Monitoring ice flow velocity of Petermann glacier combined with Sentinel-1 and −2 imagery

• Published in: International Journal of Applied Earth Observation and Geoinformation
• Main Authors: Gang Li, Yanting Mao, Xiaoman Feng, Zhuoqi Chen, Zhibin Yang, Xiao Cheng
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2023
• Subjects: Glacier velocity; Sentinel-1; Sentinel-2; Greenland ice sheet; Offset-tracking; SBAS; Physical geography; GB3-5030; Environmental sciences; GE1-350; Greenland; glacier; Ice Sheet; National Snow and Ice Data Center; Petermann glacier
• Online Access: https://doi.org/10.1016/j.jag.2023.103374; https://doaj.org/article/f404353dddd24272a3270892346fe025

Synthetic Aperture Radar (SAR) images are commonly used to monitor glacier flow velocity at Greenland Ice Sheet (GrIS). However, offset-tracking with SAR imagery in summer usually show poor quality because the rapid ice surface freezing-melting cycles contaminating the surface backscattering characteristic, while optical images are less sensitive to this phenomenon. In this study, we combine Sentinel-1 and -2 images to create the glacier velocity time series for the Petermann glacier, located in the northern GrIS. Firstly, the offset-tracking technique is employed to acquire the initial deformation fields with SAR and optical sensors separately, each SAR and/or optical acquisition is tracked with its closest next three acquisitions. Next, after removing the bad matchings, the least squares method based on connected components is employed to calculate the time series of glacier velocity for Sentinel-1 and −2, separately. Finally, these two kinds of derived time series are integrated with a weighted least squares method, where weights are evaluated according to the estimated RMSEs in the last step. Error propagation analysis suggests RMSEs of the single pair of Sentinel-1 and −2 images offset-tracking are ∼ 0.22 m and ∼ 2.5 m for Petermann glaciers. Standard deviation of the difference between Sentinel-1 and Sentinel-2 measured velocity are ∼ 0.25 m/day. Compared with 6-day velocity fields product, NSIDC (National Snow and Ice Data Center) −0766, which is only derived with Sentinel-1observations, our results show good agreement and less defects in summer. The differences are ∼ 0.20 m/day in non-melting seasons and ∼ 0.34 m/day in summer. Longitudinal velocity differences growing in 2019 and 2020 at ∼ 20 Km up to the terminus are consistency with the crevasse expansion, indicating another calving event is approaching. This research finds that the fusion of Sentinel-1 and −2 offset-tracking results improves the completeness of the ice movement time series for polar glaciers.