Strong Motion Linear Baseline Correction

Remove linear baseline drift fitted on the record tail and report the corrected peak.

Description

Remove linear baseline drift fitted on the record tail and report the corrected peak.

Strong Motion Linear Baseline Correction is a focused tool for the following task. Remove linear baseline drift fitted on the record tail and report the corrected peak. It reports PGA_corr, b₀, b₁ from the values you provide rather than inventing measurements, coefficients, or professional judgment that are not part of the input.

When to use Strong Motion Linear Baseline Correction

Use this seismology calculation to reproduce a stated convention, screen observations, or compare scenarios whose units, coordinate conventions, catalog selection, and model assumptions are known.

a_i (m/s²)
Required list in m/s². Raw acceleration samples.
f_tail
Optional number. Tail fraction used to fit the baseline line.

The cited overview of Seismology supplies background for the terminology and domain context used by this tool.1

How Strong Motion Linear Baseline Correction works

Remove linear baseline drift fitted on the record tail and report the corrected peak. Inputs are interpreted exactly in the displayed units and the calculation returns the following fields without presentation rounding.

PGA_corr (m/s²)
Returned number in m/s². Peak absolute acceleration after detrending.
b₀ (m/s²)
Returned number in m/s². Baseline offset removed at sample zero.
b₁ (m/s²/sample)
Returned number in m/s²/sample. Linear drift removed per sample.

Limitations and assumptions

  • Earth structure, source geometry, path effects, site response, instrument response, catalog completeness, uncertainty, and the fitted range can dominate the accuracy of simplified seismic calculations.
  • f_tail must be at least 0.1.
  • f_tail must be no greater than 0.5.
  • Use finite inputs in the displayed units, preserve source measurements and assumptions, and independently verify consequential decisions.

Alternative or Complementary approaches

For analysis or hazard decisions, retain uncertainty and provenance and compare the result with waveform processing, calibrated regional models, and guidance from qualified seismologists or the responsible agency.

References

  1. Seismology — Wikipedia contributors

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