Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard

Ambient noise field and propagation in a glacierized Arctic fjord, Kongsfjorden is investigated using time series measurements of noise and Conductivity Temperature Depth (CTD) measurements between July 2015–April 2016. The hydrophone recorded noise for 10 months, with a duty cycle of 1 min every 3...

Full description

Bibliographic Details
Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15102
http://id.nii.ac.jp/1291/00015012/
id ftnipr:oai:nipr.repo.nii.ac.jp:00015102
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00015102 2023-05-15T14:59:18+02:00 Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard 2018-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15102 http://id.nii.ac.jp/1291/00015012/ en eng https://doi.org/10.1016/j.polar.2018.07.003 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15102 http://id.nii.ac.jp/1291/00015012/ Polar Science, 17, 40-49(2018-09) 18739652 Ambient noise variability Sound propagation Sound speed Journal Article 2018 ftnipr https://doi.org/10.1016/j.polar.2018.07.003 2022-12-03T19:43:10Z Ambient noise field and propagation in a glacierized Arctic fjord, Kongsfjorden is investigated using time series measurements of noise and Conductivity Temperature Depth (CTD) measurements between July 2015–April 2016. The hydrophone recorded noise for 10 months, with a duty cycle of 1 min every 3 h, covering summer, fall, winter and spring season. Noise field is seen to be variable with highest levels recorded during summer-fall (112 dB at 0.125 kHz) after which there is a decrease in maximum recorded noise levels. The spectral distribution of noise deviates from the theoretical Gaussian assumption, at varying degrees over the frequency band (0.125–4 kHz). Low frequency band is dominated by marine traffic during summer and fall, and ice wave interactions during winter and spring months. Propagation studies reveal variable nature in propagation with different scenarios observed between seasons. During the summer, refracted paths are observed and a weak channel is formed around the sound channel axis (∼100 m), and a well defined surface duct is revealed during the fall (depth of ∼60 m), characterized by a lower half channel bounded by the sea surface and the sonic layer depth. Surface duct propagation is common in winter with an upward profile and weakens with the onset of spring, as a consequence of the hydrology at the region. The studies will be useful in the context of climate change owing to the critical location of Kongsfjorden which is more prone to experience ongoing warming. Article in Journal/Newspaper Arctic Climate change Kongsfjord* Kongsfjorden Polar Science Polar Science Svalbard National Institute of Polar Research Repository, Japan Arctic Svalbard Polar Science 17 40 49
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Ambient noise variability
Sound propagation
Sound speed
spellingShingle Ambient noise variability
Sound propagation
Sound speed
Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard
topic_facet Ambient noise variability
Sound propagation
Sound speed
description Ambient noise field and propagation in a glacierized Arctic fjord, Kongsfjorden is investigated using time series measurements of noise and Conductivity Temperature Depth (CTD) measurements between July 2015–April 2016. The hydrophone recorded noise for 10 months, with a duty cycle of 1 min every 3 h, covering summer, fall, winter and spring season. Noise field is seen to be variable with highest levels recorded during summer-fall (112 dB at 0.125 kHz) after which there is a decrease in maximum recorded noise levels. The spectral distribution of noise deviates from the theoretical Gaussian assumption, at varying degrees over the frequency band (0.125–4 kHz). Low frequency band is dominated by marine traffic during summer and fall, and ice wave interactions during winter and spring months. Propagation studies reveal variable nature in propagation with different scenarios observed between seasons. During the summer, refracted paths are observed and a weak channel is formed around the sound channel axis (∼100 m), and a well defined surface duct is revealed during the fall (depth of ∼60 m), characterized by a lower half channel bounded by the sea surface and the sonic layer depth. Surface duct propagation is common in winter with an upward profile and weakens with the onset of spring, as a consequence of the hydrology at the region. The studies will be useful in the context of climate change owing to the critical location of Kongsfjorden which is more prone to experience ongoing warming.
format Article in Journal/Newspaper
title Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard
title_short Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard
title_full Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard
title_fullStr Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard
title_full_unstemmed Ambient noise field and propagation in an Arctic fjord Kongsfjorden, Svalbard
title_sort ambient noise field and propagation in an arctic fjord kongsfjorden, svalbard
publishDate 2018
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15102
http://id.nii.ac.jp/1291/00015012/
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Climate change
Kongsfjord*
Kongsfjorden
Polar Science
Polar Science
Svalbard
genre_facet Arctic
Climate change
Kongsfjord*
Kongsfjorden
Polar Science
Polar Science
Svalbard
op_relation https://doi.org/10.1016/j.polar.2018.07.003
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15102
http://id.nii.ac.jp/1291/00015012/
Polar Science, 17, 40-49(2018-09)
18739652
op_doi https://doi.org/10.1016/j.polar.2018.07.003
container_title Polar Science
container_volume 17
container_start_page 40
op_container_end_page 49
_version_ 1766331412056637440