Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk

In the southwestern part of the Sea of Okhotsk off Hokkaido, sea-ice drift characteristics are investigated using the ice and water velocities obtained from a moored upward-looking acoustic Doppler current profiler (ADCP) during the winters of 1999-2001. Using hourly-mean values of these data along...

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Published in:Annals of Glaciology
Main Authors: Fukamachi, Yasushi, Ohshima, Kay I., Mukai, Yuji, Mizuta, Genta, Wakatsuchi, Masaaki
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society
Subjects:
Online Access:http://hdl.handle.net/2115/47350
https://doi.org/10.3189/172756411795931507
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author Fukamachi, Yasushi
Ohshima, Kay I.
Mukai, Yuji
Mizuta, Genta
Wakatsuchi, Masaaki
author_facet Fukamachi, Yasushi
Ohshima, Kay I.
Mukai, Yuji
Mizuta, Genta
Wakatsuchi, Masaaki
author_sort Fukamachi, Yasushi
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
container_issue 57
container_start_page 1
container_title Annals of Glaciology
container_volume 52
description In the southwestern part of the Sea of Okhotsk off Hokkaido, sea-ice drift characteristics are investigated using the ice and water velocities obtained from a moored upward-looking acoustic Doppler current profiler (ADCP) during the winters of 1999-2001. Using hourly-mean values of these data along with the wind data measured at a nearby coastal station, the wind factor and turning angle of the relative velocity between the ice and water velocities with respect to the wind are calculated assuming free drift under various conditions. Since the simultaneous sea-ice draft data are also available from a moored ice-profiling sonar (IPS), we examine the dependence of drift characteristics on ice thickness for the first time. As ice thickness increases and wind decreases, the wind factor decreases and the turning angle increases, as predicted by the theory of free drift. This study clearly shows the utility of the moored ADCP measurement for studying sea-ice drift, especially with the simultaneous IPS measurement for ice thickness, which cannot be obtained by other methods.
format Article in Journal/Newspaper
genre Annals of Glaciology
Sea ice
genre_facet Annals of Glaciology
Sea ice
geographic Okhotsk
geographic_facet Okhotsk
id fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/47350
institution Open Polar
language English
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op_container_end_page 8
op_doi https://doi.org/10.3189/172756411795931507
op_relation http://www.igsoc.org/
http://hdl.handle.net/2115/47350
Annals of Glaciology, 52(57): 1-8
http://dx.doi.org/10.3189/172756411795931507
op_rights © 2011 International Glaciological Society
publisher International Glaciological Society
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spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/47350 2025-01-16T18:59:43+00:00 Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk Fukamachi, Yasushi Ohshima, Kay I. Mukai, Yuji Mizuta, Genta Wakatsuchi, Masaaki http://hdl.handle.net/2115/47350 https://doi.org/10.3189/172756411795931507 eng eng International Glaciological Society http://www.igsoc.org/ http://hdl.handle.net/2115/47350 Annals of Glaciology, 52(57): 1-8 http://dx.doi.org/10.3189/172756411795931507 © 2011 International Glaciological Society 452 article fthokunivhus https://doi.org/10.3189/172756411795931507 2022-11-18T01:02:09Z In the southwestern part of the Sea of Okhotsk off Hokkaido, sea-ice drift characteristics are investigated using the ice and water velocities obtained from a moored upward-looking acoustic Doppler current profiler (ADCP) during the winters of 1999-2001. Using hourly-mean values of these data along with the wind data measured at a nearby coastal station, the wind factor and turning angle of the relative velocity between the ice and water velocities with respect to the wind are calculated assuming free drift under various conditions. Since the simultaneous sea-ice draft data are also available from a moored ice-profiling sonar (IPS), we examine the dependence of drift characteristics on ice thickness for the first time. As ice thickness increases and wind decreases, the wind factor decreases and the turning angle increases, as predicted by the theory of free drift. This study clearly shows the utility of the moored ADCP measurement for studying sea-ice drift, especially with the simultaneous IPS measurement for ice thickness, which cannot be obtained by other methods. Article in Journal/Newspaper Annals of Glaciology Sea ice Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Okhotsk Annals of Glaciology 52 57 1 8
spellingShingle 452
Fukamachi, Yasushi
Ohshima, Kay I.
Mukai, Yuji
Mizuta, Genta
Wakatsuchi, Masaaki
Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk
title Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk
title_full Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk
title_fullStr Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk
title_full_unstemmed Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk
title_short Sea-ice drift characteristics revealed by measurement of acoustic Doppler current profiler and ice-profiling sonar off Hokkaido in the Sea of Okhotsk
title_sort sea-ice drift characteristics revealed by measurement of acoustic doppler current profiler and ice-profiling sonar off hokkaido in the sea of okhotsk
topic 452
topic_facet 452
url http://hdl.handle.net/2115/47350
https://doi.org/10.3189/172756411795931507