TY - GEN
T1 - The Use of MODIS and Sentinel-1 Data Fusion to Estimate Precipitable Water Vapor Values
AU - Hayati, Noorlaila
AU - Putri, Shaza Flanetta
AU - Bamahry, Fikri
AU - Sumantyo, Josaphat Tetuko Sri
AU - Bioresita, Filsa
N1 - Publisher Copyright:
©2023 IEEE.
PY - 2023
Y1 - 2023
N2 - Precipitable Water Vapor (PWV) describes the amount of water vapor in the atmosphere that potentially becomes rain. Along with the development of the space geodetic technique, water vapor can be observed using the remote sensing technology. This research uses an integration of active and optical remote sensing data which are Sentinel-1 and MODIS. Since interferogram generated by Sentinel-1 SAR images contains tropospheric delay, it can be substracted as Short Wavelength Delay (SWD) which a part of PWV value. Furthermore, the absolute PWV value is obtained by extracting parameters from MODIS atmosphere level-2. MODIS provides PWV values for reconstructing the Elevation Dependent Delay (EDD) and Long Wavelength Delay (LWD) components. We used 118 epochs to represent the rainy and dry seasons between March 2017-February 2021. The result shows that a maximum absolute PWV value of 68 mm occurred on 22/2/2020 which belongs to the time of rainy season. The estimation recorded a minimum PWV value of 20 mm on 7/6/2017 and 14/6/2018. June is when Indonesia usually experiences a dry season. Generally, the maximum and minimum daily average absolute PWV values are 68.6845 mm and 1.5884 mm, respectively.
AB - Precipitable Water Vapor (PWV) describes the amount of water vapor in the atmosphere that potentially becomes rain. Along with the development of the space geodetic technique, water vapor can be observed using the remote sensing technology. This research uses an integration of active and optical remote sensing data which are Sentinel-1 and MODIS. Since interferogram generated by Sentinel-1 SAR images contains tropospheric delay, it can be substracted as Short Wavelength Delay (SWD) which a part of PWV value. Furthermore, the absolute PWV value is obtained by extracting parameters from MODIS atmosphere level-2. MODIS provides PWV values for reconstructing the Elevation Dependent Delay (EDD) and Long Wavelength Delay (LWD) components. We used 118 epochs to represent the rainy and dry seasons between March 2017-February 2021. The result shows that a maximum absolute PWV value of 68 mm occurred on 22/2/2020 which belongs to the time of rainy season. The estimation recorded a minimum PWV value of 20 mm on 7/6/2017 and 14/6/2018. June is when Indonesia usually experiences a dry season. Generally, the maximum and minimum daily average absolute PWV values are 68.6845 mm and 1.5884 mm, respectively.
KW - Long Wavelength Delay
KW - MODIS Level-2
KW - PS-InSAR
KW - Precipitable Water Vapor
UR - http://www.scopus.com/inward/record.url?scp=85184655252&partnerID=8YFLogxK
U2 - 10.1109/APSAR58496.2023.10388947
DO - 10.1109/APSAR58496.2023.10388947
M3 - Conference contribution
AN - SCOPUS:85184655252
T3 - APSAR 2023 - 2023 8th Asia-Pacific Conference on Synthetic Aperture Radar
BT - APSAR 2023 - 2023 8th Asia-Pacific Conference on Synthetic Aperture Radar
PB - Institute of Electrical and Electronics Engineers Inc.
T2 - 8th Asia-Pacific Conference on Synthetic Aperture Radar, APSAR 2023
Y2 - 23 October 2023 through 27 October 2023
ER -