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Downscaling MODIS Land Surface Temperature Product Using an Adaptive Random Forest Regression Method and Google Earth Engine for a 19-Years Spatiotemporal Trend Analysis Over Iran
被引:47
作者:
Ebrahimy, Hamid
[1
]
Aghighi, Hossein
[1
]
Azadbakht, Mohsen
[1
]
Amani, Meisam
[2
]
Mahdavi, Sahel
[2
]
Matkan, Ali Akbar
[1
]
机构:
[1] Shahid Beheshti Univ, Fac Earth Sci, Ctr Remote Sensing & GIS Res, Tehran 1983969411, Iran
[2] Wood Environm & Infrastruct Solut, Ottawa, ON K2E 7L5, Canada
关键词:
Land surface temperature;
Spatiotemporal phenomena;
Earth;
Market research;
MODIS;
Remote sensing;
Meteorology;
Adaptive random forest;
downscaling;
Google Earth Engine (GEE);
land surface temperature (LST);
trend analysis;
VARIABILITY;
LST;
VALIDATION;
DISAGGREGATION;
RESOLUTION;
DROUGHT;
IMAGERY;
EUROPE;
BASIN;
CYCLE;
D O I:
10.1109/JSTARS.2021.3051422
中图分类号:
TM [电工技术];
TN [电子技术、通信技术];
学科分类号:
0808 ;
0809 ;
摘要:
MODIS land surface temperature (LST) product (MOD11A1) has been widely used in analysing spatiotemporal trends of LST. However, its applicability is limited, partially due to its coarse spatial resolution (i.e., 1 km). In this study, an Adaptive random forest regression (ARFR) method was developed for LST downscaling at national scale. This study also provided a framework to shift from downscaling single-time image sets to extensive time-series of MOD11A1 LST images in an operational approach (i.e., a 19-years spatiotemporal LST trend analysis over Iran) using the Google Earth Engine (GEE) cloud computing platform. The performance of ARFR was assessed by comparing the results of the downscaled LSTs with the Landsat-8 LST data on different dates of six consecutive years (2014-2019) over ten different sub-areas in Iran. The results demonstrated the effectiveness of the proposed method with an average root mean square error and mean absolute error of 2.22 degrees C and 1.59 degrees C, respectively. The results of spatiotemporal LST trend analysis showed that 25.08%, 10.05%, 56.68%, 1.04%, and 32.84% of Iran experienced significant positive trends during a full year, spring, summer, fall, and winter, respectively. Significant negative trends were also observed over the 3.09%, 23.84%, 7.54%, 17.38%, and 18.77% of Iran during a full year, spring, summer, fall, and winter, respectively. In summary, the outcomes of this study not only exhibit the spatiotemporal trends of LST across Iran, but also reveal the substantial benefits of the ARFR method in downscaling LST using GEE.
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页码:2103 / 2112
页数:10
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