELLITE SENSORS, PHYSICAL PARAMETERS DERIVED FROM SATELLITE DATA | 2003年 / 32卷 / 11期
关键词
D O I
10.1016/S0273-1177(03)90548-5
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
Hiroshima Institute of Technology (HIT) in Japan has established a LANDSAT-7 Ground Station in cooperation with NASDA for receiving and processing the ETM+ data on March 15(th), 2000 in Japan. The authors performed a verification study on. the surface temperature derived from thermal infrared band image data. of LANDSAT-7/Enhanced Thematic Mapper Plus (ETM+) for the estimation of temperatures around Hiroshima city and bay area in the western part of Japan as a test site. As to the thermal infrared band, the approximate functions for converting the spectral radiance into the surface temperature are estimated by considering both typical surface temperatures measured by the simultaneous field survey with the satellite observation and the spectral radiance observed by ETM+ band 6 (10.40-12.50mum), and then the estimation of the surface temperature distribution around the test site was examined. In this study, the authors estimated the surface temperature distribution equivalent to the land cover categories around the test site for establishing a guideline of surface temperature detection by LANDSAT-7/ETM+ data. As the result of comparison of the truth data and the estimated surface temperature, the correlation coefficients of the approximate function referred to the truth data are from 0.9821 to 0.9994, and the differences are observed from +0.7 to -1.5degreesC in summer, from +0.4 to -0.9degreesC in autumn, from -1.6 to -3.4degreesC in winter and from +0.5 to -0.5degreesC in spring season respectively. It is clearly found that the estimation of surface temperature based on the approximate functions for converting the spectral radiance into the surface temperature referred to the truth data is improved over the directly estimated surface temperature obtained from satellite data. Finally, the successive seasonal change of surface temperature distribution pattern of the test site is precisely detected with the temperature legend of 0 to 80degreesC derived from LANDSAT-7/ETM+ band 6 image data for the thermal environment monitoring. (C) 2003 COSPAR. Published by Elsevier Ltd. All rights reserved.
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页码:2235 / 2240
页数:6
相关论文
共 9 条
[1]  
ERDAS Inc, 1999, ERDAS Field Guide
[2]   RETRIEVAL OF LAND AND SEA-SURFACE TEMPERATURE USING NOAA-11 AVHRR DATA IN NORTH-EASTERN BRAZIL [J].
FRANCA, GB ;
CRACKNELL, AP .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1994, 15 (08) :1695-1712
[3]  
*GEOSYSTEMS GMBH, 2002, ATCOR ERDAS IMAGINE
[4]   VOLCANO MONITORING USING SHORT WAVELENGTH INFRARED DATA FROM SATELLITES [J].
ROTHERY, DA ;
FRANCIS, PW ;
WOOD, CA .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1988, 93 (B7) :7993-&
[5]   SHORT WAVELENGTH INFRARED IMAGES FOR VOLCANO MONITORING [J].
ROTHERY, DA ;
FRANCIS, PW .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1990, 11 (10) :1665-1667
[6]   Processing and accuracy of Landsat thematic mapper data for lake surface temperature measurement [J].
Schneider, K ;
Mauser, W .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 1996, 17 (11) :2027-2041
[7]  
*SPECTR SC INC, 2000, MODTRAN4 USERS MANUA
[8]   Volcano monitoring with Landsat TM short-wave infrared bands: the 1990-1994 eruption of Unzen Volcano, Japan [J].
Urai, M .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 2000, 21 (05) :861-872
[9]  
*USGS, 2000, LANDS 7 SCI DAT US H