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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Main Authors: Colin Fox Mathematics, Colin Fox, Tim Haskell
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.17.8214
http://www.math.auckland.ac.nz/~fox/publications/cdpreprint.pdf
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spelling 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
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic dispersion equation
marginal ice
spellingShingle dispersion equation
marginal ice
Colin Fox Mathematics
Colin Fox
Tim Haskell
Ocean Wave Speed in the Antarctic
topic_facet 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.
author2 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
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