Articles | Volume 13, issue 7
https://doi.org/10.5194/tc-13-2051-2019
© Author(s) 2019. 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-13-2051-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
29 Jul 2019
Research article |
| 29 Jul 2019
| 29 Jul 2019
The 2018 North Greenland polynya observed by a newly introduced merged optical and passive microwave sea-ice concentration dataset
Institute for Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany
Gunnar Spreen
Institute for Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany
Christian Haas
Institute for Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany
Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany
Larysa Istomina
Institute for Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany
Frank Kauker
Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany
O.A.Sys – Ocean Atmosphere Systems GmbH, Tewessteg 4, 20249 Hamburg, Germany
Dmitrii Murashkin
Institute for Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, 28359 Bremen, Germany
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- Insights into German polar research during POLARSTUNDE A. Zuhr et al. 10.5194/polf-91-73-2023
- Arctic mixed-phase clouds simulated by the WRF model: Comparisons with ACLOUD radar and in situ airborne observations and sensitivity of microphysics properties D. Arteaga et al. 10.1016/j.atmosres.2024.107471
- Global Snowmelt Onset Reflects Climate Variability: Insights from Spaceborne Radiometer Observations L. Zheng et al. 10.1175/JCLI-D-21-0265.1
- A Volume‐Conserved Approach to Estimating Sea‐Ice Production in Antarctic Polynyas Y. Lin et al. 10.1029/2022GL101859
- Evaluation of a New Merged Sea-Ice Concentration Dataset at 1 km Resolution from Thermal Infrared and Passive Microwave Satellite Data in the Arctic V. Ludwig et al. 10.3390/rs12193183
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- Polar Bear Fossil and Archaeological Records from the Pleistocene and Holocene in Relation to Sea Ice Extent and Open Water Polynyas S. Crockford 10.5334/oq.107
- Recent changes in pan-Arctic sea ice, lake ice, and snow-on/off timing A. Dauginis & L. Brown 10.5194/tc-15-4781-2021
- Accelerated sea ice loss in the Wandel Sea points to a change in the Arctic’s Last Ice Area A. Schweiger et al. 10.1038/s43247-021-00197-5
- Super-Resolution-Aided Sea Ice Concentration Estimation From AMSR2 Images by Encoder–Decoder Networks With Atrous Convolution T. Feng et al. 10.1109/JSTARS.2022.3232533
- Sea Ice Production in the 2016 and 2017 Maud Rise Polynyas L. Zhou et al. 10.1029/2022JC019148
- Causes and evolution of winter polynyas north of Greenland Y. Lee et al. 10.5194/tc-17-233-2023
- Spaceborne infrared imagery for early detection of Weddell Polynya opening C. Heuzé et al. 10.5194/tc-15-3401-2021
- Multi-Year Sea Ice Conditions in the Northwest Passage: 1968–2020 S. Howell et al. 10.1080/07055900.2022.2136061
- Influence of Melt Ponds on the SSMIS-Based Summer Sea Ice Concentrations in the Arctic J. Zhao et al. 10.3390/rs13193882
- Wintertime Airborne Measurements of Ice Nucleating Particles in the High Arctic: A Hint to a Marine, Biogenic Source for Ice Nucleating Particles M. Hartmann et al. 10.1029/2020GL087770
- Ship traffic connects Antarctica’s fragile coasts to worldwide ecosystems A. McCarthy et al. 10.1073/pnas.2110303118
- Resolution enhanced sea ice concentration: a new algorithm applied to AMSR2 microwave radiometry data J. Rusin et al. 10.1017/aog.2024.6
- PMDRnet: A Progressive Multiscale Deformable Residual Network for Multi-Image Super-Resolution of AMSR2 Arctic Sea Ice Images X. Liu et al. 10.1109/TGRS.2022.3151623
- Improved machine-learning-based open-water–sea-ice–cloud discrimination over wintertime Antarctic sea ice using MODIS thermal-infrared imagery S. Paul & M. Huntemann 10.5194/tc-15-1551-2021
- Characterization of north Greenland polynyas with super-resolved passive microwave sea ice concentration X. Liu et al. 10.1080/15481603.2023.2300222
- Spatiotemporal Variability of Sea Ice in the Arctic's Last Ice Area G. Moore et al. 10.1029/2019GL083722
- Unprecedented decline of Arctic sea ice outflow in 2018 H. Sumata et al. 10.1038/s41467-022-29470-7
- Estimation of Sea Ice Production in the North Water Polynya Based on Ice Arch Duration in Winter During 2006–2019 H. Ren et al. 10.1029/2022JC018764
- Microplastics Distribution within Western Arctic Seawater and Sea Ice A. D’Angelo et al. 10.3390/toxics11090792
- The July 2019 European Heat Wave in a Warmer Climate: Storyline Scenarios with a Coupled Model Using Spectral Nudging A. Sánchez-Benítez et al. 10.1175/JCLI-D-21-0573.1
- Thinner Sea Ice Contribution to the Remarkable Polynya Formation North of Greenland in August 2018 X. Shen et al. 10.1007/s00376-021-0136-9
- Improving satellite-based monitoring of the polar regions: Identification of research and capacity gaps C. Gabarró et al. 10.3389/frsen.2023.952091
- Ice Production in Ross Ice Shelf Polynyas during 2017–2018 from Sentinel–1 SAR Images L. Dai et al. 10.3390/rs12091484
- Effects of Geophony and Anthrophony on the Underwater Acoustic Environment in the East Siberian Sea, Arctic Ocean D. Han et al. 10.1029/2021GL093097
- Concurrence of blowing snow and polynya enhances arctic surface–atmosphere interaction: a modeling study with an extreme wind event in 2018 J. Zhang et al. 10.1088/2752-5295/acb9b1
- Local and Remote Atmospheric Circulation Drivers of Arctic Change: A Review G. Henderson et al. 10.3389/feart.2021.709896
- Copernicus Marine Service Ocean State Report, Issue 4 K. von Schuckmann et al. 10.1080/1755876X.2020.1785097
1 citations as recorded by crossref.
Latest update: 29 Jun 2024
Short summary
Sea-ice concentration, the fraction of an area covered by sea ice, can be observed from satellites with different methods. We combine two methods to obtain a product which is better than either of the input measurements alone. The benefit of our product is demonstrated by observing the formation of an open water area which can now be observed with more detail. Additionally, we find that the open water area formed because the sea ice drifted in the opposite direction and faster than usual.
Sea-ice concentration, the fraction of an area covered by sea ice, can be observed from...
