Articles | Volume 16, issue 12
https://doi.org/10.5194/tc-16-4779-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-4779-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Changes in the annual sea ice freeze–thaw cycle in the Arctic Ocean from 2001 to 2018
Long Lin
Key Laboratory of Polar Science, MNR, Polar Research Institute of
China, Shanghai, China
State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, MNR, Hangzhou, China
Key Laboratory of Polar Science, MNR, Polar Research Institute of
China, Shanghai, China
Mario Hoppmann
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und
Meeresforschung, Bremerhaven, Germany
Donald K. Perovich
Thayer School of Engineering, Dartmouth College, Dartmouth, NH, USA
Hailun He
State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, MNR, Hangzhou, China
Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China
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- A Spatiotemporal Comparison and Assessment of Multisource Satellite Derived Sea Ice Thickness in the Arctic Thinner Ice Region Y. Zhang et al. https://doi.org/10.1109/JSTARS.2024.3390618
- Effects of sea surface and air temperatures on inter-annual variations and trends of Arctic sea ice concentration in summer and autumn Q. Sun et al. https://doi.org/10.1007/s13131-026-2654-x
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- Overview of the studies on the interactions between atmosphere, sea ice, and ocean in the Arctic Ocean and its climatic effects: contributions from Chinese scientists R. Lei et al. https://doi.org/10.1007/s13131-025-2466-4
- Estimation of summer pan-Arctic ice draft from satellite passive microwave observations J. Kim et al. https://doi.org/10.1016/j.rse.2023.113662
- Mass and heat balance of sea ice during the thaw-freezing transition in the Pacific sector of Arctic Ocean derived from the buoy measurements in 2018 M. Wu et al. https://doi.org/10.1007/s13131-025-2514-0
- Effects of Freezing Temperature Parameterization on Simulated Sea‐Ice Thickness Validated by MOSAiC Observations F. Gu et al. https://doi.org/10.1029/2024GL108281
- Resiliency of Arctic sea ice to warming from southerly advection in early spring C. Cox et al. https://doi.org/10.1525/elementa.2026.00027
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- Variations in the Upper Ocean Heat Content of the Southern Canadian Basin Y. Liu et al. https://doi.org/10.3390/jmse12040667
- Predators and scavengers: Polar bears as marine carrion providers H. Gamblin et al. https://doi.org/10.1002/oik.11628
Saved (final revised paper)
Latest update: 03 Sep 2026
Short summary
Ice mass balance observations indicated that average basal melt onset was comparable in the central Arctic Ocean and approximately 17 d earlier than surface melt in the Beaufort Gyre. The average onset of basal growth lagged behind the surface of the pan-Arctic Ocean for almost 3 months. In the Beaufort Gyre, both drifting-buoy observations and fixed-point observations exhibit a trend towards earlier basal melt onset, which can be ascribed to the earlier warming of the surface ocean.
Ice mass balance observations indicated that average basal melt onset was comparable in the...