Physical properties of different sea ice types at ArcticNet, CFL and CASES ice stations, eastern Beaufort Sea, supplement to: Isleifson, Dustin; Hwang, Byongjun; Barber, David G; Scharien, Randall K; Shafai, Lotfollah (2010): C-Band polarimetric backscattering signatures of newly formed sea ice during fall freeze-up. IEEE Transactions on Geoscience and Remote Sensing, 48(8), 3256-3267

• Main Authors: Isleifson, Dustin, Hwang, Byongjun, Barber, David G, Scharien, Randall K, Shafai, Lotfollah
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2010
• Subjects: International Polar Year 2007-2008 IPY; Randall; ArcticNet; Beaufort Sea; International Polar Year; IPY; Sea ice
• Online Access: https://dx.doi.org/10.1594/pangaea.811542; https://doi.pangaea.de/10.1594/PANGAEA.811542

A study of the polarimetric backscattering response of newly formed sea ice types under a large assortment of surface coverage was conducted using a ship-based C-band polarimetric radar system. Polarimetric backscattering results and physical data for 40 stations during the fall freeze-up of 2003, 2006, and 2007 are presented. Analysis of the copolarized correlation coefficient showed its sensitivity to both sea ice thickness and surface coverage and resulted in a statistically significant separation of ice thickness into two regimes: ice less than 6 cm thick and ice greater than 8 cm thick. A case study quantified the backscatter of a layer of snow infiltrated frost flowers on new sea ice, showing that the presence of the old frost flowers can enhance the backscatter by more than 6 dB. Finally, a statistical analysis of a series of temporal-spatial measurements over a visually homogeneous frost-flower-covered ice floe identified temperature as a significant, but not exclusive, factor in the backscattering measurements. : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150