Plot proxy signal-to-noise ratios of several datasets as a function of timescale (e.g., as in the firn core analysis of Münch and Laepple, 2018, Fig. 3).
Arguments
- spec
a (named) list of signal-to-noise ratio data sets: each dataset itself should be list containing at least the spectral object (
?spec.object
)snr
providing signal-to-noise ratios as a function of frequency. For Figure 3 in Münch and Laepple (2018) setspec
to the output fromPublicationSNR
.- f.cut
Shall the spectra be cut at the cutoff frequency constrained by the diffusion correction strength? Defaults to
FALSE
.- names
an optional character vector of names of the proxy data sets. If
NULL
, the names ofspec
are used or, if not present, default names.- col
a numeric or character vector of colors to use for the plotting with length recycled to match
length(spec)
.- xlim
the x limits (x1, x2) of the plot.
- ylim
the y limits (y1, y2) of the plot.
- xlab
x axis label.
- ylab
y axis label.
- xtm
x axis tick mark positions; if
NULL
computed byaxis
.- ytm
y axis tick mark positions; default setting (
NULL
) usesc(0.05, 0.1, 0.5, 1, 5)
.- xtl
x axis tick mark labels; if
NULL
determined automatically fromxtm
, else it must be a vector of labels of the same length asxtm
.- ytl
equivalent to
xtl
for the y axis tick mark labels.
References
Münch, T. and Laepple, T.: What climate signal is contained in decadal- to centennial-scale isotope variations from Antarctic ice cores? Clim. Past, 14, 2053–2070, https://doi.org/10.5194/cp-14-2053-2018, 2018.
See also
spec.object
for the definition of a proxysnr
spectral object.