Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads
International audience Eastern Beaufort Sea underwater noise was recorded from September 2005 to October 2006 at two stations, 300 km apart, on Mackenzie shelf break and Amundsen Gulf mouth. The region was ice-covered (> 90%) from November to mid-June. The regional under-ice background ambient no...
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ftccsdartic:oai:HAL:hal-00802079v1 2023-05-15T13:22:56+02:00 Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads Kinda, Bazile Simard, Yvan Gervaise, Cedric Mars, Jerome, Fortier, Louis Extraction et Exploitation de l'Information en Environnements Incertains (E3I2) École Nationale Supérieure de Techniques Avancées Bretagne (ENSTA Bretagne) Institut des Sciences de la Mer Université du Québec à Rimouski (UQAR) GIPSA - Signal Images Physique (GIPSA-SIGMAPHY) Département Images et Signal (GIPSA-DIS) Grenoble Images Parole Signal Automatique (GIPSA-lab) Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Grenoble Images Parole Signal Automatique (GIPSA-lab) Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS) Dept Biologie, Université Laval Université Laval Québec (ULaval) Institut Maurice-Lamontagne Pêches et Oceans Canada ENSTA-Bretagne Vancouver, Canada 2012-12-10 https://hal.archives-ouvertes.fr/hal-00802079 en eng HAL CCSD hal-00802079 https://hal.archives-ouvertes.fr/hal-00802079 ASM 2012 - ArcticNet's eighth Annual Scientific Meeting https://hal.archives-ouvertes.fr/hal-00802079 ASM 2012 - ArcticNet's eighth Annual Scientific Meeting, Dec 2012, Vancouver, Canada. pp.68 [SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processing [INFO.INFO-TS]Computer Science [cs]/Signal and Image Processing info:eu-repo/semantics/conferenceObject Conference papers 2012 ftccsdartic 2021-10-24T15:16:47Z International audience Eastern Beaufort Sea underwater noise was recorded from September 2005 to October 2006 at two stations, 300 km apart, on Mackenzie shelf break and Amundsen Gulf mouth. The region was ice-covered (> 90%) from November to mid-June. The regional under-ice background ambient noise, from a myriad of undistinguishable sources integrated over large ranges, was estimated daily for 3 acoustic bands and correlated with measured wind, in situ mean currents and large-scale ice speed as potential forcings. Correlations were observed between wind and ice drift, and ice drift and surface layer current. Ambient noise level was correlated with all these three variables. The ambient noise correlation with the large-scale ice drift suggests a connexion with the southern part of the large Beaufort gyre. Ice cracking, shearing and colliding add strong transient events above the general ambient noise level. An example of the opening and closing a ~500-km long lead along the large-scale offshore plume of multiyear ice moving along the shelf, is used to evidence the different types of wideband noise and tones, of variable duration, related to these events. Some tones are repeated with a period corresponding to waves and can sometime be confounded with marine mammal songs. These ice noise events are occurring all along the winter, and the most energetic ones correspond to lead openings. Conference Object Amundsen Gulf Beaufort Sea Mackenzie Shelf Sea ice Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Canada |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processing [INFO.INFO-TS]Computer Science [cs]/Signal and Image Processing |
spellingShingle |
[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processing [INFO.INFO-TS]Computer Science [cs]/Signal and Image Processing Kinda, Bazile Simard, Yvan Gervaise, Cedric Mars, Jerome, Fortier, Louis Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads |
topic_facet |
[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processing [INFO.INFO-TS]Computer Science [cs]/Signal and Image Processing |
description |
International audience Eastern Beaufort Sea underwater noise was recorded from September 2005 to October 2006 at two stations, 300 km apart, on Mackenzie shelf break and Amundsen Gulf mouth. The region was ice-covered (> 90%) from November to mid-June. The regional under-ice background ambient noise, from a myriad of undistinguishable sources integrated over large ranges, was estimated daily for 3 acoustic bands and correlated with measured wind, in situ mean currents and large-scale ice speed as potential forcings. Correlations were observed between wind and ice drift, and ice drift and surface layer current. Ambient noise level was correlated with all these three variables. The ambient noise correlation with the large-scale ice drift suggests a connexion with the southern part of the large Beaufort gyre. Ice cracking, shearing and colliding add strong transient events above the general ambient noise level. An example of the opening and closing a ~500-km long lead along the large-scale offshore plume of multiyear ice moving along the shelf, is used to evidence the different types of wideband noise and tones, of variable duration, related to these events. Some tones are repeated with a period corresponding to waves and can sometime be confounded with marine mammal songs. These ice noise events are occurring all along the winter, and the most energetic ones correspond to lead openings. |
author2 |
Extraction et Exploitation de l'Information en Environnements Incertains (E3I2) École Nationale Supérieure de Techniques Avancées Bretagne (ENSTA Bretagne) Institut des Sciences de la Mer Université du Québec à Rimouski (UQAR) GIPSA - Signal Images Physique (GIPSA-SIGMAPHY) Département Images et Signal (GIPSA-DIS) Grenoble Images Parole Signal Automatique (GIPSA-lab) Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Grenoble Images Parole Signal Automatique (GIPSA-lab) Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)-Université Pierre Mendès France - Grenoble 2 (UPMF)-Université Stendhal - Grenoble 3-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS) Dept Biologie, Université Laval Université Laval Québec (ULaval) Institut Maurice-Lamontagne Pêches et Oceans Canada ENSTA-Bretagne |
format |
Conference Object |
author |
Kinda, Bazile Simard, Yvan Gervaise, Cedric Mars, Jerome, Fortier, Louis |
author_facet |
Kinda, Bazile Simard, Yvan Gervaise, Cedric Mars, Jerome, Fortier, Louis |
author_sort |
Kinda, Bazile |
title |
Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads |
title_short |
Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads |
title_full |
Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads |
title_fullStr |
Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads |
title_full_unstemmed |
Under-ice noise in Eastern Beaufort Sea: ice drift forcing, fracturing and formation of leads |
title_sort |
under-ice noise in eastern beaufort sea: ice drift forcing, fracturing and formation of leads |
publisher |
HAL CCSD |
publishDate |
2012 |
url |
https://hal.archives-ouvertes.fr/hal-00802079 |
op_coverage |
Vancouver, Canada |
geographic |
Canada |
geographic_facet |
Canada |
genre |
Amundsen Gulf Beaufort Sea Mackenzie Shelf Sea ice |
genre_facet |
Amundsen Gulf Beaufort Sea Mackenzie Shelf Sea ice |
op_source |
ASM 2012 - ArcticNet's eighth Annual Scientific Meeting https://hal.archives-ouvertes.fr/hal-00802079 ASM 2012 - ArcticNet's eighth Annual Scientific Meeting, Dec 2012, Vancouver, Canada. pp.68 |
op_relation |
hal-00802079 https://hal.archives-ouvertes.fr/hal-00802079 |
_version_ |
1766367989445165056 |