4.7 Article

Sea-Ice Permittivity Derived From GNSS Reflection Profiles: Results of the MOSAiC Expedition

Journal

Publisher

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/TGRS.2021.3121993

Keywords

Sea ice; Arctic; Sea measurements; Permittivity; Global navigation satellite system; Temperature measurement; Ocean temperature; Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition; reflectometry; satellite navigation systems; sea-ice permittivity

Funding

  1. Research Council of Norway [280292]

Ask authors/readers for more resources

Reflectometry measurements were conducted during the MOSAiC expedition to monitor the reflectivity of Arctic sea ice. The results showed that reflectivity can serve as an indicator for sea ice monitoring under certain conditions, and the results were compared with model predictions for validation. Additionally, the analysis of anomalies in sea ice profiles provided insights into factors such as ice thickness and temperature.
Reflectometry measurements have been conducted aboard the German research icebreaker Polarstern during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. Signals of Global Navigation Satellite Systems (GNSS) were recorded using a dedicated GNSS reflectometry receiver for retrieval of sea-ice reflectivity. The primary goal is reflectometry-based monitoring of sea ice as a part of the Arctic climate study. The dataset presented here covers the expedition's first leg (late September to mid-December 2019) in the Siberian Sector of the central Arctic (at about 82 degrees N to 87 degrees N). Daily profiles of reflectivity are retrieved for satellite elevations < 45 degrees. In agreement with model prediction, the results show best reflectivity contrast (about 5 dB between compact pack-ice and lower ice concentrations) for observations at left-handed circular polarization and elevation angles of 10 degrees-20 degrees. A daily resolved time series of sea-ice relative permittivity is inverted from the left-handed data. In general, the level of inversion results is at the lower limit of sea-ice values (relative permittivity of 3 and below), potentially indicating an influence of incoherent volume scattering. An occasional increase in the relative permittivity is attributed to the presence of water. Sea-ice profiles show anomalies that are confirmed by enhanced model prediction (slab reflection). A long-term comparison of prediction and retrieved profiles indicates anomalies' dependence on ice thickness and temperature.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available