Analysis of Acoustic Data Under Response of Sperm Whales to Air Gun Sounds in the Gulf of Mexico

2004 ◽  
Author(s):  
Aaron M. Thode
2021 ◽  
Vol 9 (5) ◽  
pp. 454
Author(s):  
Kun Li ◽  
Natalia A. Sidorovskaia ◽  
Thomas Guilment ◽  
Tingting Tang ◽  
Christopher O. Tiemann

Passive acoustic monitoring has been successfully used to study deep-diving marine mammal populations. To assess regional population trends of sperm whales in the northern Gulf of Mexico (GoM), including impacts of the Deepwater Horizon platform oil spill in 2010, the Littoral Acoustic Demonstration Center-Gulf Ecological Monitoring and Modeling (LADC-GEMM) consortium collected broadband acoustic data in the Mississippi Valley/Canyon area between 2007 and 2017 using bottom-anchored moorings. These data allow the inference of short-term and long-term variations in site-specific abundances of sperm whales derived from their acoustic activity. A comparison is made between the abundances of sperm whales at specific sites in different years before and after the oil spill by estimating the regional abundance density. The results show that sperm whales were present in the region throughout the entire monitoring period. A habitat preference shift was observed for sperm whales after the 2010 oil spill with higher activities at sites farther away from the spill site. A comparison of the 2007 and 2015 results shows that the overall regional abundance of sperm whales did not recover to pre-spill levels. The results indicate that long-term spatially distributed acoustic monitoring is critical in characterizing sperm whale population changes and in understanding how environmental stressors impact regional abundances and the habitat use of sperm whales.


Geophysics ◽  
1988 ◽  
Vol 53 (11) ◽  
pp. 1388-1398 ◽  
Author(s):  
William H. Dragoset

Marine seismic data acquired with a moving vibrator suffer phase dispersion caused by Doppler shifting of the source sweep function. The dispersion for a particular reflection event depends upon frequency, the type of sweep function, and the Doppler factor associated with that event. Synthetic vibrator data show that, at typical ship speeds, the Doppler factors for steeply dipping events are big enough to cause phase dispersion as large as several hundred degrees. If unaccounted for, such dispersive effects could make a moving marine vibrator unacceptable for imaging steep dips. In a constant‐offset section, the Doppler factor for a reflection event is the product of ship speed and the event’s time dip. That key, simple relationship allows a two‐dimensional f-k filter to remove the phase dispersion caused by the Doppler effect. Comparisons of both synthetic data and Gulf of Mexico field data, before and after application of the phase‐correcting filter, show that the filter improves steep‐dip imaging in marine vibrator data. For the Gulf of Mexico line, steep dips are imaged just as well in the phase‐corrected vibrator data as in air‐gun data.


2006 ◽  
Vol 12 (4) ◽  
pp. 588-594 ◽  
Author(s):  
David W. Weller ◽  
Bernd Würsig ◽  
Hal Whitehead ◽  
Jeffrey C. Norris ◽  
Spencer K. Lynn ◽  
...  

2020 ◽  
Vol 161 ◽  
pp. 111627
Author(s):  
Janelle L. Morano ◽  
Jamey T. Tielens ◽  
Charles A. Muirhead ◽  
Bobbi J. Estabrook ◽  
Patrick J. Sullivan ◽  
...  

2019 ◽  
Vol 6 ◽  
Author(s):  
John A. Hildebrand ◽  
Kaitlin E. Frasier ◽  
Simone Baumann-Pickering ◽  
Sean M. Wiggins ◽  
Karlina P. Merkens ◽  
...  

2022 ◽  
Vol 41 (1) ◽  
pp. 9-18
Author(s):  
Andrew Brenders ◽  
Joe Dellinger ◽  
Imtiaz Ahmed ◽  
Esteban Díaz ◽  
Mariana Gherasim ◽  
...  

The promise of fully automatic full-waveform inversion (FWI) — a (seismic) data-driven velocity model building process — has proven elusive in complex geologic settings, with impactful examples using field data unavailable until recently. In 2015, success with FWI at the Atlantis Field in the U.S. Gulf of Mexico demonstrated that semiautomatic velocity model building is possible, but it also raised the question of what more might be possible if seismic data tailor-made for FWI were available (e.g., with increased source-receiver offsets and bespoke low-frequency seismic sources). Motivated by the initial value case for FWI in settings such as the Gulf of Mexico, beginning in 2007 and continuing into 2021 BP designed, built, and field tested Wolfspar, an ultralow-frequency seismic source designed to produce seismic data tailor-made for FWI. A 3D field trial of Wolfspar was conducted over the Mad Dog Field in the Gulf of Mexico in 2017–2018. Low-frequency source (LFS) data were shot on a sparse grid (280 m inline, 2 to 4 km crossline) and recorded into ocean-bottom nodes simultaneously with air gun sources shooting on a conventional dense grid (50 m inline, 50 m crossline). Using the LFS data with FWI to improve the velocity model for imaging produced only incremental uplift in the subsalt image of the reservoir, albeit with image improvements at depths greater than 25,000 ft (approximately 7620 m). To better understand this, reprocessing and further analyses were conducted. We found that (1) the LFS achieved its design signal-to-noise ratio (S/N) goals over its frequency range; (2) the wave-extrapolation and imaging operators built into FWI and migration are very effective at suppressing low-frequency noise, so that densely sampled air gun data with a low S/N can still produce useable model updates with low frequencies; and (3) data density becomes less important at wider offsets. These results may have significant implications for future acquisition designs with low-frequency seismic sources going forward.


2015 ◽  
Vol 41 (3) ◽  
pp. 252-255 ◽  
Author(s):  
Amy D. Whitt ◽  
Melody A. Baran ◽  
Maurice Bryson ◽  
Luke E. Rendell

1985 ◽  
Vol 30 (1) ◽  
pp. 101 ◽  
Author(s):  
Laura A. Collum ◽  
Thomas H. Fritts
Keyword(s):  

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