Anelastic Internal Wave Transmission

An anelastic extension to the Taylor-Goldstein equation is derived and a numerical method is developed to compute the transmission of small amplitude, two-dimensional internal waves in non-rotating, inviscid fluid having arbitrarily specified stratification and background ve-locity. Two particular a...

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Main Authors: J. T. Nault, B. R. Sutherl
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.949
http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.510.949 2023-05-15T16:57:02+02:00 Anelastic Internal Wave Transmission J. T. Nault B. R. Sutherl The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.949 http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.949 http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf text ftciteseerx 2016-01-08T09:38:45Z An anelastic extension to the Taylor-Goldstein equation is derived and a numerical method is developed to compute the transmission of small amplitude, two-dimensional internal waves in non-rotating, inviscid fluid having arbitrarily specified stratification and background ve-locity. Two particular applications are discussed. First, internal waves incident upon a piecewise-linear shear layer are examined and their transmission is computed as a function of the bulk Richardson number, Rib, and the ratio of the density scale height relative to the depth of the shear layer. The waves are found to transmit partially across critical levels if they coincide with heights where the gradient Richardson number is less than 1/4. Transmis-sion is larger if Rib is smaller. Decreasing the density scale height reduces the frequency and wavenumber range over which internal waves propagate, but this does not significantly affect the magnitude of transmission. Second, internal waves generated by flow over Jan Mayen island are examined. Although the waves are ducted, the waves are found to transmit par-tially through the top of the duct. The results are used to interpret the discrepancy between predictions of ray theory and the fully nonlinear numerical simulations of Eckermann et al. 2006. 1 Text Jan Mayen Jan Mayen Island Unknown Jan Mayen Sion ENVELOPE(13.758,13.758,66.844,66.844)
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description An anelastic extension to the Taylor-Goldstein equation is derived and a numerical method is developed to compute the transmission of small amplitude, two-dimensional internal waves in non-rotating, inviscid fluid having arbitrarily specified stratification and background ve-locity. Two particular applications are discussed. First, internal waves incident upon a piecewise-linear shear layer are examined and their transmission is computed as a function of the bulk Richardson number, Rib, and the ratio of the density scale height relative to the depth of the shear layer. The waves are found to transmit partially across critical levels if they coincide with heights where the gradient Richardson number is less than 1/4. Transmis-sion is larger if Rib is smaller. Decreasing the density scale height reduces the frequency and wavenumber range over which internal waves propagate, but this does not significantly affect the magnitude of transmission. Second, internal waves generated by flow over Jan Mayen island are examined. Although the waves are ducted, the waves are found to transmit par-tially through the top of the duct. The results are used to interpret the discrepancy between predictions of ray theory and the fully nonlinear numerical simulations of Eckermann et al. 2006. 1
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author J. T. Nault
B. R. Sutherl
spellingShingle J. T. Nault
B. R. Sutherl
Anelastic Internal Wave Transmission
author_facet J. T. Nault
B. R. Sutherl
author_sort J. T. Nault
title Anelastic Internal Wave Transmission
title_short Anelastic Internal Wave Transmission
title_full Anelastic Internal Wave Transmission
title_fullStr Anelastic Internal Wave Transmission
title_full_unstemmed Anelastic Internal Wave Transmission
title_sort anelastic internal wave transmission
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.949
http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf
long_lat ENVELOPE(13.758,13.758,66.844,66.844)
geographic Jan Mayen
Sion
geographic_facet Jan Mayen
Sion
genre Jan Mayen
Jan Mayen Island
genre_facet Jan Mayen
Jan Mayen Island
op_source http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.949
http://www.math.ualberta.ca/~bruce/papers/igwlinan/reprint_style.pdf
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