Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean

Jia YOU; Zhenhua XU; Robin ROBERTSON; Qun LI; Baoshu YIN

doi:10.1007/s00343-021-1037-6

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Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean

Physics | Updated：2023-05-20

- Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean
- Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean
- 海洋湖沼学报（英文） 2022年40卷第3期页码：846-869
- Affiliations：
  
  1.CAS Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  2.Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
  3.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
  4.College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
  5.CAS Engineering Laboratory for Marine Ranching, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  6.China-Asean College of Marine Science, Xiamen University Malaysia, Sepang 43900, Malaysia
  7.MNR Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200120, China
- Author bio：
  
  Zhenhua XU, xuzhenhua@qdio.ac.cn
  Qun LI, liqun@pric.org.cn
- Funds：
  
  the National Key Research and Development Program of China(2019YFE0105700);the National Key Research and Development Program of China(2017YFA0604102);the Strategic Priority Research Program of Chinese Academy of Sciences(XDB42000000);the Strategic Priority Research Program of Chinese Academy of Sciences(XDA22050202);the National Natural Science Foundation of China(92058202);the National Natural Science Foundation of China(41676006);the National Natural Science Foundation of China(42176244);the Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Sciences(COMS2020Q07);the CAS-CSIRO Project Fund(133244KYSB20190031);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2022
- DOI：10.1007/s00343-021-1037-6
  中图分类号：
- 纸质出版：2022-03
- Accepted：
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Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean[J]. 海洋湖沼学报（英文）, 2022,40(3):846-869.

Jia YOU, Zhenhua XU, Robin ROBERTSON, et al. Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean[J]. Journal of Oceanology and Limnology, 2022, 40(3): 846-869.
Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean[J]. 海洋湖沼学报（英文）, 2022,40(3):846-869. DOI： 10.1007/s00343-021-1037-6.

Jia YOU, Zhenhua XU, Robin ROBERTSON, et al. Geographical inhomogeneity and temporal variability of mixing property and driving mechanism in the Arctic Ocean[J]. Journal of Oceanology and Limnology, 2022, 40(3): 846-869. DOI： 10.1007/s00343-021-1037-6.

摘要

Abstract

Upper ocean mixing plays a key role in the atmosphere-ocean heat transfer and sea ice extent and thickness via modulating the upper ocean temperatures in the Arctic Ocean. Observations of diffusivities in the Arctic that directly indicate the ocean mixing properties are sparse. Therefore

the spatiotemporal pattern and magnitude of diapycnal diffusivities and kinetic energy dissipation rates in the upper Arctic Ocean are important for atmosphere-ocean heat transfers and sea ice changes. These were first estimated from the Ice-Tethered Profilers dataset (2005–2019) using a strain-based fine-scale parameterization. The resultant mixing properties showed significant geographical inhomogeneity and temporal variability. Diapycnal diffusivities and dissipation rates in the Atlantic sector of the Arctic Ocean were stronger than those on the Pacific side. Mixing in the Atlantic sector increased significantly during the observation period; whereas in the Pacific sector

it weakened before 2011 and then strengthened. Potential impact factors include wind

sea ice

near inertial waves

and stratification

while their relative contributions vary between the two sectors of the Arctic Ocean. In the Atlantic sector

turbulent mixing dominated

while in the Pacific sector

turbulent mixing was inhibited by strong stratification prior to 2011

and is able to overcome the stratification gradually after 2014. The vertical turbulent heat flux constantly increased in the Atlantic sector year by year

while it decreased in the Pacific sector post 2010. The estimated heat flux variability induced by enhanced turbulent mixing is expected to continue to diminish sea ice in the near future.

关键词

Keywords

references

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