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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 1
The Cryosphere, 10, 149-158, 2016
https://doi.org/10.5194/tc-10-149-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 149-158, 2016
https://doi.org/10.5194/tc-10-149-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 19 Jan 2016

Research article | 19 Jan 2016

Sea ice cover in Isfjorden and Hornsund, Svalbard (2000–2014) from remote sensing data

S. Muckenhuber1, F. Nilsen2,3, A. Korosov1, and S. Sandven1 S. Muckenhuber et al.
  • 1Nansen Environmental and Remote Sensing Center (NERSC), Thormøhlensgate 47, 5006 Bergen, Norway
  • 2University Centre in Svalbard (UNIS), P.O. Box 156, 9171 Longyearbyen, Norway
  • 3Geophysical Institute, University of Bergen, P.O. Box 7800, 5020 Bergen, Norway

Abstract. A satellite database including 16555 satellite images and ice charts displaying the area of Isfjorden, Hornsund, and the Svalbard region has been established with focus on the time period 2000–2014. 3319 manual interpretations of sea ice conditions have been conducted, resulting in two time series dividing the area of Isfjorden and Hornsund into "fast ice" (sea ice attached to the coastline), "drift ice", and "open water". The maximum fast ice coverage of Isfjorden is  > 40% in the periods 2000–2005 and 2009–2011 and stays  < 30% in 2006–2008 and 2012–2014. Fast ice cover in Hornsund reaches  > 40% in all considered years, except for 2012 and 2014, where the maximum stays  < 20%. The mean seasonal cycles of fast ice in Isfjorden and Hornsund show monthly averaged values of less than 1% between July and November and maxima in March (Isfjorden, 35.7%) and April (Hornsund, 42.1%), respectively. A significant reduction of the monthly averaged fast ice coverage is found when comparing the time periods 2000–2005 and 2006–2014. The seasonal maximum decreases from 57.5 to 23.2% in Isfjorden and from 52.6 to 35.2% in Hornsund. A new index, called "days of fast ice" (DFI), is introduced for quantification of the interannual variation of fast ice cover, allowing for comparison between different fjords and winter seasons. Considering the time period from 1 March until end of the sea ice season, the mean DFI values for 2000–2014 are 33.1±18.2DFI (Isfjorden) and 42.9±18.2DFI (Hornsund). A distinct shift to lower DFI values is observed in 2006. Calculating a mean before and after 2006 yields a decrease from 50 to 22DFI for Isfjorden and from 56 to 34DFI for Hornsund. Fast ice coverage generally correlates well with remote-sensing sea surface temperature and in situ air temperature. An increase of autumn ocean heat content is observed during the last few years when the DFI values decrease. The presented sea ice time series can be utilized for various climate effect studies linked to, e.g. glacier dynamics, ocean chemistry, and marine biology.

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Sea ice conditions in two fjords of Spitsbergen (Isfjorden, Hornsund) have been investigated between 2000-2014 using manual interpretation of 16555 satellite images. The result is two time series dividing the fjord area into "fast ice", "drift ice", and "open water". A significant reduction of fast ice coverage has been found comparing the time periods 2000-2005 and 2006-2014. A new concept, called "days of fast ice coverage" (DFI), is introduced for quantification of fast ice cover.
Sea ice conditions in two fjords of Spitsbergen (Isfjorden, Hornsund) have been investigated...
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