Preliminary Ideas on Sensor Configurations and Challenges for the Green Cables Christian Meinig.

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Preliminary Ideas on Sensor Configurations and Challenges for the Green Cables Christian Meinig

NOAA Pacific Marine Environmental Lab Christian Meinig, NOAA Pacific Marine Environmental Lab Seattle, WA Preliminary Ideas on Sensor Configurations and Challenges for the Green Cables

Historical Tsunamis

Oct 27, ‘12 Haida Gwaii tsunami where historical threat was very low

Sensing Configurations(for discussion) Challenges Next Steps Topics Background Sensing Configurations(for discussion) Challenges Next Steps

Additional Observations are Needed Array Status: Sept’13 Neptune Canada & OOI RSN Cable Critical for US Lack of Observations High threat Costly O&M and High Vandalism High currents Near Field Threat Lack of Observations Gap

Tsunami Forecasting Requirements: Other Technology (Bernard & Meinig 2011)

DART Tsunami Siting Parameters (from Spillane et al 2008) Tsunami travel times from potential tsunami sources Positions relative to tsunami propagation paths to U.S. impact sites Suitability of location for hardware deployment (currents, bathymetry) Avoidance of wave scattering islands, seamounts, and ridges Location relative to political boundaries

Almost No Abyssal-Ocean Measurements

From Science & Society Committee’s draft report Sensing From Science & Society Committee’s draft report Climate Variability: Bottom Pressure, Temperature Tsunami: Bottom Pressure Seismicity/Tsunami: Bottom Pressure, Accelerometer* *Additional interest in hydrophones, but not main part of report

Range, Accuracy, Sampling Rate (draft) Science & Society Measurements Range, Accuracy, Sampling Rate-Interpreted by Meinig Climate Variability   Tsunami Seismology/Tsunami Range Accuracy Rate Bottom Pressure 0-7000m <mm <60min 10-40Hz 10-100Hz Bottom Temperature -5 to 20 C <mC <10min N/A Accelerometer See Seismic ~136dB >24bit 2kHz Time <minute <second <ms

Drift per Year (draft) Science & Society Measurements Drift Uncertainty/year-Interpreted by Meinig Climate Variability Tsunami Seismology/Tsunami   drift/yr Bottom Pressure ? <1m <1cm Bottom Temperature <0.5mC N/A Accelerometer Time <minute ~second <millisecond

Data Rates (draft) Data Rate Digital (kbps) Bottom Pressure 1 y   Digital (kbps) Bottom Pressure 1 y Bottom Temperature 0.05 Accelerometer* 64 n Overhead 4 total <70 kbps *(for Silicon Audio Geolight 32bits/sample x 2kHz rate)-verbal Charlie Thompson

Power (draft) Power (W) Bottom Pressure 0.3 Bottom Temperature 0.2   Bottom Temperature 0.2 Accelerometer 0.075 (25mW/channel) -Accelerometer Digitizer 2? Overhead ? total <5W

Challenges Funding, Funding, Funding Balancing Sensing Scope and Chances of Launch Strategy?

Summary Strong societal & scientific benefits to monitoring the abyssal ocean Cost-effective in-situ observations will be needed for ~decades Next Step: Functional Requirements Document Strategy: Start simple….but ‘start’

Thank you questions?

Extra slides

1.5 Year of Data, numerous EQs and tsunamis recorded Nano-resolution Depth Sensor & Land-based Seismometer Comparison From (Paros, Chadwick Meinig, et al 2012)