EGU24-18702, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-18702
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Observation of temporal and spatial variability of deep near-inertial waves in the western Arctic Ocean

Chanhyung Jeon1,2, Samuel Boury3, Kyoung-Ho Cho4, Eun-Joo Lee5, Jae-Hun Park5, and Thomas Peacock2
Chanhyung Jeon et al.
  • 1Pusan National University, Oceanography, Korea, Republic of (jeonc@pusan.ac.kr)
  • 2Department of Mechanical Engineering, Massachusetts Institute of Technology
  • 3Courant Institute of Mathematical Sciences, New York University
  • 4Korea Polar Research Institute
  • 5Department of Ocean Sciences, Inha University

Near‐inertial waves are waves propagating in the interior of the ocean. Created by surface storms, they have the potential to influence the ocean environment by inducing vertical mixing. Compared to other oceans, the Arctic Ocean has low near-inertial wave activity, but might be changing. It is a challenge, however, to predict near-inertial wave activity in the Arctic Ocean due to its intricate vertical salinity and temperature stratification. Our in-situ campaign has obtained the first direct deep current measurements revealing notable temporal and spatial variability of deep near-inertial waves in the western Arctic Ocean. These observations are an important step towards a clearer depiction of the evolving energy budget, and concomitant mixing, associated with potentially high impact near-inertial wave activity in an increasingly ice-free Arctic Ocean.

How to cite: Jeon, C., Boury, S., Cho, K.-H., Lee, E.-J., Park, J.-H., and Peacock, T.: Observation of temporal and spatial variability of deep near-inertial waves in the western Arctic Ocean, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18702, https://doi.org/10.5194/egusphere-egu24-18702, 2024.