Project IDA (International Deployment of Accelerometers) Project IDA II GSN Calibration Procedures...

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Transcript of Project IDA (International Deployment of Accelerometers) Project IDA II GSN Calibration Procedures...

Project IDA (International Deployment of Accelerometers)Project IDA

II GSN CalibrationProcedures

November 16, 2011

Peter DavisProject IDA

Scripps Institution of OceanographyUniversity of California, San Diego

Review timing and waveform quality:

sample rate correction

Sensor failure:

loss of vacuum

Getting the metadata right…

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

DC Calibration Test

Convolve model of sensor response with input

Compare observed output with model

Iterate until fit acceptable

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:

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:

Sumatra-Andaman earthquake excited many low frequency normal modes

Figure from Park et al. (2004), courtesy G. Roult

Portable sensors used to check sensitivity of permanent sensors:

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:

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?

Accurate determination of relative response of the common instruments

Accurate determination of relative orientation

What comparing co-located broadband sensors measures:

Select data from common time period:

Correct for modeled response: