circular_sd_error {tectonicr}

Standard Error of Mean Direction of Circular Data

Description

Measure of the chance variation expected from sample to sample in estimates of the mean direction. The approximated standard error of the mean direction is computed by the mean resultant length and the MLE concentration parameter \kappa.

Usage

circular_sd_error(x, w = NULL, axial = TRUE, na.rm = TRUE)

Arguments

x

numeric vector. Values in degrees.

w

(optional) Weights. A vector of positive numbers and of the same length as x.

axial

logical. Whether the data are axial, i.e. pi-periodical (TRUE, the default) or directional, i.e. 2 \pi-periodical (FALSE).

na.rm

logical value indicating whether NA values in x should be stripped before the computation proceeds.

Value

Angle in degrees

References

Davis (1986) Statistics and data analysis in geology. 2nd ed., John Wiley & Sons.

See Also

mean_resultant_length(), circular_mean()

Examples

# Example data from Davis (1986), pp. 316
finland_stria <- c(
  23, 27, 53, 58, 64, 83, 85, 88, 93, 99, 100, 105, 113,
  113, 114, 117, 121, 123, 125, 126, 126, 126, 127, 127, 128, 128, 129, 132,
  132, 132, 134, 135, 137, 144, 145, 145, 146, 153, 155, 155, 155, 157, 163,
  165, 171, 172, 179, 181, 186, 190, 212
)
circular_sd_error(finland_stria, axial = FALSE)

data(san_andreas)
data("nuvel1")
PoR <- subset(nuvel1, nuvel1$plate.rot == "na")
sa.por <- PoR_shmax(san_andreas, PoR, "right")
circular_sd_error(sa.por$azi.PoR, w = 1 / san_andreas$unc)