Airborne sea ice parameters during aircraft flight P6_217_ICEBIRD_2019_1904020901, Version 2 ...

• Main Authors: Jutila, Arttu, Hendricks, Stefan, Ricker, Robert, von Albedyll, Luisa, Haas, Christian
• Format: Dataset
• Language: unknown
• Published: PANGAEA 2024
• Subjects: Arctic Ocean; Cryosphere; Freeboard; Sea ice; Sea ice density; Sea ice thickness; snow depth; DATE/TIME; LATITUDE; LONGITUDE; Sea ice and snow thickness; Sea ice and snow thickness, uncertainty; Snow thickness; Snow thickness, uncertainty; Snow thickness, standard deviation; Snow thickness, minimum; Snow thickness, maximum; Number of observations; Snow freeboard; Snow freeboard, uncertainty; Snow freeboard, standard deviation; Snow freeboard, minimum; Snow freeboard, maximum; Surface temperature; Surface temperature, standard deviation; Surface temperature, minimum; Surface temperature, maximum; Sea ice freeboard; Density, ice; Density, ice, uncertainty; Sea ice, age; Ice type; Quality flag; Aircraft; Airborne electromagnetic EM induction sounding; Airborne ultrawideband radar; Calculated; Airborne Laserscanner ALS RIEGL VQ580; Infrared radiation pyrometer, Heitronics, KT19.85II; P6-217_ICEBIRD_2019; POLAR 6; Airborne surveys to collect measurements of sea ice thickness in the Arctic AWI_IceBird; Sea Ice Physics @ AWI AWI_SeaIce; Arctic; Beaufort Sea; Lincoln Sea; ice covered areas
• Online Access: https://dx.doi.org/10.1594/pangaea.966058; https://doi.pangaea.de/10.1594/PANGAEA.966058

Airborne multi-instrument measurements of sea ice were made in April 2019 during the winter campaign of the AWI IceBird campaign series. The data consist of five surveys spanning sea-ice covered areas in the Lincoln Sea, Central Arctic Ocean, as well as the Beaufort Sea. For each flight, the geolocated total (ice+snow) thickness data from an airborne electromagnetic (EM) induction sensor are provided with a point spacing of approximately 5-6 meters. Larger gaps in the trajectories arise from high-altitude calibrations of the EM sensor. The data are combined with collocated and simultaneous snow depth measurements from an airborne frequency-modulated continuous-wave ultrawideband radar, snow freeboard measurements from an airborne near-infrared laser scanner, and surface temperature measurements from an airborne infrared radiation pyrometer. Each value represents the average within the approximately 40 m diameter footprint of the EM sensor, thus representing a smoothed representation. These values are then ...