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Author Spotlight: A Stable Phantom Material for Optical and Acoustic Imaging
Published on: June 16, 2023
Direct inference of first-year sea ice thickness using broadband acoustic backscattering
Christopher Bassett1, Andone C Lavery2, Anthony P Lyons3
1Applied Physics Laboratory, University of Washington, 1013 Northeast 40th Street, Seattle, Washington 98105, USA.
Acoustic techniques offer a novel method for measuring sea ice thickness. This study validates a broadband acoustic approach, providing accurate sea ice thickness estimates independent of water depth.
Area of Science:
- Geophysics
- Climate Science
- Oceanography
Background:
- Accurate sea ice thickness measurements are crucial for climate change research, maritime safety, and Arctic community resilience.
- Current methods for measuring sea ice thickness are often invasive (ice cores) or indirect (altimetry, sonar, electromagnetic techniques), limiting regular, widespread assessment.
- Remote sensing of sea ice thickness remains a significant challenge in polar regions.
Purpose of the Study:
- To explore the viability of broadband acoustic techniques as an alternative method for measuring total sea ice thickness.
- To develop and validate a time-domain acoustic model for sea ice thickness estimation.
- To investigate optimal acoustic frequencies for in situ sea ice thickness measurements.
Main Methods:
- Laboratory-grown sea ice samples were used to compare acoustic thickness estimations with traditional ice core measurements.
- A time-domain acoustic model was developed to simulate scattering mechanisms and invert echo time delays (water-ice and ice-air interfaces) for thickness.
- Experimental measurements were compared with model predictions to validate the acoustic technique.
Main Results:
- Acoustic thickness estimations derived from the time delay between water-ice and ice-air echoes showed good agreement with ice core measurements.
- The developed time-domain model accurately captured dominant scattering mechanisms relevant to sea ice.
- The acoustic method successfully decoupled sea ice thickness estimates from variations in water column properties.
Conclusions:
- Broadband acoustic techniques show significant promise for accurate, non-invasive measurement of total sea ice thickness.
- This method offers an alternative to traditional techniques and can potentially be integrated with ice draft measurements.
- Further research into optimal frequencies can enhance the in situ application of acoustic sea ice thickness monitoring.
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