View source: R/inla.climate.tcr.R
| inla.climate.tcr | R Documentation | 
Computes Bayesian inference about the transient climate response by Monte Carlo simulations generated by sampling from the posterior marginal distributions obtained by INLA.
inla.climate.tcr(result, Qco2, nsamples = 100000, seed = 1234, print.progress = FALSE,model = "fgn")
result | 
 An   | 
Qco2 | 
 The slope of the forcing when assuming a CO2 doubling in the future.  | 
nsamples | 
 The number of Monte Carlo simulations used in obtaining transient climate response inference.  | 
seed | 
 Seed used for random number generator.  | 
print.progress | 
 Prints progression if   | 
model | 
 The model used to describe stochastic forcing. For long memory responses the fractional Gaussian noise (  | 
Returns a list of class inla.climate.tcr which contains the following objects:
 | 
 The mean value of the transient climate response simulations.  | 
 | 
 The standard deviation of the transient climate response simulations.  | 
 | 
 The 2.5% quantile value of the transient climate response simulations.  | 
 | 
 The 50% quantile of the transient climate response simulations.  | 
 | 
 The 97.5% quantile of the transient climate response simulations.  | 
 | 
 List containing the Monte Carlo simulations of the TCR and all hyperparameters.  | 
 | 
 The time spent doing the Monte Carlo simulations.  | 
Eirik Myrvoll-Nilsen eirik.myrvoll-nilsen@uit.no
Fredriksen, H.B., Rypdal, M. (2017) Long-Range Persistence in Global Surface Temperatures Explained by Linear Multibox Energy Balance Models. Journal of Climate 30 (18), 7157–7168.
inla.climate, inla.climate.mu
if(require("INLA",quietly=TRUE)){
  data(GISS_E2_R)
  result.climate <- inla.climate(data=GISS_E2_R$Temperature,forcing=GISS_E2_R$Forcing)
  result.tcr <- inla.climate.tcr(result.climate$inla.result,Qco2=3.8)
}
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