TY - JOUR
T1 - Time varying spatial downscaling of satellite-based drought index
AU - Chu, Hone Jay
AU - Wijayanti, Regita Faridatunisa
AU - Jaelani, Lalu Muhamad
AU - Tsai, Hui Ping
N1 - Funding Information:
Acknowledgments: The authors would like to thank the editors and anonymous reviewers for providing suggestions of paper improvement. We are grateful for the support from SATU joint research scheme and SDGs joint research project in NCKU.
Funding Information:
The study was supported by Ministry of Education, Culture, Research, and Technology, Indonesia (3/E1/KP.PTNBH/2021; 885/PKS/ITS/2021), and Ministry of Science and Technology (MOST), Taiwan (109-2621-M-006-003-).
Funding Information:
Funding: The study was supported by Ministry of Education, Culture, Research, and Technology, Indonesia (3/E1/KP.PTNBH/2021; 885/PKS/ITS/2021), and Ministry of Science and Technology (MOST), Taiwan (109-2621-M-006 -003-).
Publisher Copyright:
© 2021 by the authors. Licensee MDPI, Basel, Switzerland.
PY - 2021/9
Y1 - 2021/9
N2 - Drought monitoring is essential to detect the presence of drought, and the comprehensive change of drought conditions on a regional or global scale. This study used satellite precipitation data from the Tropical Rainfall Measuring Mission (TRMM), but refined the data for drought monitoring in Java, Indonesia. Firstly, drought analysis was conducted to establish the standardized precipitation index (SPI) of TRMM data for different durations. Time varying SPI spatial downscaling was conducted by selecting the environmental variables, normalized difference vegetation index (NDVI), and land surface temperature (LST) that were highly correlated with precipitation because meteorological drought was associated with vegetation and land drought. This study used time-dependent spatial regression to build the relation among original SPI, auxiliary variables, i.e., NDVI and LST. Results indicated that spatial downscaling was better than nonspatial downscaling (overall RMSEs: 0.25 and 0.46 in spatial and nonspatial downscaling). Spatial downscaling was more suitable for heterogeneous SPI, particularly in the transition time (R: 0.863 and 0.137 in June 2019 for spatial and nonspatial models). The fine resolution (1 km) SPI can be composed of the environmental data. The fine-resolution SPI captured a similar trend of the original SPI. Furthermore, the detailed SPI maps can be used to understand the spatio-temporal pattern of drought severity.
AB - Drought monitoring is essential to detect the presence of drought, and the comprehensive change of drought conditions on a regional or global scale. This study used satellite precipitation data from the Tropical Rainfall Measuring Mission (TRMM), but refined the data for drought monitoring in Java, Indonesia. Firstly, drought analysis was conducted to establish the standardized precipitation index (SPI) of TRMM data for different durations. Time varying SPI spatial downscaling was conducted by selecting the environmental variables, normalized difference vegetation index (NDVI), and land surface temperature (LST) that were highly correlated with precipitation because meteorological drought was associated with vegetation and land drought. This study used time-dependent spatial regression to build the relation among original SPI, auxiliary variables, i.e., NDVI and LST. Results indicated that spatial downscaling was better than nonspatial downscaling (overall RMSEs: 0.25 and 0.46 in spatial and nonspatial downscaling). Spatial downscaling was more suitable for heterogeneous SPI, particularly in the transition time (R: 0.863 and 0.137 in June 2019 for spatial and nonspatial models). The fine resolution (1 km) SPI can be composed of the environmental data. The fine-resolution SPI captured a similar trend of the original SPI. Furthermore, the detailed SPI maps can be used to understand the spatio-temporal pattern of drought severity.
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U2 - 10.3390/rs13183693
DO - 10.3390/rs13183693
M3 - Article
AN - SCOPUS:85115163988
SN - 2072-4292
VL - 13
JO - Remote Sensing
JF - Remote Sensing
IS - 18
M1 - 3693
ER -