Model-based Estimation of Noise Impact Zones for Deep Offshore Seismic Surveys Alexander MacGillivray, Marie-Noël R. Matthews JASCO Applied Sciences,

Slides:



Advertisements
Similar presentations
Advanced Acoustical Modeling Tools for ESME
Advertisements

Christopher O. Tiemann Michael B. Porter Science Applications International Corporation John A. Hildebrand Scripps Institution of Oceanography Automated.
Ocean Observation, Climate Change and Disaster Warning: the Context David Meldrum Consultant, IOC/UNESCO, Paris
NNMREC Estimating the Acoustic Impact of a Tidal Energy Project Chris Bassett, Jim Thomson, and Brian Polagye University of Washington Mechanical Engineering.
NVC0901 Maritime Alliance Symposium San Diego, August 2011 By: Michael Broadbent Fugro Pelagos Inc. Seafloor Mapping Technologies.
NNMREC National Marine Renewable Energy Centers Hawaii National Marine Renewable Energy Center (HINMREC) University of Hawaii Wave, OTEC Southeast National.
Val Veirs Colorado College Colorado Springs, CO, Scott Veirs Beam Reach marine science and sustainability school Seattle, WA,
Monitoring Processes at Sea using Underwater Sound Jeffrey Nystuen Marie Curie International Fellow Hellenic Center for Marine Research and Principal Oceanographer.
NNMREC November 5, 2010 Northwest National Marine Renewable Energy Center Standards and Protocols for Environmental Assessment Renewable Ocean Energy and.
NNMREC Summary for Congressman Dave Reichart April 22, 2011 Northwest National Marine Renewable Energy Center University of Washington
Tsunamis Detection The Mission  Tsunamis Detection can help to minimize loss of life and property from future tsunamis. Mission Introduction Mechanism.
NNMREC Passive Acoustic Monitoring for Tidal Energy Projects Brian Polagye, Chris Bassett, and Jim Thomson University of Washington Northwest National.
Seismic reflection Seismic reflection profiling basically same principle as echo sounding But lower frequency used for greater subbottom penetration Trade.
ACOUSTIC SIGNATURES Oğuzhan U. BAŞKURT B. Sertaç SERBEST.
Kay Graf Physics Institute University of Erlangen TeV Particle Astrophysics II Madison, WI, USA August 28 – 31, 2006 Towards Acoustic Detection of UHE.
Listening to the Sound: Ambient Noise in Admiralty Inlet
Long-Term Ambient Noise Statistics in the Gulf of Mexico Mark A. Snyder & Peter A. Orlin Naval Oceanographic Office Stennis Space Center, MS Anthony I.
Barrow’s Arctic Ocean Developing a Cabled Seafloor Observatory to Complement the Barrow Global Climate Change Facility the “BGCCRF” Developing a Cabled.
NNMREC November 4, 2010 Passive Acoustics New Environmental Technologies Renewable Ocean Energy and the Marine Environment Brian Polagye, Chris Bassett,
VESSEL NOISE AND ORCA VOCALIZATION: IMPLICATIONS FOR POLICY ALEXANDRA KOUGENTAKIS BEAM REACH FALL beamreach.org/071.
Overview of Oil & Gas Sector The following slides are not a tutorial but merely an overview of the various phases involved in an oil & gas development.
-for saving innocent lives
Tsunami Warning System Elements IOC Assessment Mission to Indonesia 29 August-1 September 2005.
NNMREC April 20, 2011 Ambient Noise in Admiralty Inlet Chris Bassett, Brian Polagye, and Jim Thomson University of Washington Northwest National Marine.
Patrick Lazar, Tausif Shaikh, Johanna Thomas, Kaleel Mahmood
Northwest National Marine Renewable Energy Center Brian Polagye NW National Marine Renewable Energy Center Tidal Hydrokinetic Energy Overview Western Energy.
Page 1 CONSULTANCY AND RESEARCH IN AQUACULTURE AND THE AQUATIC ENVIRONMENT A Company in the NIVA-group Methodology for Environmental monitoring of aquaculture.
Ensemble-variational sea ice data assimilation Anna Shlyaeva, Mark Buehner, Alain Caya, Data Assimilation and Satellite Meteorology Research Jean-Francois.
Satellite-derived bathymetry (SDB) over the North Slope of Alaska, USA JHC/CCOM NOAA/NOS/OCS/MCD.
Joint Industry Program (JIP) Acoustic Research Roger L. Gentry, Ph. D. ProScience Consulting, LLC
A PILOT EXPERIMENT ON THE TEMPORAL VARIABILITY OF THE NEPHELOID AND DYNAMICAL STRUCTURES IN THE BESOS CANYON (NW MEDITERRANEAN SEA) [1] Instituto de Ciencias.
The role of gliders in sustained observations of the ocean Deliverable 4.1 or WP 4.
A method whereby, in contrast to conventional marine seismic (towed streamer) acquisition, acoustic reflections are recorded by receivers placed on the.
Statistics of broadband transmissions through a range-dependent fluctuating ocean waveguide Mark Andrews and Purnima Ratilal; Northeastern University,
Final General Assembly – Paris, France – September 19, 2014 FP7-Infra : Design studies for European Research Infrastrutures 1st October 2011.
J.R. Marko and D.B. Fissel ASL Environmental Sciences Inc. Sidney B.C. Canada Martin Jasek BC Hydro Ltd. ASL Shallow Water Ice Profiler SWIP-5.
HOW DO WE STUDY THE SEAFLOOR?. 1. Line-sounding – starting around 85 B.C. lead weighted ropes were dropped over the side of the boat and the depth was.
Hydroacoustics ODOT Hydroacoustic Work Group Agreement on Thresholds Specifications Effects to fish Attenuation Monitoring and Reporting Information needs.
6/6/07 1 Sources of Anthropogenic Sound in the Ocean John Hildebrand Scripps Institution of Oceanography University of California San Diego Capital Hill.
SAN DIEGO 16/11/2010 Contact: Philippe Plantevin - Website : Tél. +33 (0)4.
Momo An Anni Eloyan Heather Wright Geology 12 #7341
CHAPTER 5: Data sampling design, data quality, calibration, presentation Sampling Physical variables are continuous, but samples (water samples) and digital.
Evaluation of the Real-Time Ocean Forecast System in Florida Atlantic Coastal Waters June 3 to 8, 2007 Matthew D. Grossi Department of Marine & Environmental.
Time (s) Angle (degrees) Pump via bottom reflection Pump via surface reflection Pump Drag head Underwater Anthropogenic.
The Global Ocean The Vast World Ocean.
Universitat Politècnica de Catalunya Michel André MEUST: Real-time Monitoring of Noise and Acoustic Events in Cetacean Acoustic Niches.
Ice-Based Observatories network in the Arctic Ocean Andrey Proshutinsky, Woods Hole Oceanographic Institution NOAA Arctic Science Priorities Workshop,
SIDE SCAN Theory and Operation
Offshore Central Coastal California Seismic Imaging Project April 4, 2012 Central Coastal California Seismic Imaging Program September 10, 2012.
NEMO-O DE NEMO First results from the NEMO Test Site G. Riccobene, for the NEMO Collaboration The NEMO Collaboration is performing the Phase 1 of the project,
Evaluation of SVP-BW drifters thanks to deployments near moored buoys DBCP-18 workshop - Martinique October 2002 By Pierre Blouch Presentation :
SIDE SCAN OVERVIEW. Sidescan Survey Overview A sidescan sonar can be used for a wide variety of survey operations. Search and recovery Geological Identification.
Andrea Kaiser-Weiss, Melbourne Joint GHRSST Workshop, 6 th March 2012 Experiences with SST profiles from near-surface Argo measurements A. Kaiser-Weiss.
Dutch program offshore wind energy Cumulative effects and Mitigation measures ORELG 4 february 2016.
UNDERWATER WIRELESS COMMUNICATION
Web - Mail – Sound Sensors Market Forecast ( )
Acoustic Telemetry Tagging Hillary Sinnott SCM 330 March 12, 2008 Hillary Sinnott SCM 330 March 12, 2008.
SIDE SCAN Theory and Operation
Environmental Studies Program 1  The Studies Program functions to establish information needed for assessment and management of impacts from OCS exploration,
© 2014 Pearson Education, Inc. Marine Provinces Chapter 1 Clickers Essentials of Oceanography Eleventh Edition Alan P. Trujillo Harold V. Thurman © 2014.
Reverberations: Ocean Acoustics and the Environment
Robert Lahmann VLVnT – Toulon – 24-April-2008
Sound Source Verification
Ocean Instrumentation
PARAMETRIC SUB-BOTTOM PROFILER: A NEW APPROACH FOR AN OLD PROBLEM
Underwater wireless communication
OS 72B-0355 Analysis of Acoustic Signals from Ship Traffic at Pioneer Seamount Carl O. Vuosalo,1 Craig Huber,1 Michael D. Hoffman,1 Newell Garfield,2 and.
Preliminary Ideas on Sensor Configurations and Challenges for the Green Cables Christian Meinig.
Real-time Uncertainty Output for MBES Systems
Presentation transcript:

Model-based Estimation of Noise Impact Zones for Deep Offshore Seismic Surveys Alexander MacGillivray, Marie-Noël R. Matthews JASCO Applied Sciences, Victoria BC N ORTHERN O IL AND G AS R ESEARCH F ORUM 2012

Overview The Project: Acoustic modelling and measurement of underwater noise from a deep-water marine seismic survey (Chevron Sirluaq 2012) The Objective: To verify pre-season model estimates of marine mammal exclusion zones for airgun arrays JASCO used computer-based modelling to forecast exclusion zones for marine mammals Our results showed good agreement between modelled and measured sound levels The deep water environment (500 m – 1500 m) was challenging for performing acoustic measurements The Outcome: Showed computer-based modelling is an effective tool for forecasting underwater noise levels from deep-water seismic surveys

Background: Regulatory Context Noise from marine seismic surveys can potentially have negative effects on marine mammals: 1. Behavioural disturbance (harassment) 2. Auditory injury (PTS) Seismic operators implement exclusion zones and other mitigation practices (e.g., soft start) to limit potential impacts In US and Canada, permit applications and environmental assessments require advance estimates of noise impact zones

Marine Mammal Impact Zones Regulatory agencies (e.g., NMFS, DFO) use standard sound pressure level (SPL) thresholds to define noise impact zones Although there are minor differences between Canada and the US, the most commonly applied thresholds are as follows:  Auditory Injury (level A take):  180 dB SPL (rms) re 1 μPa for Whales  190 dB SPL (rms) re 1 μPa for Seals, Walrus, and Bears  Behavioural Disturbance (level B take):  160 dB SPL (rms) re 1 μPa for Whales  120 dB SPL (rms) re 1 μPa for Bowhead cow-calf pairs The size of these zones is not static… different for each survey Sound levels strongly depend on two factors: 1. The sound output of the seismic source (e.g., airgun array design) 2. The environment where the source is operating (e.g., water depth)

Methods for Estimating Impact Zones F IELD M EASUREMENTS During survey operations, sound source verification (SSV) measurements are used to determine distances to impact zones Marine SSVs have been done for nearly all Arctic seismic programs over the last 6 years SSV measurements are carried out at the start of a survey (1-2 weeks to complete, typically) M ODELLING Computer-based prediction tools Underwater sound propagation is very complex Physics-based acoustic models must be used to accurately predict noise footprints Requires detailed description of source and environment  Imperfect knowledge limits model accuracy

Sirluaq 3-D Survey 2012 Chevron conducted Sirluaq 3-D survey in Canadian Beaufort Sea during summer 2012 Survey operator was WesternGeco (M/V Western Neptune) JASCO performed environmental acoustics studies: 1. Pre-season acoustic modelling 2. Sound source verification measurements Sirluaq prospect area (EL460) located in very deep water  Continental slope and ocean basin (> 800 m) Deep ocean = unique measurement and modelling challenges…

Pre-Season Modelling (MONM) JASCO modelled acoustic footprint of airgun arrays (2011) at 5 different locations in survey area using our standard acoustic models: 1. Marine Operations Noise Model 1. Marine Operations Noise Model (MONM) – Propagation Model 2. Airgun Array Source Model 2. Airgun Array Source Model (AASM) – Source Model Model inputs include the following:  High resolution digital bathymetry  Sound speed profiles in water  Geoacoustics of seabed  Airgun array design Maps below show contours of SPL around airguns Sound emissions from airguns are anisotropic  Airgun arrays are directional  Environment is heterogeous

Sound Source Verification JASCO performed SSV measurements at start of Sirluaq survey We measured sound levels during 8-15 Aug 2012 using five autonomous recorders We measured sound levels at distances of 50 m to 50 km Two sets of measurements were carried out in distinct water depth regimes 1. Intermediate depth:  m  Continental slope 2. Deep water:  > 1000 m  Ocean basin M/V Jim Kilabuk

Instrumentation Acoustic sensors were JASCO AMARs  Autonomous Multichannel Acoustic Recorder  Digital underwater sound recorders AMAR configuration:  Calibrated M8E/M8K reference hydrophones  Recording bandwidth: kHz  24-bit 64 kHz audio recording  ~30 days of continuous recording (1 TB) AMAR suspended in water column  Target recording depth m We used two different methods to deploy the AMARs: 1. Moored to bottom at intermediate depth (< 800 m) 2. Towed from vessel in deep water (> 1 km)

Bottom Moored AMARs (< 800 m depth) I NTERMEDIATE D EPTHS AMAR was suspended in water column using floatation and anchor line Tandem acoustic releases were used to retrieve AMAR 5 recorders were deployed simultaneously to measure sound levels at multiple distances and directions from survey line One mooring was lost during intermediate depth measurements  Possible failure of acoustic release system  Four remaining recorders was sufficient to characterize footprint of airgun array

Towed from Vessel (> 1 km depth) D EEP W ATER AMAR was suspended from surface float, connected to vessel via tow line Vessel drifting while recording CTD loggers used to record depth of hydrophone To reduce noise interference from vessel: 1. Vessel drifting with engines off 2. Hydrophone isolated from surface waves with suspension system Sampled at ~15 locations to measure different distances and directions

SSV Measurement Locations

Data Processing Data were downloaded from AMARs after completion of measurements at each site Data were processed using JASCO’s custom data analysis suite: 1. Airgun pulses automatically identified using feature extraction algorithm 2. SPLs for each pulse computed according to standard methods Pistonphone calibrations performed before and after AMAR deployment to ensure accurate sound level reporting

Examples of Airgun Sounds 1 km5 km10 km50 km

Model vs. Data Comparison Plots show comparison of model (black) and data (green)  Plots show data from multiple recording locations  Lower thin line represents SPL at 50 m depth  Distance scale is logarithmic Overall model data agreement was good down to 160 dB SPL  Model accurately predicted propagation loss trend < 20 km  Model predicted shadow zone at ~1-2 km Convergence zone at ~3.5 km range not predicted by MONM – related to imperfect environmental model  Critical reflection from seabed?  Refraction in water column?

Challenges of Deep Water Acoustic Measurements Towed measurements cannot be performed within ~1 km of 3D survey: vessel collision with streamers is major hazard Moorings have many advantages over towed hydrophones:  Multiple instruments can be deployed at once (faster data collection)  Hydrophones can sample very close to airguns (as close as 50 m)  Higher quality acoustic data (less noise) Design of moored hydrophone systems are very complex:  Floatation and instruments must be rated for extreme depths  Long mooring cables must use low-weight, low-drag materials  Deployment of > 1 km mooring from vessel is complex  Accurate positioning of hydrophone is difficult  Greater risk of equipment loss JASCO is developing deep-water mooring designs for future deep-sea SSV measurements

Conclusions Modelling and measurements provide complementary methods for estimating marine mammal impact zones for seismic surveys:  Models allow forecasting of impact zones and noise “footprints”  SSV measurements allow ground-truthing of model estimates  Regulatory compliance often requires that both methods be used Results from Sirluaq 2012 survey show that modelling is an effective method for predicting impact zones in deep water However, acoustic measurements are particularly challenging in deep water environments:  More logistically challenging  Engineering of moorings is more complex  Risk of equipment loss is greater

Questions? Acknowledgements: Thanks to Party Chief and Crew of M/V Western Neptune (WesternGeco)Thanks to Party Chief and Crew of M/V Western Neptune (WesternGeco) Thanks to Captain and Crew of the M/V Jim Kilabuk (NTCL)Thanks to Captain and Crew of the M/V Jim Kilabuk (NTCL)