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Project IDA (International Deployment of Accelerometers) Project IDA II GSN Calibration Procedures November 16, 2011 Peter Davis Project IDA Scripps Institution.

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Presentation on theme: "Project IDA (International Deployment of Accelerometers) Project IDA II GSN Calibration Procedures November 16, 2011 Peter Davis Project IDA Scripps Institution."— Presentation transcript:

1 Project IDA (International Deployment of Accelerometers) Project IDA II GSN Calibration Procedures November 16, 2011 Peter Davis Project IDA Scripps Institution of Oceanography University of California, San Diego

2 Review timing and waveform quality:

3  sample rate correction

4 Sensor failure:

5  loss of vacuum

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9 Getting the metadata right…

10 Traditional calibration procedures verified the DAS sensitivity and measured shape of system response.

11 DC Calibration Test

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13  Convolve model of sensor response with input  Compare observed output with model  Iterate until fit acceptable

14  Random binary test determines shape of response curve within 1%  Step input to digitizer determines sensitivity to > 0.1%  Manufacturer provides value of sensor generator constant to within 1% What these tests measure:

15  Random binary test determines shape of response curve within 1%  Pitfall – capturing the input signal, test only ‘snapshot’  Step input to digitizer determines sensitivity to > 0.1%  Pitfall – compensate for system load  Manufacturer provides value of sensor generator constant to within 1%  Pitfall – not verified What these tests measure:

16 Sumatra- Andaman earthquake excited many low frequency normal modes Figure from Park et al. (2004), courtesy G. Roult

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18 Portable sensors used to check sensitivity of permanent sensors:

19  Relative performance of GSN as a network  Pitfall – no measure of absolute sensitivity  Pitfall – accuracy limited by mode coupling  Pitfall – need a very large earthquake to excite the mode to observable amplitude What this test measures:

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21  Tides are a continuous, constant signal  Tidal amplitudes can be predicted to 1% accuracy globally  Tides are observed at all times at most GSN stations  Pitfall – must include effects of ocean loading  Pitfall – horizontal sensors effected too strongly by local tilts  Pitfall – tidal periods outside band of seismic interest Why use tides?

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26  Accurate determination of relative response of the common instruments  Accurate determination of relative orientation What comparing co-located broadband sensors measures:

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28 Select data from common time period:

29 Correct for modeled response:

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