Ocean Wave Speed in the Antarctic
The propagation of ocean waves in the marginal ice zone (MIZ) is investigated with the aim of determining whether the loading and scattering of waves by ice floes is significant. Measurements made using instrumented ice floes in the MIZ north of the Ross Sea, Antarctica, during June 1998, are used t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.17.8214 2023-05-15T13:57:03+02:00 Ocean Wave Speed in the Antarctic Colin Fox Mathematics Colin Fox Tim Haskell The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.17.8214 http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.17.8214 http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf dispersion equation marginal ice text ftciteseerx 2016-01-07T16:00:12Z The propagation of ocean waves in the marginal ice zone (MIZ) is investigated with the aim of determining whether the loading and scattering of waves by ice floes is significant. Measurements made using instrumented ice floes in the MIZ north of the Ross Sea, Antarctica, during June 1998, are used to determine the frequency-wavelength relationship for propagating ocean waves in that region. This measured dispersion equation is related to the effective large-scale properties of the MIZ that occur in models for wave propagation and scattering. We present the measured wave speeds to enable estimation of the parameters in these models. Text Antarc* Antarctic Antarctica Ross Sea Unknown Antarctic Ross Sea The Antarctic |
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English |
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dispersion equation marginal ice |
spellingShingle |
dispersion equation marginal ice Colin Fox Mathematics Colin Fox Tim Haskell Ocean Wave Speed in the Antarctic |
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dispersion equation marginal ice |
description |
The propagation of ocean waves in the marginal ice zone (MIZ) is investigated with the aim of determining whether the loading and scattering of waves by ice floes is significant. Measurements made using instrumented ice floes in the MIZ north of the Ross Sea, Antarctica, during June 1998, are used to determine the frequency-wavelength relationship for propagating ocean waves in that region. This measured dispersion equation is related to the effective large-scale properties of the MIZ that occur in models for wave propagation and scattering. We present the measured wave speeds to enable estimation of the parameters in these models. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Colin Fox Mathematics Colin Fox Tim Haskell |
author_facet |
Colin Fox Mathematics Colin Fox Tim Haskell |
author_sort |
Colin Fox Mathematics |
title |
Ocean Wave Speed in the Antarctic |
title_short |
Ocean Wave Speed in the Antarctic |
title_full |
Ocean Wave Speed in the Antarctic |
title_fullStr |
Ocean Wave Speed in the Antarctic |
title_full_unstemmed |
Ocean Wave Speed in the Antarctic |
title_sort |
ocean wave speed in the antarctic |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.17.8214 http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf |
geographic |
Antarctic Ross Sea The Antarctic |
geographic_facet |
Antarctic Ross Sea The Antarctic |
genre |
Antarc* Antarctic Antarctica Ross Sea |
genre_facet |
Antarc* Antarctic Antarctica Ross Sea |
op_source |
http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.17.8214 http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766264647206305792 |