Observing the evolution of summer melt on multiyear sea ice with ICESat-2 and Sentinel-2

• Published in: The Cryosphere
• Main Authors: Buckley, Ellen M., Farrell, Sinéad L., Herzfeld, Ute C., Webster, Melinda A., Trantow, Thomas, Baney, Oliwia N., Duncan, Kyle A., Han, Huilin, Lawson, Matthew
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2023
• Subjects: article; Verlagsveröffentlichung; Arctic; Sea ice; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-17-3695-2023; https://noa.gwlb.de/receive/cop_mods_00068607; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00067029/tc-17-3695-2023.pdf; https://tc.copernicus.org/articles/17/3695/2023/tc-17-3695-2023.pdf

We investigate sea ice conditions during the 2020 melt season, when warm air temperature anomalies in spring led to early melt onset, an extended melt season, and the second-lowest September minimum Arctic ice extent observed. We focus on the region of the most persistent ice cover and examine melt pond depth retrieved from Ice, Cloud, and land Elevation Satellite-2 (ICESat-2) using two distinct algorithms in concert with a time series of melt pond fraction and ice concentration derived from Sentinel-2 imagery to obtain insights about the melting ice surface in three dimensions. We find the melt pond fraction derived from Sentinel-2 in the study region increased rapidly in June, with the mean melt pond fraction peaking at 16 % ± 6 % on 24 June 2020, followed by a slow decrease to 8 % ± 6 % by 3 July, and remained below 10 % for the remainder of the season through 15 September. Sea ice concentration was consistently high (>95 %) at the beginning of the melt season until 4 July, and as floes disintegrated, it decreased to a minimum of 70 % on 30 July and then became more variable, ranging from 75 % to 90 % for the remainder of the melt season. Pond depth increased steadily from a median depth of 0.40 m ± 0.17 m in early June and peaked at 0.97 m ± 0.51 m on 16 July, even as melt pond fraction had already started to decrease. Our results demonstrate that by combining high-resolution passive and active remote sensing we now have the ability to track evolving melt conditions and observe changes in the sea ice cover throughout the summer season.