Abstract

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.

Publication Date

2012

Journal or Conference Title

Proceeding of Meetings on Acoustics (POMA)

Volume

17, Issue 1

Pages

1-8

Conference Date

July 2 - July 6, 2012

Publisher Place

Edinburgh, Scotland

Publisher

Acoustical Society of America

Digital Object Identifier (DOI)

10.1121/1.4772948

Document Type

Conference Proceeding

Rights

© 2012 Acoustical Society of America

Share

COinS