Nearfield measurements of ice melting noise in the central Arctic Ocean in summer

Sea ice melting is very common in Arctic summer, so it is important to study ice melting noise. This paper analyzes a 456 min time series of under-ice noise that was recorded at a depth of 29.9 m in the central Arctic Ocean when the area was approximately 89% ice cover, UTC time, on August 8th, 2017...

Full description

Bibliographic Details
Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16019
http://id.nii.ac.jp/1291/00015907/
id ftnipr:oai:nipr.repo.nii.ac.jp:00016019
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00016019 2023-05-15T14:48:11+02:00 Nearfield measurements of ice melting noise in the central Arctic Ocean in summer 2020-06 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16019 http://id.nii.ac.jp/1291/00015907/ en eng https://doi.org/10.1016/j.polar.2020.100528 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16019 http://id.nii.ac.jp/1291/00015907/ Polar Science, 24, 100528(2020-06) 18739652 Ice melting noise Bubble clouds Air temperature Summer Central arctic ocean Journal Article 2020 ftnipr https://doi.org/10.1016/j.polar.2020.100528 2022-12-03T19:43:16Z Sea ice melting is very common in Arctic summer, so it is important to study ice melting noise. This paper analyzes a 456 min time series of under-ice noise that was recorded at a depth of 29.9 m in the central Arctic Ocean when the area was approximately 89% ice cover, UTC time, on August 8th, 2017. When the air temperature was higher than the freezing point of the surface sea water, the under-ice noise levels increased. In particular, the noise levels at 80–240 Hz and 380–660 Hz had two broad peaks and increased by 5–15 dB, furthermore, there was a large number of transient signals in the noise data. When the air temperature decreased and was less than the freezing point of the surface sea water, the under-ice noise levels gradually decreased, the broad peaks of the under-ice noise levels gradually disappeared, and the transient signals also disappeared. At the above two frequency bands, the correlation coefficients between the air temperature and under-ice noise levels were generally above 0.5 and reached a maximum value of 0.81. These results suggest that the changes in the under-ice noise levels could be attributed to sea ice melting. Article in Journal/Newspaper Arctic Arctic Ocean Polar Science Polar Science Sea ice National Institute of Polar Research Repository, Japan Arctic Arctic Ocean Polar Science 24 100528
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Ice melting noise
Bubble clouds
Air temperature
Summer
Central arctic ocean
spellingShingle Ice melting noise
Bubble clouds
Air temperature
Summer
Central arctic ocean
Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
topic_facet Ice melting noise
Bubble clouds
Air temperature
Summer
Central arctic ocean
description Sea ice melting is very common in Arctic summer, so it is important to study ice melting noise. This paper analyzes a 456 min time series of under-ice noise that was recorded at a depth of 29.9 m in the central Arctic Ocean when the area was approximately 89% ice cover, UTC time, on August 8th, 2017. When the air temperature was higher than the freezing point of the surface sea water, the under-ice noise levels increased. In particular, the noise levels at 80–240 Hz and 380–660 Hz had two broad peaks and increased by 5–15 dB, furthermore, there was a large number of transient signals in the noise data. When the air temperature decreased and was less than the freezing point of the surface sea water, the under-ice noise levels gradually decreased, the broad peaks of the under-ice noise levels gradually disappeared, and the transient signals also disappeared. At the above two frequency bands, the correlation coefficients between the air temperature and under-ice noise levels were generally above 0.5 and reached a maximum value of 0.81. These results suggest that the changes in the under-ice noise levels could be attributed to sea ice melting.
format Article in Journal/Newspaper
title Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
title_short Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
title_full Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
title_fullStr Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
title_full_unstemmed Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
title_sort nearfield measurements of ice melting noise in the central arctic ocean in summer
publishDate 2020
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16019
http://id.nii.ac.jp/1291/00015907/
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Polar Science
Polar Science
Sea ice
genre_facet Arctic
Arctic Ocean
Polar Science
Polar Science
Sea ice
op_relation https://doi.org/10.1016/j.polar.2020.100528
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16019
http://id.nii.ac.jp/1291/00015907/
Polar Science, 24, 100528(2020-06)
18739652
op_doi https://doi.org/10.1016/j.polar.2020.100528
container_title Polar Science
container_volume 24
container_start_page 100528
_version_ 1766319285466038272