Open AccessA new approach to processing and imaging multibeam water column echosounder data: Application to a complex methane seep on the southern Cascadia margin
Author(s) -
A. M. Tréhu,
Jeffrey W. Beeson,
S. G. Merle
Publication year - 2022
Publication title -
interpretation
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.362
H-Index - 25
eISSN - 2324-8866
pISSN - 2324-8858
DOI - 10.1190/int-2021-0195.1
Subject(s) - seafloor spreading , submarine pipeline , flare , geology , echo sounding , backscatter (email) , water column , methane , oceanography , remote sensing , physics , ecology , biology , telecommunications , astrophysics , computer science , wireless
Acoustic echosounding systems are increasingly used to image water-column backscatter in addition to mapping the seafloor. We have imaged an acoustic flare generated by methane bubbles emanating from a vent sourced at 1840 m water depth offshore northern California using a shipboard Kongsberg EM122. Data include five transits over the flare and approximately 11 h of continuous observation when the ship held station. Shipboard observations showed a strong flare splitting into multiple smaller, intermittent flares at a water depth of 800–1200 m and pronounced temporal variability. We introduce a new approach to processing the data in which we correct the backscatter data for ship motion and bin the data into voxels with dimensions of 20 m in X and Y and 40 m in Z for a transit over the flare and into vertical slices with dimensions of 15 m in X and Z and 4 min in time when the ship was stationary. The processed data indicate that the signal is dominated by bubbles emanating from a source region with a diameter of approximately 40 m located on the southern edge of what is likely a ring of sources with a diameter of approximately 600 m. When the ship was stationary, we were able to track an individual pulse rising at a rate of 8–10 m/min. Our results illustrate the limitations of monitoring temporal variation in gas flux using multibeam echosounders because of the trade-off between imaging the entire flare by averaging over tens of minutes to hours and observing a slice through the flare to capture short-lived pulses of gas expulsion. Nevertheless, because echosounders are widely available, they can continue to provide valuable data on the spatial and temporal distribution of gas emissions on continental margins that can be used to frame hypotheses and plan more comprehensive follow-up experiments.