Articles | Volume 15, issue 2
https://doi.org/10.5194/tc-15-883-2021
© Author(s) 2021. 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-15-883-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Trends and spatial variation in rain-on-snow events over the Arctic Ocean during the early melt season
College of Resources and Environment, University of Chinese Academy of
Sciences, Beijing 100049, China
Cunde Xiao
State Key Laboratory of Earth Surface Processes and Resource Ecology,
Beijing Normal University, Beijing 100875, China
Jiping Liu
Department of Atmospheric and Environmental Sciences, University at
Albany, State University of New York, Albany, NY, USA
Qiang Wang
Alfred Wegener Institute Helmholtz Centre for Polar and Marine
Research, Bremerhaven, Germany
Shifeng Pan
College of atmospheric science, Nanjing University of Information
Science & Technology, Nanjing 210044, China
Physical Oceanography Laboratory, Ocean University of China, 238
Songling Road, Qingdao 266100, China
Xiaojun Yuan
Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W,
Palisades, NY 10964, USA
Minghu Ding
Institute of Tibetan Plateau and Polar Meteorology, Chinese Academy of
Meteorological Sciences, Beijing 100081, China
Feng Zhang
Institute of Atmospheric Sciences, Fudan University, Shanghai 200438,
China/Shanghai Qi Zhi Institute, Shanghai 200232, China
Kai Xue
College of Resources and Environment, University of Chinese Academy of
Sciences, Beijing 100049, China
Peter A. Bieniek
International Arctic Research Center, University of Alaska Fairbanks,
Fairbanks, AK 99775-7340, USA
Hajo Eicken
International Arctic Research Center, University of Alaska Fairbanks,
Fairbanks, AK 99775-7340, USA
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- An Explainable Deep Learning Model for Daily Sea Ice Concentration Forecast Y. Li et al. 10.1109/TGRS.2024.3386930
- Combined effects of temperature and precipitation on the spring runoff generation process in a seasonal freezing agricultural watershed Q. Zhao et al. 10.1007/s12665-021-09777-2
- Snow depth retrieval using GPS signal-to-noise ratio data based on improved complete ensemble empirical mode decomposition Q. Wu et al. 10.1007/s10291-023-01537-y
- Southward migration of the zero-degree isotherm latitude over the Southern Ocean and the Antarctic Peninsula: Cryospheric, biotic and societal implications S. González-Herrero et al. 10.1016/j.scitotenv.2023.168473
- Trends and spatial variations of rain-on-snow events over the High Mountain Asia T. Yang et al. 10.1016/j.jhydrol.2022.128593
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- An analysis of the characteristics of precipitation in the Northeast passage and its relationship with sea ice M. Cheng et al. 10.3389/fenvs.2022.890787
17 citations as recorded by crossref.
- Contribution of warm and moist atmospheric flow to a record minimum July sea ice extent of the Arctic in 2020 Y. Liang et al. 10.5194/tc-16-1107-2022
- Estimated changes in different forms of precipitation (snow, sleet, and rain) across China: 1961–2016 B. Su et al. 10.1016/j.atmosres.2022.106078
- Critical Factors Affecting Water and Nitrogen Losses from Sloping Farmland during the Snowmelt Process Q. Zhao et al. 10.3390/agronomy13020350
- Modeling pan-Arctic seasonal and interannual landfast sea ice thickness and snow depth between 1979 and 2021 Z. Wang et al. 10.1080/17538947.2024.2376253
- Assessment of ERA5 and ERA-Interim in Reproducing Mean and Extreme Climates over West Africa I. Gbode et al. 10.1007/s00376-022-2161-8
- An intercomparison of empirical schemes for partitioning precipitation phase J. Hu et al. 10.1016/j.ejrh.2024.101757
- More Frequent, Intense, and Extensive Rainfall Events in a Strongly Warming Arctic T. Dou et al. 10.1029/2021EF002378
- Rain on snow (ROS) understudied in sea ice remote sensing: a multi-sensor analysis of ROS during MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) J. Stroeve et al. 10.5194/tc-16-4223-2022
- Performance of climate reanalyses in the determination of pan-Arctic terrestrial rain-on-snow events J. Tao et al. 10.1016/j.accre.2023.08.002
- Wintertime extreme warming events in the high Arctic: characteristics, drivers, trends, and the role of atmospheric rivers W. Ma et al. 10.5194/acp-24-4451-2024
- An Explainable Deep Learning Model for Daily Sea Ice Concentration Forecast Y. Li et al. 10.1109/TGRS.2024.3386930
- Combined effects of temperature and precipitation on the spring runoff generation process in a seasonal freezing agricultural watershed Q. Zhao et al. 10.1007/s12665-021-09777-2
- Snow depth retrieval using GPS signal-to-noise ratio data based on improved complete ensemble empirical mode decomposition Q. Wu et al. 10.1007/s10291-023-01537-y
- Southward migration of the zero-degree isotherm latitude over the Southern Ocean and the Antarctic Peninsula: Cryospheric, biotic and societal implications S. González-Herrero et al. 10.1016/j.scitotenv.2023.168473
- Trends and spatial variations of rain-on-snow events over the High Mountain Asia T. Yang et al. 10.1016/j.jhydrol.2022.128593
- Modeling ringed seal Pusa hispida habitat and lair emergence timing in the eastern Bering and Chukchi Seas J. Lindsay et al. 10.3354/esr01140
- An analysis of the characteristics of precipitation in the Northeast passage and its relationship with sea ice M. Cheng et al. 10.3389/fenvs.2022.890787
Latest update: 07 Nov 2024
Short summary
Rain-on-snow (ROS) events can accelerate the surface ablation of sea ice, greatly influencing the ice–albedo feedback. We found that spring ROS events have shifted to earlier dates over the Arctic Ocean in recent decades, which is correlated with sea ice melt onset in the Pacific sector and most Eurasian marginal seas. There has been a clear transition from solid to liquid precipitation, leading to a reduction in spring snow depth on sea ice by more than −0.5 cm per decade since the 1980s.
Rain-on-snow (ROS) events can accelerate the surface ablation of sea ice, greatly influencing...