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Ice extent in sub-arctic fjords and coastal areas from 2001 to 2019 analyzed from MODIS imagery

Permanent link
https://hdl.handle.net/10037/18540
DOI
https://doi.org/10.1017/aog.2020.34
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Date
2020-06-03
Type
Journal article
Tidsskriftartikkel
Peer reviewed

Author
O'Sadnick, Megan; Petrich, Christian; Brekke, Camilla; Skarðhamar, Jofrid
Abstract
Results examining variations in the ice extent along the Norwegian coastline based on the analysis of Moderate Resolution Imaging Spectroradiometer (MODIS) images from 2001 to 2019, February through May, are presented. A total of 386 fjords and coastal areas were outlined and grouped into ten regions to assess seasonal and long-term trends in ice extent. In addition, three fjords were examined to investigate how ice extent may vary over short distances (<100 km). Of the 386 outlined, 47 fjords/coastal areas held >5 km2 of ice at least once between 2001 and 2019. Over this span of time, no statistically significant trend in ice extent is found for all ten regions; however, variations between regions and years are evident. Ice extent is assessed through comparison to three weather variables – freezing degree days (FDD), daily new snowfall and daily freshwater supply from rainfall plus snowmelt. Six out of ten regions are significantly positively correlated (p < 0.05) to FDD. In addition, ice in two regions is significantly positively correlated to daily new snowfall, and in one region negatively correlated to rainfall plus snowmelt. The importance of fjord geometry and bathymetry as well as other weather variables including wind is discussed.
Is part of
O'Sadnick, M. (2022). Ice in Norwegian subarctic fjords and coastal regions: An examination of ice formation, properties, and trends based on remote sensing and in situ data. (Doctoral thesis). https://hdl.handle.net/10037/26462
Publisher
Cambridge University Press
Citation
Megan, Christian, Brekke C, Jofrid. Ice extent in sub-arctic fjords and coastal areas from 2001-19 analysed from MODIS imagery. Annals of Glaciology. 2020:1-17
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