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Title: Measured and modeled acoustic propagation underneath the rough Arctic sea-ice

Abstract

A characteristic surface duct beneath the sea-ice in the Marginal Ice Zone causes acoustic waves to be trapped and continuously interact with the sea-ice. The reflectivity of the sea-ice depends on the thickness, the elastic properties, and its roughness. This work focuses on the influence of sea-ice roughness on long-range acoustic propagation, and on how well the arrival structure can be predicted by the full wave integration model OASES. In 2013, acoustic signals centered at 900 Hz were transmitted every hour for three days between ice-tethered buoys in a drifting network in the Fram Strait. The experiment was set up to study the signal stability in the surface channel below the sea-ice. Oceanographic profiles were collected during the experiment, while a statistical description of the rough sea-ice was established based on historical ice-draft measurements. This environmental description is used as input to the range independent version of OASES. The model simulations correspond fairly well with the observations, despite that a flat bathymetry is used and the sea-ice roughness cannot be fully approximated by the statistical representation used in OASES. Long-range transmissions around 900 Hz are found to be more sensitive to the sea-ice roughness than the elastic parameters.

Authors:
 [1];  [1];  [1];  [1];  [2]
  1. Nansen Environmental and Remote Sensing Center, Bergen (Norway)
  2. Woods Hole Research Center, Falmouth, MA (United States)
Publication Date:
Research Org.:
Lawrence Berkeley National Laboratory-National Energy Research Scientific Computing Center
Sponsoring Org.:
USDOE
OSTI Identifier:
1524053
Resource Type:
Journal Article
Journal Name:
Journal of the Acoustical Society of America
Additional Journal Information:
Journal Volume: 142; Journal Issue: 3; Journal ID: ISSN 0001-4966
Publisher:
Acoustical Society of America
Country of Publication:
United States
Language:
English

Citation Formats

Hope, Gaute, Sagen, Hanne, Storheim, Espen, Hobæk, Halvor, and Freitag, Lee. Measured and modeled acoustic propagation underneath the rough Arctic sea-ice. United States: N. p., 2017. Web. doi:10.1121/1.5003786.
Hope, Gaute, Sagen, Hanne, Storheim, Espen, Hobæk, Halvor, & Freitag, Lee. Measured and modeled acoustic propagation underneath the rough Arctic sea-ice. United States. doi:10.1121/1.5003786.
Hope, Gaute, Sagen, Hanne, Storheim, Espen, Hobæk, Halvor, and Freitag, Lee. Fri . "Measured and modeled acoustic propagation underneath the rough Arctic sea-ice". United States. doi:10.1121/1.5003786.
@article{osti_1524053,
title = {Measured and modeled acoustic propagation underneath the rough Arctic sea-ice},
author = {Hope, Gaute and Sagen, Hanne and Storheim, Espen and Hobæk, Halvor and Freitag, Lee},
abstractNote = {A characteristic surface duct beneath the sea-ice in the Marginal Ice Zone causes acoustic waves to be trapped and continuously interact with the sea-ice. The reflectivity of the sea-ice depends on the thickness, the elastic properties, and its roughness. This work focuses on the influence of sea-ice roughness on long-range acoustic propagation, and on how well the arrival structure can be predicted by the full wave integration model OASES. In 2013, acoustic signals centered at 900 Hz were transmitted every hour for three days between ice-tethered buoys in a drifting network in the Fram Strait. The experiment was set up to study the signal stability in the surface channel below the sea-ice. Oceanographic profiles were collected during the experiment, while a statistical description of the rough sea-ice was established based on historical ice-draft measurements. This environmental description is used as input to the range independent version of OASES. The model simulations correspond fairly well with the observations, despite that a flat bathymetry is used and the sea-ice roughness cannot be fully approximated by the statistical representation used in OASES. Long-range transmissions around 900 Hz are found to be more sensitive to the sea-ice roughness than the elastic parameters.},
doi = {10.1121/1.5003786},
journal = {Journal of the Acoustical Society of America},
issn = {0001-4966},
number = 3,
volume = 142,
place = {United States},
year = {2017},
month = {9}
}