Upper‐Ocean Turbulence Structure and Ocean‐Ice Drag Coefficient Estimates Using an Ascending Microstructure Profiler During the MOSAiC Drift
Author:
Affiliation:
1. Geophysical Institute University of Bergen and Bjerknes Center for Climate Research Bergen Norway
2. Norwegian Polar Institute Tromsø Norway
3. Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Bremerhaven Germany
Funder
Research Council of Norway
Publisher
American Geophysical Union (AGU)
Subject
Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022JC018751
Reference41 articles.
1. Baumann T. Fer I. Bryhni H. Peterson A. K. Allerholt J. Fang Y.‐C. et al. (2021).Under‐ice current measurements during MOSAiC from a 75 kHz acoustic Doppler profiler[dataset].PANGAEA. Retrieved fromhttps://doi.org/10.1594/PANGAEA.934792
2. Toward Quantifying the Increasing Role of Oceanic Heat in Sea Ice Loss in the New Arctic
3. Ekman Veering, Internal Waves, and Turbulence Observed under Arctic Sea Ice
4. Ice and ocean velocity in the Arctic marginal ice zone: Ice roughness and momentum transfer
5. Mixing Rates and Bottom Drag in Bering Strait
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