Articles | Volume 13, issue 5
https://doi.org/10.5194/tc-13-1423-2019
© 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-13-1423-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Contributions of advection and melting processes to the decline in sea ice in the Pacific sector of the Arctic Ocean
Haibo Bi
CORRESPONDING AUTHOR
Key laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
Qinghua Yang
Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai, China
State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics (IAP), Chinese Academy of Sciences, Beijing, China
Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China
Key Laboratory of Research on Marine Hazards Forecasting, National Marine Environmental Forecasting Center, Beijing, China
Liang Zhang
Key laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
Yunhe Wang
Key laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
Yu Liang
Key laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
Haijun Huang
Key laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, China
College of Earth and Planetary Science, University of Chinese Academy of Sciences, Beijing, China
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Cited
16 citations as recorded by crossref.
- Influence of Arctic sea-ice variability on Pacific trade winds C. Kennel & E. Yulaeva 10.1073/pnas.1717707117
- The Roles of Sea Ice Export, Atmospheric and Oceanic Factors in the Seasonal and Regional Variability of Arctic Sea Ice during 1979–2020 M. Li et al. 10.3390/rs14040904
- Trends and spatial variation in rain-on-snow events over the Arctic Ocean during the early melt season T. Dou et al. 10.5194/tc-15-883-2021
- Decadal phase shift of summertime Arctic dipole pattern and its nonlinear effect on sea ice extent E. Heo et al. 10.1002/joc.7097
- Spatio-temporal analysis of the melt onset dates over Arctic sea ice from 1979 to 2017 S. Liang et al. 10.1007/s13131-021-1827-x
- Distinct Role of a Spring Atmospheric Circulation Mode in the Arctic Sea Ice Decline in Summer H. Bi et al. 10.1029/2022JD037477
- Spatial characterization of global heat waves using satellite-based land surface temperature Y. Hu et al. 10.1016/j.jag.2023.103604
- Four- to Six-Year Periodic Variation of Arctic Sea-Ice Extent and Its Three Main Driving Factors P. Chen et al. 10.1007/s00376-024-3104-3
- Arctic multiyear sea ice variability observed from satellites: a review H. Bi et al. 10.1007/s00343-020-0093-7
- Arctic sea ice motion change and response to atmospheric forcing between 1979 and 2019 F. Zhang et al. 10.1002/joc.7340
- Prediction of Pan-Arctic Sea Ice Using Attention-Based LSTM Neural Networks J. Wei et al. 10.3389/fmars.2022.860403
- Seasonal changes in sea ice kinematics and deformation in the Pacific sector of the Arctic Ocean in 2018/19 R. Lei et al. 10.5194/tc-15-1321-2021
- Investigation of the Arctic Sea ice volume from 2002 to 2018 using multi‐source data M. Li et al. 10.1002/joc.6972
- Variability of Arctic Sea ice age and its relationship with atmospheric circulation patterns P. Chen et al. 10.3389/fmars.2023.1274665
- Influences of Summertime Arctic Dipole Atmospheric Circulation on Sea Ice Concentration Variations in the Pacific Sector of the Arctic during Different Pacific Decadal Oscillation Phases H. Bi et al. 10.1175/JCLI-D-19-0843.1
- Impact of Arctic Oscillation on cloud radiative forcing and September sea ice retreat Y. Li et al. 10.1007/s13131-022-2010-8
16 citations as recorded by crossref.
- Influence of Arctic sea-ice variability on Pacific trade winds C. Kennel & E. Yulaeva 10.1073/pnas.1717707117
- The Roles of Sea Ice Export, Atmospheric and Oceanic Factors in the Seasonal and Regional Variability of Arctic Sea Ice during 1979–2020 M. Li et al. 10.3390/rs14040904
- Trends and spatial variation in rain-on-snow events over the Arctic Ocean during the early melt season T. Dou et al. 10.5194/tc-15-883-2021
- Decadal phase shift of summertime Arctic dipole pattern and its nonlinear effect on sea ice extent E. Heo et al. 10.1002/joc.7097
- Spatio-temporal analysis of the melt onset dates over Arctic sea ice from 1979 to 2017 S. Liang et al. 10.1007/s13131-021-1827-x
- Distinct Role of a Spring Atmospheric Circulation Mode in the Arctic Sea Ice Decline in Summer H. Bi et al. 10.1029/2022JD037477
- Spatial characterization of global heat waves using satellite-based land surface temperature Y. Hu et al. 10.1016/j.jag.2023.103604
- Four- to Six-Year Periodic Variation of Arctic Sea-Ice Extent and Its Three Main Driving Factors P. Chen et al. 10.1007/s00376-024-3104-3
- Arctic multiyear sea ice variability observed from satellites: a review H. Bi et al. 10.1007/s00343-020-0093-7
- Arctic sea ice motion change and response to atmospheric forcing between 1979 and 2019 F. Zhang et al. 10.1002/joc.7340
- Prediction of Pan-Arctic Sea Ice Using Attention-Based LSTM Neural Networks J. Wei et al. 10.3389/fmars.2022.860403
- Seasonal changes in sea ice kinematics and deformation in the Pacific sector of the Arctic Ocean in 2018/19 R. Lei et al. 10.5194/tc-15-1321-2021
- Investigation of the Arctic Sea ice volume from 2002 to 2018 using multi‐source data M. Li et al. 10.1002/joc.6972
- Variability of Arctic Sea ice age and its relationship with atmospheric circulation patterns P. Chen et al. 10.3389/fmars.2023.1274665
- Influences of Summertime Arctic Dipole Atmospheric Circulation on Sea Ice Concentration Variations in the Pacific Sector of the Arctic during Different Pacific Decadal Oscillation Phases H. Bi et al. 10.1175/JCLI-D-19-0843.1
- Impact of Arctic Oscillation on cloud radiative forcing and September sea ice retreat Y. Li et al. 10.1007/s13131-022-2010-8
Latest update: 20 Nov 2024
Short summary
The Arctic sea ice extent is diminishing, which is deemed an immediate response to a warmer Earth. However, quantitative estimates about the contribution due to transport and melt to the sea ice loss are still vague. This study mainly utilizes satellite observations to quantify the dynamic and thermodynamic aspects of ice loss for nearly 40 years (1979–2016). In addition, the potential impacts on ice reduction due to different atmospheric circulation pattern are highlighted.
The Arctic sea ice extent is diminishing, which is deemed an immediate response to a warmer...