| bomsoi {DAAG} | R Documentation |
The Southern Oscillation Index (SOI) is the difference in barometric pressure at sea level between Tahiti and Darwin. Annual SOI and Australian rainfall data, for the years 1900-2001, are given. Australia's annual mean rainfall is an area-weighted average of the total annual precipitation at approximately 370 rainfall stations around the country.
bomsoi
This data frame contains the following columns:
Australian Bureau of Meteorology web pages:
http://www.bom.gov.au/climate/change/rain02.txt and http://www.bom.gov.au/climate/current/soihtm1.shtml
Nicholls, N., Lavery, B., Frederiksen, C. and Drosdowsky, W. 1996. Recent apparent changes in relationships between the El Nino – southern oscillation and Australian rainfall and temperature. Geophysical Research Letters 23: 3357-3360.
plot(ts(bomsoi[, 15:14], start=1900),
panel=function(y,...)panel.smooth(1900:2001, y,...))
# Check for skewness by comparing the normal probability plots for
# different a, e.g.
par(mfrow = c(2,3))
for (a in c(50, 100, 150, 200, 250, 300))
qqnorm(log(bomsoi[, "avrain"] - a))
# a = 250 leads to a nearly linear plot
par(mfrow = c(1,1))
plot(bomsoi$SOI, log(bomsoi$avrain - 250), xlab = "SOI",
ylab = "log(avrain = 250)")
lines(lowess(bomsoi$SOI)$y, lowess(log(bomsoi$avrain - 250))$y, lwd=2)
# NB: separate lowess fits against time
lines(lowess(bomsoi$SOI, log(bomsoi$avrain - 250)))
detsoi <- data.frame(
detSOI = bomsoi[, "SOI"] - lowess(bomsoi[, "SOI"])$y,
detrain = log(bomsoi$avrain - 250) - lowess(log(bomsoi$avrain - 250))$y)
row.names(detsoi) <- paste(1900:2001)
par(mfrow = c(1,2))
plot(log(avrain-250) ~ SOI, data = bomsoi, ylab =
"log(Average rainfall - 250)")
lines(lowess(bomsoi$SOI, log(bomsoi$avrain-250)))
plot(detrain ~ detSOI, data = detsoi,
xlab="Detrended SOI", ylab = "Detrended log(Rainfall-250)")
lines(lowess(detsoi$detrain ~ detsoi$detSOI))
par(mfrow = c(1,1))