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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/16019f5dfe886-3564-44c7-9dfb-3a13a125726f
Item type | 学術雑誌論文 / Journal Article(1) | |||||
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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× Yang, Yanming× Ruan, Hailin× Zhou, Hongtao× 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 |
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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 |