Can we extend local sea-ice measurements to satellite scale? An example from the N-ICE2015 expedition

• Published in: Annals of Glaciology
• Main Authors: Anja Rösel, Jennifer King, Anthony P. Doulgeris, Penelope M. Wagner, A. Malin Johansson, Sebastian Gerland
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2018
• Subjects: airborne electromagnetic soundings; electromagnetic induction; remote sensing; sea-ice; sea-ice classification; Meteorology. Climatology; QC851-999; Arctic; Svalbard; Annals of Glaciology; Climate change; Sea ice
• Online Access: https://doi.org/10.1017/aog.2017.37; https://doaj.org/article/92cec6abf1c34a389e9f7a461b5b9b31

Knowledge of Arctic sea-ice conditions is of great interest for Arctic residents, as well as for commercial usage, and to study the effects of climate change. Information gained from analysis of satellite data contributes to this understanding. In the course of using in situ data in combination with remotely sensed data, the question of how representative local scale measurements are of a wider region may arise. We compare in situ total sea-ice thickness measurements from the Norwegian young sea ICE expedition in the area north of Svalbard with airborne-derived total sea-ice thickness from electromagnetic soundings. A segmented and classified synthetic aperture radar (SAR) quad-pol ALOS-2 Palsar-2 satellite scene was grouped into three simplified ice classes. The area fractions of the three classes are: 11.2% ‘thin’, 74.4% ‘level’, and 14.4% ‘deformed’. The area fractions of the simplified classes from ground- and helicopter-based measurements are comparable with those achieved from the SAR data. Thus, this study shows that there is potential for a stepwise upscaling from in situ, to airborne, to satellite data, which allow us to assess whether in situ data collected are representative of a wider region as observed by satellites.