| coolingFromNuclearWar | R Documentation |
Global cooling from a nuclear war
Description
Average surface temperature changes world wide and in the Northern Hemisphere 3 and 10 years after the injections of 5, 50 and 150 Tg (teragrams = millions of metric tons) of smoke into the upper troposphere, per Robock, Oman, and Stenchikov (2007).
These numbers are relative to the average for 1925-1975, which explains why the numbers are positive with smoke = 0.
Usage
data(coolingFromNuclearWar)
Format
A dataframe containing :
- smoke
teragrams = millions of metric tons
- dC3g, dC10g, dC3n, dC10n
-
average change in surface temperature 3 and 10 years after injection of
smokeinto the upper troposphere globally (g) or in the Northern Hemisphere (n) in degrees Celsius.
Source
Alan Robock, Luke Oman, and Georgiy L. Stenchikov (2007) Nuclear winter revisited with a modern climate model and current nuclear arsenals: Still catastrophic consequences, Journal of Geophysical Research, 112
Examples
data(coolingFromNuclearWar)
matplot(coolingFromNuclearWar[, 'smoke'],
coolingFromNuclearWar[, 2:5], type='l')
(linFit <- lm(cbind(dC3g, dC10g, dC3n, dC10n)~smoke,
coolingFromNuclearWar))
# total change
dC <- as.matrix(coolingFromNuclearWar[, 2:5] -
rep(unlist(coolingFromNuclearWar[1, -1]), e=4))
(linFit0 <- lm(dC~smoke, coolingFromNuclearWar))
summary(linFit0)