Authors

Marcel Nicolaus, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Donald K. Perovich, Thayer School of Engineering at Dartmouth
Gunnar Spreen, Universität Bremen
Mats A. Granskog, Norsk Polarinstitutt
Luisa von Albedyll, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Michael Angelopoulos, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Philipp Anhaus, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Stefanie Arndt, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
H. Jakob Belter, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Vladimir Bessonov, Arctic and Antarctic Research Institute
Gerit Birnbaum, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Jörg Brauchle, Deutsches Zentrum für Luft- und Raumfahrt (DLR)
Radiance Calmer, University of Colorado Boulder
Estel Cardellach, Instituto de Estudios Espaciales de Cataluña
Bin Cheng, Finnish Meteorological Institute
David Clemens-Sewall, Thayer School of Engineering at Dartmouth
Ruzica Dadic, Victoria University of Wellington
Ellen Damm, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Gijs de Boer, University of Colorado Boulder
Oguz Demir, The Ohio State University
Klaus Dethloff, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Dmitry V. Divine, Norsk Polarinstitutt
Allison A. Fong, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Steven Fons, NASA Goddard Space Flight Center
Markus M. Frey, British Antarctic Survey
Niels Fuchs, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Carolina Gabarró, CSIC - Instituto de Ciencias del Mar (ICM)
Sebastian Gerland, Norsk Polarinstitutt
Helge F. Goessling, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Rolf Gradinger, UiT Norges Arktiske Universitet
Jari Haapala, Finnish Meteorological Institute
Christian Haas, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Jonathan Hamilton, University of Colorado Boulder
Henna Reetta Hannula, Finnish Meteorological Institute
Stefan Hendricks, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Andreas Herber, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung

Document Type

Article

Date of Original Version

2-7-2022

Abstract

Year-round observations of the physical snow and ice properties and processes that govern the ice pack evolution and its interaction with the atmosphere and the ocean were conducted during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition of the research vessel Polarstern in the Arctic Ocean from October 2019 to September 2020. This work was embedded into the interdisciplinary design of the 5 MOSAiC teams, studying the atmosphere, the sea ice, the ocean, the ecosystem, and biogeochemical processes. The overall aim of the snow and sea ice observations during MOSAiC was to characterize the physical properties of the snow and ice cover comprehensively in the central Arctic over an entire annual cycle. This objective was achieved by detailed observations of physical properties and of energy and mass balance of snow and ice. By studying snow and sea ice dynamics over nested spatial scales from centimeters to tens of kilometers, the variability across scales can be considered. On-ice observations of in situ and remote sensing properties of the different surface types over all seasons will help to improve numerical process and climate models and to establish and validate novel satellite remote sensing methods; the linkages to accompanying airborne measurements, satellite observations, and results of numerical models are discussed. We found large spatial variabilities of snow metamorphism and thermal regimes impacting sea ice growth. We conclude that the highly variable snow cover needs to be considered in more detail (in observations, remote sensing, and models) to better understand snow-related feedback processes. The ice pack revealed rapid transformations and motions along the drift in all seasons. The number of coupled ice–ocean interface processes observed in detail are expected to guide upcoming research with respect to the changing Arctic sea ice.

Publication Title, e.g., Journal

Elementa

Volume

10

Issue

1

Creative Commons License

Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.

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