An UWB UHF Ice-Penetreating Radar for the Thwaites Melt Project

As a part of the project "Melting at Thwaites grounding zone and its control on sea level" (MELT), we developed a compact 750-MHz ice-penetrating radar for phase-sensitive measurements to infer basal melt and ice layer displacement using multiple passes. The radar operates with 300-MHz ban...

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Bibliographic Details
Published in:IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium
Main Authors: Rodriguez-Morales, F., Paden, J., Escalera Mendoza, A. S., Hale, R., Karidi, K. T., Schroeder, B., Shang, J., Talasila, H., Robinson, C., Jordan, T., Nicholls, K.
Format: Article in Journal/Newspaper
Language:unknown
Published: IEEE 2024
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Online Access:http://nora.nerc.ac.uk/id/eprint/537979/
https://doi.org/10.1109/IGARSS53475.2024.10642054
Description
Summary:As a part of the project "Melting at Thwaites grounding zone and its control on sea level" (MELT), we developed a compact 750-MHz ice-penetrating radar for phase-sensitive measurements to infer basal melt and ice layer displacement using multiple passes. The radar operates with 300-MHz bandwidth and a peak output power of 400 W. It is equipped with a small antenna array designed to fit within the limited space underneath the floor of a Twin Otter aircraft (without out-of-mold-line protuberances). The radar was installed and deployed onboard a Twin Otter airplane from the British Antarctic Survey (BAS) as a part of the ongoing International Thwaites Glacier Collaboration (ITGC). We conducted multiple radar survey flights during two consecutive austral summer seasons, collecting ~5 TB of raw data. In this paper, we present an overview of the radar system and antenna implementations. We provide a summary of our field operations and present sample data products to illustrate the instrument capabilities to sound ice as thick as ~1,400 m and map internal reflecting horizons near the grounding line of TG with sub-m vertical resolution. We also discuss the utility of our repeat pass data for inferring ice shelf basal melt rates.