Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone
The Arctic seas are in a period of transition as they adjust to stimuli from anthropogenic climate change. The acoustic response to this adjustment is of fundamental interest, as acoustics provide an important means for Arctic remote sensing, communication and navigation, and there are important bio...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:6226d9ab16d74da2a254da41abdf69ff 2023-05-15T14:53:03+02:00 Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone Dominic DiMaggio John A. Colosi John Joseph Annalise Pearson Peter F. Worcester Matthew A. Dzieciuch 2018-04-01 https://doi.org/10.1525/elementa.186 https://doaj.org/article/6226d9ab16d74da2a254da41abdf69ff en eng BioOne 2325-1026 doi:10.1525/elementa.186 https://doaj.org/article/6226d9ab16d74da2a254da41abdf69ff undefined Elementa: Science of the Anthropocene, Vol 6, Iss 1 (2018) acoustics observations Arctic Ocean Canada Basin marginal ice zone geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.1525/elementa.186 2023-01-22T19:28:45Z The Arctic seas are in a period of transition as they adjust to stimuli from anthropogenic climate change. The acoustic response to this adjustment is of fundamental interest, as acoustics provide an important means for Arctic remote sensing, communication and navigation, and there are important biological implications for marine mammals and other organisms that use sound. The Canada Basin Acoustic Propagation Experiment (CANAPE) is an effort to study Arctic acoustics; this paper reports on ocean sound-speed measurements from a pilot study undertaken between 30 July and 16 August 2015. Moored and shipborne observations of temperature and salinity were made in the upper 600 m of the ocean, allowing analysis along isopycnals (surfaces of constant density) to separate sound-speed structure due to internal-wave-induced vertical displacements from those originating from density-compensated temperature and salinity variations termed spice. Frequency spectra and vertical covariance functions were used to describe the space/time scales of displacements and spice. Internal-wave frequency spectra show a spectral slope much lower than the Garrett-Munk model, with the energy level roughly 4% of the standard Garrett-Munk value. Frequency spectra of spice show a form similar to the internal-wave spectra but with a slightly steeper spectral slope, presumably due to the horizontal advection of the spice by internal-wave currents. The root mean square sound-speed fluctuations from internal waves were small with values less than 0.1 m s–1. Spicy sound-speed fluctuations were much stronger, particularly in the upper 100 m where a maximum of 0.25 m s–1 was observed. Both processes have vertical decorrelation lengths less than 100 m. The observed strong variations in vertical and horizontal sound-speed structure will have significant impacts on acoustic applications, especially in the realm of communications, navigation, and remote sensing. Article in Journal/Newspaper Arctic Arctic Ocean canada basin Climate change Unknown Arctic Arctic Ocean Canada Munk ENVELOPE(-95.993,-95.993,55.979,55.979) Elementa: Science of the Anthropocene 6 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
acoustics observations Arctic Ocean Canada Basin marginal ice zone geo envir |
spellingShingle |
acoustics observations Arctic Ocean Canada Basin marginal ice zone geo envir Dominic DiMaggio John A. Colosi John Joseph Annalise Pearson Peter F. Worcester Matthew A. Dzieciuch Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone |
topic_facet |
acoustics observations Arctic Ocean Canada Basin marginal ice zone geo envir |
description |
The Arctic seas are in a period of transition as they adjust to stimuli from anthropogenic climate change. The acoustic response to this adjustment is of fundamental interest, as acoustics provide an important means for Arctic remote sensing, communication and navigation, and there are important biological implications for marine mammals and other organisms that use sound. The Canada Basin Acoustic Propagation Experiment (CANAPE) is an effort to study Arctic acoustics; this paper reports on ocean sound-speed measurements from a pilot study undertaken between 30 July and 16 August 2015. Moored and shipborne observations of temperature and salinity were made in the upper 600 m of the ocean, allowing analysis along isopycnals (surfaces of constant density) to separate sound-speed structure due to internal-wave-induced vertical displacements from those originating from density-compensated temperature and salinity variations termed spice. Frequency spectra and vertical covariance functions were used to describe the space/time scales of displacements and spice. Internal-wave frequency spectra show a spectral slope much lower than the Garrett-Munk model, with the energy level roughly 4% of the standard Garrett-Munk value. Frequency spectra of spice show a form similar to the internal-wave spectra but with a slightly steeper spectral slope, presumably due to the horizontal advection of the spice by internal-wave currents. The root mean square sound-speed fluctuations from internal waves were small with values less than 0.1 m s–1. Spicy sound-speed fluctuations were much stronger, particularly in the upper 100 m where a maximum of 0.25 m s–1 was observed. Both processes have vertical decorrelation lengths less than 100 m. The observed strong variations in vertical and horizontal sound-speed structure will have significant impacts on acoustic applications, especially in the realm of communications, navigation, and remote sensing. |
format |
Article in Journal/Newspaper |
author |
Dominic DiMaggio John A. Colosi John Joseph Annalise Pearson Peter F. Worcester Matthew A. Dzieciuch |
author_facet |
Dominic DiMaggio John A. Colosi John Joseph Annalise Pearson Peter F. Worcester Matthew A. Dzieciuch |
author_sort |
Dominic DiMaggio |
title |
Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone |
title_short |
Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone |
title_full |
Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone |
title_fullStr |
Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone |
title_full_unstemmed |
Observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 Canada Basin marginal ice zone |
title_sort |
observations of thermohaline sound-speed structure induced by internal waves and spice in the summer 2015 canada basin marginal ice zone |
publisher |
BioOne |
publishDate |
2018 |
url |
https://doi.org/10.1525/elementa.186 https://doaj.org/article/6226d9ab16d74da2a254da41abdf69ff |
long_lat |
ENVELOPE(-95.993,-95.993,55.979,55.979) |
geographic |
Arctic Arctic Ocean Canada Munk |
geographic_facet |
Arctic Arctic Ocean Canada Munk |
genre |
Arctic Arctic Ocean canada basin Climate change |
genre_facet |
Arctic Arctic Ocean canada basin Climate change |
op_source |
Elementa: Science of the Anthropocene, Vol 6, Iss 1 (2018) |
op_relation |
2325-1026 doi:10.1525/elementa.186 https://doaj.org/article/6226d9ab16d74da2a254da41abdf69ff |
op_rights |
undefined |
op_doi |
https://doi.org/10.1525/elementa.186 |
container_title |
Elementa: Science of the Anthropocene |
container_volume |
6 |
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1766324471410458624 |