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OBSIP Overview Instrumentation Centers: Lamont-Doherty Earth Observatory A. Barclay, J. Gaherty, M. Tolstoy Scripps Institution of Oceanography J. Babcock, A. Harding, G. Kent, J. Orcutt Woods Hole Oceanographic Institution J. Collins, K. Peal, B. Wooding Oversight Committee: Doug Toomey, Chair, Oregon Rob Dunn, Hawaii Jim Fowler, IRIS Gail Christeson, Texas Francis Wu, Binghamton ed by the NSF, Marine Geology and Geophysics Progra . Collins, J. Gaherty, D. Toomey arthScope National Meeting, May 12, 2009 www.obsip.org

OBSIP Overview

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www.obsip.org. OBSIP Overview. Instrumentation Centers: Lamont-Doherty Earth Observatory A. Barclay, J. Gaherty, M. Tolstoy Scripps Institution of Oceanography J. Babcock, A. Harding, G. Kent, J. Orcutt Woods Hole Oceanographic Institution J. Collins, K. Peal, B. Wooding. - PowerPoint PPT Presentation

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Page 1: OBSIP Overview

OBSIP OverviewInstrumentation Centers:Lamont-Doherty Earth Observatory

A. Barclay, J. Gaherty, M. Tolstoy

Scripps Institution of OceanographyJ. Babcock, A. Harding, G. Kent, J. Orcutt

Woods Hole Oceanographic Institution

J. Collins, K. Peal, B. Wooding

Oversight Committee:Doug Toomey, Chair, OregonRob Dunn, HawaiiJim Fowler, IRISGail Christeson, TexasFrancis Wu, Binghamton

Funded by the NSF, Marine Geology and Geophysics Program

J. Collins, J. Gaherty, D. ToomeyEarthScope National Meeting, May 12, 2009

www.obsip.org

Page 2: OBSIP Overview

• 1999: NSF-OCE funds new OBS designs and establishes U.S. National Ocean Bottom Seismic Instrumentation Pool (OBSIP).

• OBSIP is charged by NSF with providing state-of-the-art ocean-bottom seismic instrumentation and at-sea technical assistance for the collection of marine seismic data by the entire U.S. scientific community.

• Members are WHOI, SIO, and LDEO. To date (April 2009), 37 separate field program supported, involving 71 research cruises. Subscribed through 2011.

• OBSIP is funded via Cooperative Agreements with WHOI, SIO, and LDEO. Members receive modest annual, non-project specific, base suppot to maintain/upgrade their OBS fleet; all other support is tied to funded field programs.

Ocean Bottom Seismology in the U.S.

www.obsip.org

Page 3: OBSIP Overview

As of April 2009, OBSIP (WHOI,SIO, LDEO) has supported 37 separate field program, involving 71 research cruises. Red stars show locations of passive deployments; orange circles show locations of active-source experiments.

OBSIP Experiments 2001-2009

www.obsip.org

Page 4: OBSIP Overview

Instrumentation

Broad Band instruments

• 3-component seismometer spanning 0.01-10 Hz or better

• wide-band differential pressure gauge (DPG) and/or hydrophone

• High-resolution (24 bit) A/D seismograph

• 1+ year recording at 20-40 Hz

Short Period Broad Band

LDEO - 30

SIO 67 41

WHOI 29 32

Total 96 103

Short Period instruments

• Vertical-component 2-4 Hz seismometer

• Hydrophone

• 24 bit A/D seismograph

• 60+ day recording at 200 Hz or betterMore info at

http://www.obsip.org

www.obsip.org

Page 5: OBSIP Overview

SIO BB

WHOI BB

LDEO BB

www.obsip.org

Page 6: OBSIP Overview

Challenges and Limitations• Free-fall design

– No control on seismometer placement (poor coupling)

– Susceptible to bottom currents (tilt noise) and trawling• Poor performance of horizontal components

• Long-duration deployments limited to depths greater than 1000 m, even greater in heavy fishing regions

– High risk with many potential failure points

• Glass flotation – maximum depth ~6000 m

• No GPS timing – clock drift rates of 2-5 ms/day

• No SOH, no intermediate data recovery

www.obsip.org

Page 7: OBSIP Overview

New Developments • Trawl-resistant mounts

– Allow for shallow (shelf) deployments

• Sub-seafloor burial system– Improve noise characteristics in both shallow and deep water

• Ultra broad-band bottom-pressure sensors– Detect vertical deformation with 1 mm precision from DC to 10 Hz

• Three-component accelerometers – On-scale near-fault deployment

• ROV recovery– Reduce risk of loss and enhance data recovery

• Near-shore buoy telemetry– GPS timing and real-time data recovery

www.obsip.org

Page 8: OBSIP Overview

Borehole

Buried

Seafloor

Seafloor SP

Borehole

Buried

Seafloor

Seafloor SP

Horizontal components on buried seismometer (red traces) are much less noisy at long periods than the horizontal components of an identical seismometer sitting on the seafloor (blue traces).

Performance Gain Achieved by Seismometer Burial

Collins et al., GRL, 2001

www.obsip.org

Page 9: OBSIP Overview

www.obsip.org

Page 10: OBSIP Overview

www.obsip.org

New WHOI Seismometer Burial System

Page 11: OBSIP Overview

Scheduling• Fill out instrument-request form (obsip.org) prior to

proposal submittal– OBSIP provides cost-estimate to be included as supplemental

information in proposal (not in budget)

• Scheduled in order of official funding– In conjunction with ship scheduling

• Non-NSF projects allowed, but have lower priority in scheduling

More info at http://www.obsip.org

www.obsip.org

Page 12: OBSIP Overview

Availability as of Jan 2009Broad-Band

• Fully booked through 2010 (pending ship schedules)– Wiens, Forsyth, Baldwin, Kohler

• ~ 44-52 instruments now scheduled through much of 2011– Baldwin, Kohler, Wiens

Short-Period

• Dependent on cruise schedule of (usually) the Langseth

• In general available for short duration (< 60 day) experiments.

More info at http://www.obsip.org

www.obsip.org

Page 13: OBSIP Overview

http://www.obsip.org

www.obsip.org