The Cryosphere
The Cryosphere
TC
Articles | Volume 17, issue 7
Articles | Volume 17, issue 7
https://doi.org/10.5194/tc-17-2871-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-17-2871-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 17, issue 7
Research article
 | 
18 Jul 2023
Research article |  | 18 Jul 2023

A climatology of thermodynamic vs. dynamic Arctic wintertime sea ice thickness effects during the CryoSat-2 era

James Anheuser, Yinghui Liu, and Jeffrey R. Key

Data sets

A climatology of thermodynamic vs. dynamic Arctic wintertime sea ice thickness effects during the CryoSat-2 era: Data James Anheuser, Yinghui Liu, and Jeff Key https://doi.org/10.5281/zenodo.7987917

Drift trajectory of the site M1 of the Distributed Network of MOSAiC 2019/2020 Marcel Nicolaus, Kathrin Riemann-Campe, Angela Bliss, Jennifer K. Hutchings, Mats A. Granskog, Christian Haas, Mario Hoppmann, Torsten Kanzow, Richard A. Krishfield, Ruibo Lei, Markus Rex, Tao Li, and Benjamin Rabe https://doi.org/10.1594/PANGAEA.937193

Model code and software

A climatology of thermodynamic vs. dynamic Arctic wintertime sea ice thickness effects during the CryoSat-2 era: Code James Anheuser https://doi.org/10.5281/zenodo.7987926

CryoSat-SMOS Merged Sea Ice Thickness L. Kaleschke, S. Hendricks, X. Tian-Kunze, and R. Ricker https://spaces.awi.de/display/CS2SMOS/CryoSat-SMOS+Merged+Sea+Ice+Thickness

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Short summary
Sea ice parcels may experience thickness changes primarily through two processes: due to freezing or melting or due to motion relative to other parcels. These processes are independent and will be affected differently in a changing climate. In order to better understand these processes and compare them against models, observational estimates of these process independent from one another are necessary. We present a large spatial- and temporal-scale observational estimate of these processes.
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