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  1. 極地研刊行誌
  2. Polar Science
  3. Vol.24 (Jun. 2020)

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

https://nipr.repo.nii.ac.jp/records/16019
https://nipr.repo.nii.ac.jp/records/16019
f5dfe886-3564-44c7-9dfb-3a13a125726f
Item type 学術雑誌論文 / Journal Article(1)
公開日 2020-06-24
タイトル
タイトル Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
タイトル
タイトル Nearfield measurements of ice melting noise in the central Arctic Ocean in summer
言語 en
言語
言語 eng
キーワード
言語 en
主題Scheme Other
主題 Ice melting noise
キーワード
言語 en
主題Scheme Other
主題 Bubble clouds
キーワード
言語 en
主題Scheme Other
主題 Air temperature
キーワード
言語 en
主題Scheme Other
主題 Summer
キーワード
言語 en
主題Scheme Other
主題 Central arctic ocean
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
アクセス権
アクセス権 metadata only access
アクセス権URI http://purl.org/coar/access_right/c_14cb
著者 Wen, Hongtao

× Wen, Hongtao

en Wen, Hongtao

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Yang, Yanming

× Yang, Yanming

en Yang, Yanming

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Ruan, Hailin

× Ruan, Hailin

en Ruan, Hailin

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Zhou, Hongtao

× Zhou, Hongtao

en Zhou, Hongtao

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Wang, Ning

× Wang, Ning

en Wang, Ning

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抄録
内容記述タイプ Abstract
内容記述 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.
書誌情報 en : Polar Science

巻 24, p. 100528, 発行日 2020-06
ISSN
収録物識別子タイプ ISSN
収録物識別子 18739652
DOI
識別子タイプ DOI
関連識別子 https://doi.org/10.1016/j.polar.2020.100528
関連名称 10.1016/j.polar.2020.100528
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