An automated method for removing line spectrum elements embedded in co
lored spectra is presented. Since smooth spectrum estimates are desire
d, line spectra tend to smear out over an effective smoothing window.
This introduces a bias in spectrum estimation that seriously degrades
signal-to-noise ratios, spectral deconvolution or any other operation
where spectrum shape is important. Multitaper analysis provides a simp
le algorithmic solution including a method of determining where spectr
al peaks are both significant with high power. The method is completel
y general, and examples include estimation of signal-to-noise ratio at
the 1990 high frequency array, Pinyon Flat, CA. A comparison of noise
spectra line segments and signal spectra line spectra reveals similar
ities associates with instrument noise ans shallow resonances stimulat
ed by incoming seismic signals. Identification and removal of resonanc
es can provide a better means of estimating background noise spectra f
or modeling earthquake source spectra and path effects associated with
attenuation.