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

Abstract

Reflectometry measurements have been conducted aboard the German research icebreaker Polarstern during the MOSAiC expedition (Multidisciplinary drifting Observatory for the Study of Arctic Climate).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 a reflectometry-based monitoring of sea ice as part of the Arctic climate study. The data set presented here covers the expedition's first leg (late Sep. to mid Dec. 2019) in the Siberian Sector of the central Arctic (at about 82 • N to 87 • N). Daily profiles of reflectivity are retrieved for satellite elevations < 45 • . 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 • to 20 • . 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 (rel. permittivity of 3 and below), potentially indicating an influence of incoherent volume scattering. Occasional increase of 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.

Overview of the MOSAiC expedition: Snow and sea ice

“…First results with a focus on snow and sea ice conditions have been published, for example, on the history of the ice drift prior to the MOSAiC expedition , on the ice conditions from satellite observation along the drift track in previous years (Krumpen et al, 2021), on the representativeness of the selected ice floe (Belter et al, 2021), on the linkages to the general atmospheric circulation (Dethloff et al, 2021), on sea ice RS methods (Munoz-Martin et al, 2020;Stroeve et al, 2020;Semmling et al, 2021), and on the platelet ice accumulation in winter (Katlein et al, 2020).…”

Ionosphere Sounding in the Central Arctic: Preliminary Results of the Multidisciplinary Drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition

“…We investigate the space weather impact on global navigation satellite system (GNSS) data recorded on a ship in the central Arctic. The study is linked to the expedition of the German research icebreaker Polarstern, [1] as part of Multidisciplinary Drifting Observatory for the Study of Arctic Climate (MOSAiC) [2], and is part in a series of studies focusing on GNSS for remote sensing application within MOSAiC and previous scientific cruises to the Arctic: for atmospheric sounding [3,4] and for sea ice characterization [5][6][7]. An ionospheric sounding approach is used to detect space weather-induced scintillations as described by [8].…”