Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation
Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directio...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Komissarova, N. N. [verfasserIn] |
|---|
| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2001 |
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| Schlagwörter: |
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| Anmerkung: |
© Komissarova 2001 |
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| Übergeordnetes Werk: |
Enthalten in: Acoustical physics - Nauka/Interperiodica, 1993, 47(2001), 3 vom: Mai, Seite 313-322 |
|---|---|
| Übergeordnetes Werk: |
volume:47 ; year:2001 ; number:3 ; month:05 ; pages:313-322 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF03353586 |
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OLC2085599087 |
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| 520 | |a Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. | ||
| 650 | 4 | |a Coastal Zone | |
| 650 | 4 | |a Acoustical Physic | |
| 650 | 4 | |a Normal Wave | |
| 650 | 4 | |a Wedge Angle | |
| 650 | 4 | |a Reception Point | |
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10.1007/BF03353586 doi (DE-627)OLC2085599087 (DE-He213)BF03353586-p DE-627 ger DE-627 rakwb eng 530 VZ Komissarova, N. N. verfasserin aut Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Komissarova 2001 Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. Coastal Zone Acoustical Physic Normal Wave Wedge Angle Reception Point Enthalten in Acoustical physics Nauka/Interperiodica, 1993 47(2001), 3 vom: Mai, Seite 313-322 (DE-627)17114936X (DE-600)1158030-6 (DE-576)038488353 1063-7710 nnns volume:47 year:2001 number:3 month:05 pages:313-322 https://doi.org/10.1007/BF03353586 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2256 AR 47 2001 3 05 313-322 |
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10.1007/BF03353586 doi (DE-627)OLC2085599087 (DE-He213)BF03353586-p DE-627 ger DE-627 rakwb eng 530 VZ Komissarova, N. N. verfasserin aut Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Komissarova 2001 Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. Coastal Zone Acoustical Physic Normal Wave Wedge Angle Reception Point Enthalten in Acoustical physics Nauka/Interperiodica, 1993 47(2001), 3 vom: Mai, Seite 313-322 (DE-627)17114936X (DE-600)1158030-6 (DE-576)038488353 1063-7710 nnns volume:47 year:2001 number:3 month:05 pages:313-322 https://doi.org/10.1007/BF03353586 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2256 AR 47 2001 3 05 313-322 |
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10.1007/BF03353586 doi (DE-627)OLC2085599087 (DE-He213)BF03353586-p DE-627 ger DE-627 rakwb eng 530 VZ Komissarova, N. N. verfasserin aut Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Komissarova 2001 Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. Coastal Zone Acoustical Physic Normal Wave Wedge Angle Reception Point Enthalten in Acoustical physics Nauka/Interperiodica, 1993 47(2001), 3 vom: Mai, Seite 313-322 (DE-627)17114936X (DE-600)1158030-6 (DE-576)038488353 1063-7710 nnns volume:47 year:2001 number:3 month:05 pages:313-322 https://doi.org/10.1007/BF03353586 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2256 AR 47 2001 3 05 313-322 |
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10.1007/BF03353586 doi (DE-627)OLC2085599087 (DE-He213)BF03353586-p DE-627 ger DE-627 rakwb eng 530 VZ Komissarova, N. N. verfasserin aut Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Komissarova 2001 Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. Coastal Zone Acoustical Physic Normal Wave Wedge Angle Reception Point Enthalten in Acoustical physics Nauka/Interperiodica, 1993 47(2001), 3 vom: Mai, Seite 313-322 (DE-627)17114936X (DE-600)1158030-6 (DE-576)038488353 1063-7710 nnns volume:47 year:2001 number:3 month:05 pages:313-322 https://doi.org/10.1007/BF03353586 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2256 AR 47 2001 3 05 313-322 |
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10.1007/BF03353586 doi (DE-627)OLC2085599087 (DE-He213)BF03353586-p DE-627 ger DE-627 rakwb eng 530 VZ Komissarova, N. N. verfasserin aut Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Komissarova 2001 Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. Coastal Zone Acoustical Physic Normal Wave Wedge Angle Reception Point Enthalten in Acoustical physics Nauka/Interperiodica, 1993 47(2001), 3 vom: Mai, Seite 313-322 (DE-627)17114936X (DE-600)1158030-6 (DE-576)038488353 1063-7710 nnns volume:47 year:2001 number:3 month:05 pages:313-322 https://doi.org/10.1007/BF03353586 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_40 GBV_ILN_70 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2256 AR 47 2001 3 05 313-322 |
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Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation |
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Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. © Komissarova 2001 |
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Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. © Komissarova 2001 |
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Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom. © Komissarova 2001 |
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N.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Sound Field Features in the Coastal Zone of a Shallow Sea with an Airborne Source of Excitation</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2001</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Komissarova 2001</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Features of the sound field in the coastal zone are theoretically investigated in the case of a moving airborne sound source. It is shown that two factors govern the drastic increase in the signal level measured at the observation point when the source moves near the shoreline: the directional property of the field transmitted from the air into the water and the structure of the normal wave in the wedge near the caustic. The magnitude of the increase in the sound field level depends on the depth of the reception point and, what is more essential, on the structure of the bottom.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coastal Zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Acoustical Physic</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Normal Wave</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Wedge Angle</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Reception Point</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Acoustical physics</subfield><subfield code="d">Nauka/Interperiodica, 1993</subfield><subfield code="g">47(2001), 3 vom: Mai, Seite 313-322</subfield><subfield code="w">(DE-627)17114936X</subfield><subfield code="w">(DE-600)1158030-6</subfield><subfield code="w">(DE-576)038488353</subfield><subfield code="x">1063-7710</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:47</subfield><subfield code="g">year:2001</subfield><subfield code="g">number:3</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:313-322</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF03353586</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_201</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2256</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">47</subfield><subfield code="j">2001</subfield><subfield code="e">3</subfield><subfield code="c">05</subfield><subfield code="h">313-322</subfield></datafield></record></collection>
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