Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders

When in the form of free gas in the water column, methane seeps emanating from the seabed are strong acoustic targets that are often detectable from surface vessels using echo sounders.In addition to detecting that a seep is present at some location, it is also desirable to characterize the nature o...

Full description

Bibliographic Details
Main Authors: Weber, Thomas C., Jerram, Kevin W., Mayer, Larry A.
Format: Text
Language:unknown
Published: University of New Hampshire Scholars' Repository 2012
Subjects:
Online Access:https://scholars.unh.edu/ccom/833
https://scholars.unh.edu/cgi/viewcontent.cgi?article=1833&context=ccom
id ftuninhampshire:oai:scholars.unh.edu:ccom-1833
record_format openpolar
spelling ftuninhampshire:oai:scholars.unh.edu:ccom-1833 2023-05-15T17:12:02+02:00 Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders Weber, Thomas C. Jerram, Kevin W. Mayer, Larry A. 2012-01-01T08:00:00Z application/pdf https://scholars.unh.edu/ccom/833 https://scholars.unh.edu/cgi/viewcontent.cgi?article=1833&context=ccom unknown University of New Hampshire Scholars' Repository https://scholars.unh.edu/ccom/833 https://scholars.unh.edu/cgi/viewcontent.cgi?article=1833&context=ccom © 2012 Acoustical Society of America Center for Coastal and Ocean Mapping gas seeps Gulf of Mexico Oceanography and Atmospheric Sciences and Meteorology text 2012 ftuninhampshire 2023-01-30T21:33:15Z When in the form of free gas in the water column, methane seeps emanating from the seabed are strong acoustic targets that are often detectable from surface vessels using echo sounders.In addition to detecting that a seep is present at some location, it is also desirable to characterize the nature of the seep in terms of its morphology and flux rates. Here, we examine how much we can learn about seeps in the deep (> 1000 m) northern Gulf of Mexico using narrow-band split-beam echo sounders operating at fixed frequencies (18 kHz and 38 kHz).Methane seeps in this region are deeper than the methane hydrate stability zone, implying that bubbles of free gas form hydrate rinds that allow them to rise further in the water column than they otherwise would. While this behavior may aid in the classification of gas types in the seep, it is possible that the presence of hydrate rinds may also change the acoustic response of the bubbles and thereby make flux rate estimates more challenging. These and other aspects of seep characterization will be discussed. Text Methane hydrate University of New Hampshire: Scholars Repository
institution Open Polar
collection University of New Hampshire: Scholars Repository
op_collection_id ftuninhampshire
language unknown
topic gas seeps
Gulf of Mexico
Oceanography and Atmospheric Sciences and Meteorology
spellingShingle gas seeps
Gulf of Mexico
Oceanography and Atmospheric Sciences and Meteorology
Weber, Thomas C.
Jerram, Kevin W.
Mayer, Larry A.
Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
topic_facet gas seeps
Gulf of Mexico
Oceanography and Atmospheric Sciences and Meteorology
description When in the form of free gas in the water column, methane seeps emanating from the seabed are strong acoustic targets that are often detectable from surface vessels using echo sounders.In addition to detecting that a seep is present at some location, it is also desirable to characterize the nature of the seep in terms of its morphology and flux rates. Here, we examine how much we can learn about seeps in the deep (> 1000 m) northern Gulf of Mexico using narrow-band split-beam echo sounders operating at fixed frequencies (18 kHz and 38 kHz).Methane seeps in this region are deeper than the methane hydrate stability zone, implying that bubbles of free gas form hydrate rinds that allow them to rise further in the water column than they otherwise would. While this behavior may aid in the classification of gas types in the seep, it is possible that the presence of hydrate rinds may also change the acoustic response of the bubbles and thereby make flux rate estimates more challenging. These and other aspects of seep characterization will be discussed.
format Text
author Weber, Thomas C.
Jerram, Kevin W.
Mayer, Larry A.
author_facet Weber, Thomas C.
Jerram, Kevin W.
Mayer, Larry A.
author_sort Weber, Thomas C.
title Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
title_short Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
title_full Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
title_fullStr Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
title_full_unstemmed Acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
title_sort acoustic sensing of gas seeps in the deep ocean with split-beam echosounders
publisher University of New Hampshire Scholars' Repository
publishDate 2012
url https://scholars.unh.edu/ccom/833
https://scholars.unh.edu/cgi/viewcontent.cgi?article=1833&context=ccom
genre Methane hydrate
genre_facet Methane hydrate
op_source Center for Coastal and Ocean Mapping
op_relation https://scholars.unh.edu/ccom/833
https://scholars.unh.edu/cgi/viewcontent.cgi?article=1833&context=ccom
op_rights © 2012 Acoustical Society of America
_version_ 1766068786490769408