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The Cryosphere An interactive open-access journal of the European Geosciences Union
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In October 2019 the research vessel Polarstern was moored to an ice floe in order to travel with it on the 1-year-long MOSAiC journey through the Arctic. Here we provide historical context of the floe's evolution and initial state for upcoming studies. We show that the ice encountered on site was exceptionally thin and was formed on the shallow Siberian shelf. The analyses presented provide the initial state for the analysis and interpretation of upcoming biogeochemical and ecological studies.
TC | Articles | Volume 14, issue 7
The Cryosphere, 14, 2173–2187, 2020
https://doi.org/10.5194/tc-14-2173-2020
The Cryosphere, 14, 2173–2187, 2020
https://doi.org/10.5194/tc-14-2173-2020

Research article 06 Jul 2020

Research article | 06 Jul 2020

The MOSAiC ice floe: sediment-laden survivor from the Siberian shelf

Thomas Krumpen et al.

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Cited articles

AARI: Guidance to Special Shipborne Ice Observations, Technical Report, Arctic and Antarctic Research Insitute (AARI), Saint-Petersburg, Russia, 2011. 
Alekseeva, T., Tikhonov, V., Frolov, S., Repina, I., Raev, M., Sokolova, J., Sharkov, E., Afanasieva, E., and Serovetnikov, S.: Comparison of Arctic Sea Ice Concentration from the NASA Team, ASI, and VASIA2 Algorithms with Summer and Winter Ship Data, Remote Sensing, 11, 2481, https://doi.org/h10.3390/rs11212481, 2019. 
Bitz, C. M. and Lipscomb, W. H.: An energy-conserving thermodynamic sea ice model for climate study, J. Geophys. Res.-Oceans, 104, C7, https://doi.org/10.1029/1999JC900100, 1999. 
CICE Consortium Icepack: Icepack version 1.1.0, Zenodo, https://doi.org/10.5281/zenodo.1213462, 2020. 
Damm, E., Bauch, D., Krumpen, T., Rabe, B., Korhonen, M., Vinogradova, E., and Uhlig, C.: The Transpolar Drift conveys methane from the Siberian Shelf to the central Arctic Ocean, Sci. Rep., 8, 4515, https://doi.org/10.1038/s41598-018-22801-z, 2018. 
Publications Copernicus
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Short summary
In October 2019 the research vessel Polarstern was moored to an ice floe in order to travel with it on the 1-year-long MOSAiC journey through the Arctic. Here we provide historical context of the floe's evolution and initial state for upcoming studies. We show that the ice encountered on site was exceptionally thin and was formed on the shallow Siberian shelf. The analyses presented provide the initial state for the analysis and interpretation of upcoming biogeochemical and ecological studies.
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