Generation of Underwater Noise by the Rip Zone of a Large-Amplitude Internal Wave in the Ocean
The article discusses the results of measuring underwater noise generated by a large-amplitude solitary internal wave based on observations made near the Mascarene Ridge in the Indian Ocean. The measurements were taken from a ship drifting over large depths, equipped with a vertical string of hydrop...
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Veröffentlicht in: | Acoustical physics 2022-06, Vol.68 (3), p.272-281 |
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description | The article discusses the results of measuring underwater noise generated by a large-amplitude solitary internal wave based on observations made near the Mascarene Ridge in the Indian Ocean. The measurements were taken from a ship drifting over large depths, equipped with a vertical string of hydrophones and equipment for recording internal waves. The parameters of the recorded 50 m internal wave and characteristics of the emitted underwater noise are given. Powerful orbital currents accompanying the internal wave form rips on the ocean surface: areas of chaotic, collapsing waves that increase the air bubble concentration in the near-surface layer and emit underwater noise. Analysis of the data showed that the passage of a rip caused by an internal wave over a hydrophone leads to a significant (up to 18 dB) increase in the level of underwater noise in the 5–15 kHz frequency range. |
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Analysis of the data showed that the passage of a rip caused by an internal wave over a hydrophone leads to a significant (up to 18 dB) increase in the level of underwater noise in the 5–15 kHz frequency range.</description><identifier>ISSN: 1063-7710</identifier><identifier>EISSN: 1562-6865</identifier><identifier>DOI: 10.1134/S1063771022030125</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Acoustics ; Air bubbles ; Amplitudes ; Frequency ranges ; Hydrophones ; Internal waves ; Noise measurement ; Ocean Acoustics. Hydroacoustics ; Ocean currents ; Ocean surface ; Physics ; Physics and Astronomy ; Surface layers ; Underwater</subject><ispartof>Acoustical physics, 2022-06, Vol.68 (3), p.272-281</ispartof><rights>Pleiades Publishing, Ltd. 2022. ISSN 1063-7710, Acoustical Physics, 2022, Vol. 68, No. 3, pp. 272–281. © Pleiades Publishing, Ltd., 2022. 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A.</creatorcontrib><creatorcontrib>Okhrimenko, N. N.</creatorcontrib><title>Generation of Underwater Noise by the Rip Zone of a Large-Amplitude Internal Wave in the Ocean</title><title>Acoustical physics</title><addtitle>Acoust. Phys</addtitle><description>The article discusses the results of measuring underwater noise generated by a large-amplitude solitary internal wave based on observations made near the Mascarene Ridge in the Indian Ocean. The measurements were taken from a ship drifting over large depths, equipped with a vertical string of hydrophones and equipment for recording internal waves. The parameters of the recorded 50 m internal wave and characteristics of the emitted underwater noise are given. Powerful orbital currents accompanying the internal wave form rips on the ocean surface: areas of chaotic, collapsing waves that increase the air bubble concentration in the near-surface layer and emit underwater noise. Analysis of the data showed that the passage of a rip caused by an internal wave over a hydrophone leads to a significant (up to 18 dB) increase in the level of underwater noise in the 5–15 kHz frequency range.</description><subject>Acoustics</subject><subject>Air bubbles</subject><subject>Amplitudes</subject><subject>Frequency ranges</subject><subject>Hydrophones</subject><subject>Internal waves</subject><subject>Noise measurement</subject><subject>Ocean Acoustics. Hydroacoustics</subject><subject>Ocean currents</subject><subject>Ocean surface</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Surface layers</subject><subject>Underwater</subject><issn>1063-7710</issn><issn>1562-6865</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kEFLw0AQhRdRsFZ_gLcFz9HZ3WSTHEvRtlAsqEXwYJhkJzWl3cTdVOm_N7GCB_E0A-99j5nH2KWAayFUePMoQKs4FiAlKBAyOmIDEWkZ6ERHx93eyUGvn7Iz79cAkColB-x1QpYctlVteV3ypTXkPrElx-_ryhPP97x9I_5QNfylttR7kM_RrSgYbZtN1e4M8ZntAIsb_owfxCv7jSwKQnvOTkrceLr4mUO2vLt9Gk-D-WIyG4_mQSFD3QYEpAxKpUwqUQEaFeWYYBKBNCloHQqRxlqFhYowT0I0uSiLPEkgBCgQhBqyq0Nu4-r3Hfk2W9e7_iSfSZ2A7D6Po84lDq7C1d47KrPGVVt0-0xA1teY_amxY-SB8Z3Xrsj9Jv8PfQH_5XIU</recordid><startdate>20220601</startdate><enddate>20220601</enddate><creator>Serebryany, A. N.</creator><creator>Furduev, A. V.</creator><creator>Aredov, A. A.</creator><creator>Okhrimenko, N. 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Hydroacoustics</topic><topic>Ocean currents</topic><topic>Ocean surface</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Surface layers</topic><topic>Underwater</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Serebryany, A. N.</creatorcontrib><creatorcontrib>Furduev, A. V.</creatorcontrib><creatorcontrib>Aredov, A. A.</creatorcontrib><creatorcontrib>Okhrimenko, N. N.</creatorcontrib><collection>CrossRef</collection><jtitle>Acoustical physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Serebryany, A. N.</au><au>Furduev, A. V.</au><au>Aredov, A. A.</au><au>Okhrimenko, N. N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Generation of Underwater Noise by the Rip Zone of a Large-Amplitude Internal Wave in the Ocean</atitle><jtitle>Acoustical physics</jtitle><stitle>Acoust. Phys</stitle><date>2022-06-01</date><risdate>2022</risdate><volume>68</volume><issue>3</issue><spage>272</spage><epage>281</epage><pages>272-281</pages><issn>1063-7710</issn><eissn>1562-6865</eissn><abstract>The article discusses the results of measuring underwater noise generated by a large-amplitude solitary internal wave based on observations made near the Mascarene Ridge in the Indian Ocean. The measurements were taken from a ship drifting over large depths, equipped with a vertical string of hydrophones and equipment for recording internal waves. The parameters of the recorded 50 m internal wave and characteristics of the emitted underwater noise are given. Powerful orbital currents accompanying the internal wave form rips on the ocean surface: areas of chaotic, collapsing waves that increase the air bubble concentration in the near-surface layer and emit underwater noise. Analysis of the data showed that the passage of a rip caused by an internal wave over a hydrophone leads to a significant (up to 18 dB) increase in the level of underwater noise in the 5–15 kHz frequency range.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1063771022030125</doi><tpages>10</tpages></addata></record> |
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subjects | Acoustics Air bubbles Amplitudes Frequency ranges Hydrophones Internal waves Noise measurement Ocean Acoustics. Hydroacoustics Ocean currents Ocean surface Physics Physics and Astronomy Surface layers Underwater |
title | Generation of Underwater Noise by the Rip Zone of a Large-Amplitude Internal Wave in the Ocean |
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