Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau

Land surface temperature (LST) is one of the most valuable variables for applications relating to hydrological processes, drought monitoring and climate change. LST from satellite data provides consistent estimates over large scales but is only available for cloud-free pixels, greatly limiting appli...

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Autores principales: Yanmei Zhong, Lingkui Meng, Zushuai Wei, Jian Yang, Weiwei Song, Mohammad Basir
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:df63c917d5994317ae9723f4e9cd85042021-11-25T18:54:28ZRetrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau10.3390/rs132245742072-4292https://doaj.org/article/df63c917d5994317ae9723f4e9cd85042021-11-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/22/4574https://doaj.org/toc/2072-4292Land surface temperature (LST) is one of the most valuable variables for applications relating to hydrological processes, drought monitoring and climate change. LST from satellite data provides consistent estimates over large scales but is only available for cloud-free pixels, greatly limiting applications over frequently cloud-covered regions. With this study, we propose a method for estimating all-weather 1 km LST by combining passive microwave and thermal infrared data. The product is based on clear-sky LST retrieved from Moderate-resolution Imaging Spectroradiometer (MODIS) thermal infrared measurements complemented by LST estimated from the Advanced Microwave Scanning Radiometer Version 2 (AMSR2) brightness temperature to fill gaps caused by clouds. Terrain, vegetation conditions, and AMSR2 multiband information were selected as the auxiliary variables. The random forest algorithm was used to establish the non-linear relationship between the auxiliary variables and LST over the Tibetan Plateau. To assess the error of this method, we performed a validation experiment using clear-sky MODIS LST and in situ measurements. The estimated all-weather LST approximated MODIS LST with an acceptable error, with a coefficient of correlation (r) between 0.87 and 0.99 and a root mean square error (RMSE) between 2.24 K and 5.35 K during the day. At night-time, r was between 0.89 and 0.99 and the RMSE was between 1.02 K and 3.39 K. The error between the estimated LST and in situ LST was also found to be acceptable, with the RMSE for cloudy pixels between 5.15 K and 6.99 K. This method reveals a significant potential to derive all-weather 1 km LST using AMSR2 and MODIS data at a regional and global scale, which will be explored in the future.Yanmei ZhongLingkui MengZushuai WeiJian YangWeiwei SongMohammad BasirMDPI AGarticleland surface temperatureall-weatherfusionrandom forestAMSR-2Tibetan PlateauScienceQENRemote Sensing, Vol 13, Iss 4574, p 4574 (2021)
institution DOAJ
collection DOAJ
language EN
topic land surface temperature
all-weather
fusion
random forest
AMSR-2
Tibetan Plateau
Science
Q
spellingShingle land surface temperature
all-weather
fusion
random forest
AMSR-2
Tibetan Plateau
Science
Q
Yanmei Zhong
Lingkui Meng
Zushuai Wei
Jian Yang
Weiwei Song
Mohammad Basir
Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau
description Land surface temperature (LST) is one of the most valuable variables for applications relating to hydrological processes, drought monitoring and climate change. LST from satellite data provides consistent estimates over large scales but is only available for cloud-free pixels, greatly limiting applications over frequently cloud-covered regions. With this study, we propose a method for estimating all-weather 1 km LST by combining passive microwave and thermal infrared data. The product is based on clear-sky LST retrieved from Moderate-resolution Imaging Spectroradiometer (MODIS) thermal infrared measurements complemented by LST estimated from the Advanced Microwave Scanning Radiometer Version 2 (AMSR2) brightness temperature to fill gaps caused by clouds. Terrain, vegetation conditions, and AMSR2 multiband information were selected as the auxiliary variables. The random forest algorithm was used to establish the non-linear relationship between the auxiliary variables and LST over the Tibetan Plateau. To assess the error of this method, we performed a validation experiment using clear-sky MODIS LST and in situ measurements. The estimated all-weather LST approximated MODIS LST with an acceptable error, with a coefficient of correlation (r) between 0.87 and 0.99 and a root mean square error (RMSE) between 2.24 K and 5.35 K during the day. At night-time, r was between 0.89 and 0.99 and the RMSE was between 1.02 K and 3.39 K. The error between the estimated LST and in situ LST was also found to be acceptable, with the RMSE for cloudy pixels between 5.15 K and 6.99 K. This method reveals a significant potential to derive all-weather 1 km LST using AMSR2 and MODIS data at a regional and global scale, which will be explored in the future.
format article
author Yanmei Zhong
Lingkui Meng
Zushuai Wei
Jian Yang
Weiwei Song
Mohammad Basir
author_facet Yanmei Zhong
Lingkui Meng
Zushuai Wei
Jian Yang
Weiwei Song
Mohammad Basir
author_sort Yanmei Zhong
title Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau
title_short Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau
title_full Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau
title_fullStr Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau
title_full_unstemmed Retrieval of All-Weather 1 km Land Surface Temperature from Combined MODIS and AMSR2 Data over the Tibetan Plateau
title_sort retrieval of all-weather 1 km land surface temperature from combined modis and amsr2 data over the tibetan plateau
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/df63c917d5994317ae9723f4e9cd8504
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AT mohammadbasir retrievalofallweather1kmlandsurfacetemperaturefromcombinedmodisandamsr2dataoverthetibetanplateau
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