Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition
We examined mixing processes within the ice–ocean boundary layer (IOBL) close to the geographic North Pole, with an emphasis on wind-driven sea ice drift. Observations were conducted from late August to late September 2020, during the final leg of the international Multidisciplinary drifting Observa...
Published in: | Journal of Geophysical Research: Oceans |
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American Geophysical Union (AGU)
2022
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Online Access: | https://epic.awi.de/id/eprint/58801/ https://epic.awi.de/id/eprint/58801/1/JGR%20Oceans%20-%202022%20-%20Kawaguchi%20-%20Turbulent%20Mixing%20During%20Late%20Summer%20in%20the%20Ice%20Ocean%20Boundary%20Layer%20in%20the%20Central%20Arctic.pdf https://doi.org/10.1029/2021jc017975 https://hdl.handle.net/10013/epic.64eeff98-20d5-44bd-a96f-a64484145ea0 |
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ftawi:oai:epic.awi.de:58801 2024-06-23T07:48:45+00:00 Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition Kawaguchi, Yusuke Koenig, Zoé Nomura, Daiki Hoppmann, Mario Inoue, Jun Fang, Ying‐Chih Schulz, Kirstin Gallagher, Michael Katlein, Christian Nicolaus, Marcel Rabe, Benjamin 2022-08 application/pdf https://epic.awi.de/id/eprint/58801/ https://epic.awi.de/id/eprint/58801/1/JGR%20Oceans%20-%202022%20-%20Kawaguchi%20-%20Turbulent%20Mixing%20During%20Late%20Summer%20in%20the%20Ice%20Ocean%20Boundary%20Layer%20in%20the%20Central%20Arctic.pdf https://doi.org/10.1029/2021jc017975 https://hdl.handle.net/10013/epic.64eeff98-20d5-44bd-a96f-a64484145ea0 unknown American Geophysical Union (AGU) https://epic.awi.de/id/eprint/58801/1/JGR%20Oceans%20-%202022%20-%20Kawaguchi%20-%20Turbulent%20Mixing%20During%20Late%20Summer%20in%20the%20Ice%20Ocean%20Boundary%20Layer%20in%20the%20Central%20Arctic.pdf Kawaguchi, Y. , Koenig, Z. , Nomura, D. , Hoppmann, M. , Inoue, J. , Fang, Y. , Schulz, K. , Gallagher, M. , Katlein, C. , Nicolaus, M. and Rabe, B. (2022) Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition , Journal of Geophysical Research - Oceans, 127 (8) . doi:10.1029/2021jc017975 <https://doi.org/10.1029/2021jc017975> , hdl:10013/epic.64eeff98-20d5-44bd-a96f-a64484145ea0 EPIC3Journal of Geophysical Research - Oceans, American Geophysical Union (AGU), 127(8), ISSN: 2169-9275 Article isiRev 2022 ftawi https://doi.org/10.1029/2021jc017975 2024-06-04T23:48:21Z We examined mixing processes within the ice–ocean boundary layer (IOBL) close to the geographic North Pole, with an emphasis on wind-driven sea ice drift. Observations were conducted from late August to late September 2020, during the final leg of the international Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. Measurements of ice motion, and profiles of currents, hydrography, and microstructure turbulence were conducted. The multifarious direct observations of sea ice and the upper ocean were used to quantify the transport of momentum, heat, and salt in the IOBL. The ice drift was mostly characterized by the inertial oscillation at a semi-diurnal frequency, which forced an inertial current in the mixed layer. Observation-derived heat and salinity fluxes at the ice–ocean interface suggest early termination of basal melting and transitioning to refreezing, resulting from a rise in the freezing point temperature by the presence of freshened near-surface water. Based on the friction velocity, the measured dissipation rate (ε) of turbulent energy can be approximated as 1.4–1.7 times of the “Law of the Wall” criterion. We also observed a spiraling Ekman flow and find its vertical extent in line with the estimate from ε-based diffusivity. Following passage of a storm, the enhanced oscillatory motions of the ice drift caused trapping of the near-inertial waves (NIWs) that exclusively propagated through the base of the weakly stratified mixed layer. We accounted Holmboe instabilities and NIWs for the observed distinct peak of the dissipation rate near the bottom of the mixed layer. Article in Journal/Newspaper Arctic Arctic Arctic Ocean North Pole Sea ice Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Arctic Ocean Holmboe ENVELOPE(-86.583,-86.583,-77.333,-77.333) North Pole Journal of Geophysical Research: Oceans 127 8 |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
We examined mixing processes within the ice–ocean boundary layer (IOBL) close to the geographic North Pole, with an emphasis on wind-driven sea ice drift. Observations were conducted from late August to late September 2020, during the final leg of the international Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. Measurements of ice motion, and profiles of currents, hydrography, and microstructure turbulence were conducted. The multifarious direct observations of sea ice and the upper ocean were used to quantify the transport of momentum, heat, and salt in the IOBL. The ice drift was mostly characterized by the inertial oscillation at a semi-diurnal frequency, which forced an inertial current in the mixed layer. Observation-derived heat and salinity fluxes at the ice–ocean interface suggest early termination of basal melting and transitioning to refreezing, resulting from a rise in the freezing point temperature by the presence of freshened near-surface water. Based on the friction velocity, the measured dissipation rate (ε) of turbulent energy can be approximated as 1.4–1.7 times of the “Law of the Wall” criterion. We also observed a spiraling Ekman flow and find its vertical extent in line with the estimate from ε-based diffusivity. Following passage of a storm, the enhanced oscillatory motions of the ice drift caused trapping of the near-inertial waves (NIWs) that exclusively propagated through the base of the weakly stratified mixed layer. We accounted Holmboe instabilities and NIWs for the observed distinct peak of the dissipation rate near the bottom of the mixed layer. |
format |
Article in Journal/Newspaper |
author |
Kawaguchi, Yusuke Koenig, Zoé Nomura, Daiki Hoppmann, Mario Inoue, Jun Fang, Ying‐Chih Schulz, Kirstin Gallagher, Michael Katlein, Christian Nicolaus, Marcel Rabe, Benjamin |
spellingShingle |
Kawaguchi, Yusuke Koenig, Zoé Nomura, Daiki Hoppmann, Mario Inoue, Jun Fang, Ying‐Chih Schulz, Kirstin Gallagher, Michael Katlein, Christian Nicolaus, Marcel Rabe, Benjamin Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition |
author_facet |
Kawaguchi, Yusuke Koenig, Zoé Nomura, Daiki Hoppmann, Mario Inoue, Jun Fang, Ying‐Chih Schulz, Kirstin Gallagher, Michael Katlein, Christian Nicolaus, Marcel Rabe, Benjamin |
author_sort |
Kawaguchi, Yusuke |
title |
Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition |
title_short |
Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition |
title_full |
Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition |
title_fullStr |
Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition |
title_full_unstemmed |
Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition |
title_sort |
turbulent mixing during late summer in the ice–ocean boundary layer in the central arctic ocean: results from the mosaic expedition |
publisher |
American Geophysical Union (AGU) |
publishDate |
2022 |
url |
https://epic.awi.de/id/eprint/58801/ https://epic.awi.de/id/eprint/58801/1/JGR%20Oceans%20-%202022%20-%20Kawaguchi%20-%20Turbulent%20Mixing%20During%20Late%20Summer%20in%20the%20Ice%20Ocean%20Boundary%20Layer%20in%20the%20Central%20Arctic.pdf https://doi.org/10.1029/2021jc017975 https://hdl.handle.net/10013/epic.64eeff98-20d5-44bd-a96f-a64484145ea0 |
long_lat |
ENVELOPE(-86.583,-86.583,-77.333,-77.333) |
geographic |
Arctic Arctic Ocean Holmboe North Pole |
geographic_facet |
Arctic Arctic Ocean Holmboe North Pole |
genre |
Arctic Arctic Arctic Ocean North Pole Sea ice |
genre_facet |
Arctic Arctic Arctic Ocean North Pole Sea ice |
op_source |
EPIC3Journal of Geophysical Research - Oceans, American Geophysical Union (AGU), 127(8), ISSN: 2169-9275 |
op_relation |
https://epic.awi.de/id/eprint/58801/1/JGR%20Oceans%20-%202022%20-%20Kawaguchi%20-%20Turbulent%20Mixing%20During%20Late%20Summer%20in%20the%20Ice%20Ocean%20Boundary%20Layer%20in%20the%20Central%20Arctic.pdf Kawaguchi, Y. , Koenig, Z. , Nomura, D. , Hoppmann, M. , Inoue, J. , Fang, Y. , Schulz, K. , Gallagher, M. , Katlein, C. , Nicolaus, M. and Rabe, B. (2022) Turbulent Mixing During Late Summer in the Ice–Ocean Boundary Layer in the Central Arctic Ocean: Results From the MOSAiC Expedition , Journal of Geophysical Research - Oceans, 127 (8) . doi:10.1029/2021jc017975 <https://doi.org/10.1029/2021jc017975> , hdl:10013/epic.64eeff98-20d5-44bd-a96f-a64484145ea0 |
op_doi |
https://doi.org/10.1029/2021jc017975 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
127 |
container_issue |
8 |
_version_ |
1802639073443053568 |