A reexamination of evanescent acoustic-gravity waves: Special properties and aeronomical significance
Acoustic‐gravity wave relations indicate that when wave frequency and horizontal wave number approach the characteristic curve‐delineating gravity and acoustic solutions, the horizontal group velocity and Eckart's characteristic impedance become infinite and wave energy E vanishes. It is shown...
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Veröffentlicht in: | Journal of Geophysical Research. D. Atmospheres 2003-06, Vol.108 (D11), p.ACL8.1-n/a |
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description | Acoustic‐gravity wave relations indicate that when wave frequency and horizontal wave number approach the characteristic curve‐delineating gravity and acoustic solutions, the horizontal group velocity and Eckart's characteristic impedance become infinite and wave energy E vanishes. It is shown that this behavior is equivalent to assuming incorrectly that wave energy is the same function of vertical wave number for internal and evanescent waves. When the correct form of E for evanescent waves is used, the energy flow velocity U defined in terms of the energy flux Fx = EU is bounded by the sound speed, impedance is bounded by values near unity, and E does not vanish. For waves near the Lamb‐wave solution, the dominant dynamical control of the vertically integrated airglow response is the horizontal divergence. The only significant long‐lived evanescent response following an excitation event should be near the Lamb curve, and here the horizontal divergence is largest for small‐scale high‐frequency waves. The transient response is strongest for those waves that disperse least: waves with long‐horizontal wavelengths and waves not too far from the Lamb and Brunt‐Vaisala (BV) curves. Wave properties are well behaved near the characteristic curve and solutions are linked at the common intersection of the Lamb and BV curves implying that waves should be able to transfer energy from one regime to the other in response to background variations. Nonisothermal calculations show that when lapse rates are large enough waves that are at least partially internal can exist at all frequencies. |
doi_str_mv | 10.1029/2002JD002421 |
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L. ; Hecht, J. H.</creator><creatorcontrib>Walterscheid, R. L. ; Hecht, J. H.</creatorcontrib><description>Acoustic‐gravity wave relations indicate that when wave frequency and horizontal wave number approach the characteristic curve‐delineating gravity and acoustic solutions, the horizontal group velocity and Eckart's characteristic impedance become infinite and wave energy E vanishes. It is shown that this behavior is equivalent to assuming incorrectly that wave energy is the same function of vertical wave number for internal and evanescent waves. When the correct form of E for evanescent waves is used, the energy flow velocity U defined in terms of the energy flux Fx = EU is bounded by the sound speed, impedance is bounded by values near unity, and E does not vanish. For waves near the Lamb‐wave solution, the dominant dynamical control of the vertically integrated airglow response is the horizontal divergence. The only significant long‐lived evanescent response following an excitation event should be near the Lamb curve, and here the horizontal divergence is largest for small‐scale high‐frequency waves. The transient response is strongest for those waves that disperse least: waves with long‐horizontal wavelengths and waves not too far from the Lamb and Brunt‐Vaisala (BV) curves. Wave properties are well behaved near the characteristic curve and solutions are linked at the common intersection of the Lamb and BV curves implying that waves should be able to transfer energy from one regime to the other in response to background variations. Nonisothermal calculations show that when lapse rates are large enough waves that are at least partially internal can exist at all frequencies.</description><identifier>ISSN: 0148-0227</identifier><identifier>EISSN: 2156-2202</identifier><identifier>DOI: 10.1029/2002JD002421</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>acoustic waves ; dispersion ; Earth, ocean, space ; evanescence ; Exact sciences and technology ; External geophysics ; Gravity waves ; group velocity ; impedance ; Physics of the high neutral atmosphere ; Tides, waves, convection, winds, turbulence</subject><ispartof>Journal of Geophysical Research. D. 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L.</creatorcontrib><creatorcontrib>Hecht, J. H.</creatorcontrib><title>A reexamination of evanescent acoustic-gravity waves: Special properties and aeronomical significance</title><title>Journal of Geophysical Research. D. Atmospheres</title><addtitle>J. Geophys. Res</addtitle><description>Acoustic‐gravity wave relations indicate that when wave frequency and horizontal wave number approach the characteristic curve‐delineating gravity and acoustic solutions, the horizontal group velocity and Eckart's characteristic impedance become infinite and wave energy E vanishes. It is shown that this behavior is equivalent to assuming incorrectly that wave energy is the same function of vertical wave number for internal and evanescent waves. When the correct form of E for evanescent waves is used, the energy flow velocity U defined in terms of the energy flux Fx = EU is bounded by the sound speed, impedance is bounded by values near unity, and E does not vanish. For waves near the Lamb‐wave solution, the dominant dynamical control of the vertically integrated airglow response is the horizontal divergence. The only significant long‐lived evanescent response following an excitation event should be near the Lamb curve, and here the horizontal divergence is largest for small‐scale high‐frequency waves. The transient response is strongest for those waves that disperse least: waves with long‐horizontal wavelengths and waves not too far from the Lamb and Brunt‐Vaisala (BV) curves. Wave properties are well behaved near the characteristic curve and solutions are linked at the common intersection of the Lamb and BV curves implying that waves should be able to transfer energy from one regime to the other in response to background variations. Nonisothermal calculations show that when lapse rates are large enough waves that are at least partially internal can exist at all frequencies.</description><subject>acoustic waves</subject><subject>dispersion</subject><subject>Earth, ocean, space</subject><subject>evanescence</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Gravity waves</subject><subject>group velocity</subject><subject>impedance</subject><subject>Physics of the high neutral atmosphere</subject><subject>Tides, waves, convection, winds, turbulence</subject><issn>0148-0227</issn><issn>2156-2202</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNqFkMFO3DAURS1EJUbArh_gTbsire3Eid0dApqCoLRQxNJ68Twjt5lksMPA_H1fNYh2VbywLfncK5_H2FspPkih7EclhDo7pq1ScovNlNR1oZRQ22wmZGUKoVSzw_Zz_iloVbquhJwxPOQJ8QkWcYApjgMfA8cVDJg9DhMHPz7kKfriLsEqTmv-CCvMn_j1En2Eni_TuMQ0RcwchjkHTOMwLqKnpxzvhhjoOnjcY28C9Bn3n89ddvP55MfRl-L8sj09OjwvfGUaW3RSAsqym1vbdBIbrQF9CEqUtbbQdEEEhV1V67lVVskA2lhthQVTGVN2ZbnL3m966V_3D5gnt4gk0vckRCJONbbWZP4qKI0hrjYEHmxAn8acEwa3THEBae2kcH_m7v6dO-Hvnnsh0xBCIvuY_2a0IBdRE6c23GPscf3fTnfWXh1boy2Fik0o5gmfXkKQfrm6KRvtbr-2rmyvLq7b79-cKX8D1RegUQ</recordid><startdate>20030616</startdate><enddate>20030616</enddate><creator>Walterscheid, R. L.</creator><creator>Hecht, J. H.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20030616</creationdate><title>A reexamination of evanescent acoustic-gravity waves: Special properties and aeronomical significance</title><author>Walterscheid, R. L. ; Hecht, J. H.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4879-b11ae13bd997b1e755aecff203659a7bf0f2eb465d92921fa5895909a84883b33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>acoustic waves</topic><topic>dispersion</topic><topic>Earth, ocean, space</topic><topic>evanescence</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Gravity waves</topic><topic>group velocity</topic><topic>impedance</topic><topic>Physics of the high neutral atmosphere</topic><topic>Tides, waves, convection, winds, turbulence</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Walterscheid, R. L.</creatorcontrib><creatorcontrib>Hecht, J. H.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of Geophysical Research. D. Atmospheres</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Walterscheid, R. L.</au><au>Hecht, J. H.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A reexamination of evanescent acoustic-gravity waves: Special properties and aeronomical significance</atitle><jtitle>Journal of Geophysical Research. D. Atmospheres</jtitle><addtitle>J. Geophys. Res</addtitle><date>2003-06-16</date><risdate>2003</risdate><volume>108</volume><issue>D11</issue><spage>ACL8.1</spage><epage>n/a</epage><pages>ACL8.1-n/a</pages><issn>0148-0227</issn><eissn>2156-2202</eissn><abstract>Acoustic‐gravity wave relations indicate that when wave frequency and horizontal wave number approach the characteristic curve‐delineating gravity and acoustic solutions, the horizontal group velocity and Eckart's characteristic impedance become infinite and wave energy E vanishes. It is shown that this behavior is equivalent to assuming incorrectly that wave energy is the same function of vertical wave number for internal and evanescent waves. When the correct form of E for evanescent waves is used, the energy flow velocity U defined in terms of the energy flux Fx = EU is bounded by the sound speed, impedance is bounded by values near unity, and E does not vanish. For waves near the Lamb‐wave solution, the dominant dynamical control of the vertically integrated airglow response is the horizontal divergence. The only significant long‐lived evanescent response following an excitation event should be near the Lamb curve, and here the horizontal divergence is largest for small‐scale high‐frequency waves. The transient response is strongest for those waves that disperse least: waves with long‐horizontal wavelengths and waves not too far from the Lamb and Brunt‐Vaisala (BV) curves. Wave properties are well behaved near the characteristic curve and solutions are linked at the common intersection of the Lamb and BV curves implying that waves should be able to transfer energy from one regime to the other in response to background variations. Nonisothermal calculations show that when lapse rates are large enough waves that are at least partially internal can exist at all frequencies.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2002JD002421</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record> |
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subjects | acoustic waves dispersion Earth, ocean, space evanescence Exact sciences and technology External geophysics Gravity waves group velocity impedance Physics of the high neutral atmosphere Tides, waves, convection, winds, turbulence |
title | A reexamination of evanescent acoustic-gravity waves: Special properties and aeronomical significance |
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