Description Usage Arguments Details Value Author(s) References See Also Examples
Fits wavelet linear models. Also the generator function of the wlm
class, which
inherits from the list
class.
1 2 3 4 5 6 7 8 9 10 11 |
dat |
A list of matrices representing the data (or in the case of one location, a list of vectors). All the same dimensions (respectively, lengths) |
times |
The times at which measurements were made, spacing 1 |
resp |
Index in dat for the response variable of the model |
pred |
Vector of indices in dat for the predictor variables of the model; must differ from |
norm |
The normalization of wavelet transforms to use. One of "none", "powall", "powind". See details. |
scale.min |
The smallest scale of fluctuation that will be examined. At least 2. |
scale.max.input |
The largest scale of fluctuation that will be examined. Note that if this is set too high relative to the length of the timeseries it will be truncated. |
sigma |
The ratio of each time scale examined relative to the next timescale. Greater than 1. |
f0 |
The ratio of the period of fluctuation to the width of the envelope |
Normalization is as specified in the documentation for coh
, HOWEVER, only
the "powall
" option is currently implemented, other choices throw an error. Details
are specified in appendices S7 and S9 of Sheppard et al, 2018. The output modval
is v in appendix S7, and coefs
are the betas in equation 12 in that appendix.
wlm
returns an object of class wlm
. Slots are:
dat |
The input data list, but reordered and subsetted so the response is first and only used predictors are included |
times |
The times associated with the data |
norm |
The input |
wtopt |
The inputted wavelet transform options scale.min, scale.max.input, sigma, f0 in a list |
wts |
List of transforms, normalized as specified in |
timescales |
The timescales associated with the wavelet transforms of the data |
coefs |
A list (data frame, actually) of complex vectors, each of length the same
as |
modval |
The model values. |
coher |
Appropriately normalized version of coherence of the model and response transforms. See details. |
Thomas Anderson, anderstl@gmail.com, Jon Walter, jaw3es@virginia.edu; Lawrence Sheppard, lwsheppard@ku.edu; Daniel Reuman, reuman@ku.edu
Sheppard, LW et al. (2019) Synchrony is more than its top-down and climatic parts: interacting Moran effects on phytoplankton in British seas. Plos Computational Biology 15, e1006744. doi: 10.1371/journal.pcbi.1006744
wlm_methods
, wlmtest
, syncexpl
, predsync
,
browseVignettes("wsyn")
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