
Relative Index of Agreement
rd.RdThis function computes the Relative Index of Agreement (d) between sim and obs, with treatment of missing values.
If x is a matrix or a data frame, a vector of the relative index of agreement among the columns is returned.
Usage
rd(sim, obs, ...)
# Default S3 method
rd(sim, obs, na.rm=TRUE, fun=NULL, ...,
epsilon.type=c("none", "Pushpalatha2012", "otherFactor", "otherValue"),
epsilon.value=NA)
# S3 method for class 'data.frame'
rd(sim, obs, na.rm=TRUE, fun=NULL, ...,
epsilon.type=c("none", "Pushpalatha2012", "otherFactor", "otherValue"),
epsilon.value=NA)
# S3 method for class 'matrix'
rd(sim, obs, na.rm=TRUE, fun=NULL, ...,
epsilon.type=c("none", "Pushpalatha2012", "otherFactor", "otherValue"),
epsilon.value=NA)
# S3 method for class 'zoo'
rd(sim, obs, na.rm=TRUE, fun=NULL, ...,
epsilon.type=c("none", "Pushpalatha2012", "otherFactor", "otherValue"),
epsilon.value=NA)Arguments
- sim
numeric, zoo, matrix or data.frame with simulated values
- obs
numeric, zoo, matrix or data.frame with observed values
- na.rm
a logical value indicating whether 'NA' should be stripped before the computation proceeds.
When an 'NA' value is found at the i-th position inobsORsim, the i-th value ofobsANDsimare removed before the computation.- fun
function to be applied to
simandobsin order to obtain transformed values thereof before computing the Nash-Sutcliffe efficiency.The first argument MUST BE a numeric vector with any name (e.g.,
x), and additional arguments are passed using....- ...
arguments passed to
fun, in addition to the mandatory first numeric vector.- epsilon.type
argument used to define a numeric value to be added to both
simandobsbefore applyingFUN.It is was designed to allow the use of logarithm and other similar functions that do not work with zero values.
Valid values of
epsilon.typeare:1) "none":
simandobsare used byFUNwithout the addition of any nummeric value.2) "Pushpalatha2012": one hundredth (1/100) of the mean observed values is added to both
simandobsbefore applyingFUN, as described in Pushpalatha et al. (2012).3) "otherFactor": the numeric value defined in the
epsilon.valueargument is used to multiply the the mean observed values, instead of the one hundredth (1/100) described in Pushpalatha et al. (2012). The resulting value is then added to bothsimandobs, before applyingFUN.4) "otherValue": the numeric value defined in the
epsilon.valueargument is directly added to bothsimandobs, before applyingFUN.- epsilon.value
-) when
epsilon.type="otherValue"it represents the numeric value to be added to bothsimandobsbefore applyingfun.
-) whenepsilon.type="otherFactor"it represents the numeric factor used to multiply the mean of the observed values, instead of the one hundredth (1/100) described in Pushpalatha et al. (2012). The resulting value is then added to bothsimandobsbefore applyingfun.
Details
$$rd = 1 - \frac{ \sum_{i=1}^N { \left( \frac{O_i - S_i}{O_i} \right) ^2} } { \sum_{i=1}^N { \left( \frac{ \left| S_i - \bar{O} \right| + \left| O_i - \bar{O} \right|}{\bar{O}} \right)^2 } } $$
It varies between 0 and 1. A value of 1 indicates a perfect match, and 0 indicates no agreement at all.
Value
Relative index of agreement between sim and obs.
If sim and obs are matrixes, the returned value is a vector, with the relative index of agreement between each column of sim and obs.
References
Krause, P.; Boyle, D.P.; Base, F. (2005). Comparison of different efficiency criteria for hydrological model assessment, Advances in Geosciences, 5, 89-97. doi:10.5194/adgeo-5-89-2005.
Willmott, C.J. (1981). On the validation of models. Physical Geography, 2, 184–194. doi:10.1080/02723646.1981.10642213.
Willmott, C.J. (1984). On the evaluation of model performance in physical geography. Spatial Statistics and Models, G. L. Gaile and C. J. Willmott, eds., 443-460. doi:10.1007/978-94-017-3048-8_23.
Willmott, C.J.; Ackleson, S.G. Davis, R.E.; Feddema, J.J.; Klink, K.M.; Legates, D.R.; O'Donnell, J.; Rowe, C.M. (1985), Statistics for the Evaluation and Comparison of Models, J. Geophys. Res., 90(C5), 8995-9005. doi:10.1029/JC090iC05p08995.
Legates, D.R.; McCabe, G. J. Jr. (1999), Evaluating the Use of "Goodness-of-Fit" Measures in Hydrologic and Hydroclimatic Model Validation, Water Resour. Res., 35(1), 233-241. doi:10.1029/1998WR900018.
Note
obs and sim has to have the same length/dimension
The missing values in obs and sim are removed before the computation proceeds, and only those positions with non-missing values in obs and sim are considered in the computation.
If some of the observed values are equal to zero (at least one of them), this index can not be computed.
Examples
##################
# Example 1: basic ideal case
obs <- 1:10
sim <- 1:10
rd(sim, obs)
#> [1] 1
obs <- 1:10
sim <- 2:11
rd(sim, obs)
#> [1] 0.8625206
##################
# Example 2:
# Loading daily streamflows of the Ega River (Spain), from 1961 to 1970
data(EgaEnEstellaQts)
obs <- EgaEnEstellaQts
# Generating a simulated daily time series, initially equal to the observed series
sim <- obs
# Computing the 'rd' for the "best" (unattainable) case
rd(sim=sim, obs=obs)
#> [1] 1
##################
# Example 3: rd for simulated values equal to observations plus random noise
# on the first half of the observed values.
# This random noise has more relative importance for ow flows than
# for medium and high flows.
# Randomly changing the first 1826 elements of 'sim', by using a normal distribution
# with mean 10 and standard deviation equal to 1 (default of 'rnorm').
sim[1:1826] <- obs[1:1826] + rnorm(1826, mean=10)
ggof(sim, obs)
rd(sim=sim, obs=obs)
#> [1] 0.6257483
##################
# Example 4: rd for simulated values equal to observations plus random noise
# on the first half of the observed values and applying (natural)
# logarithm to 'sim' and 'obs' during computations.
rd(sim=sim, obs=obs, fun=log)
#> [1] -0.4378264
# Verifying the previous value:
lsim <- log(sim)
lobs <- log(obs)
rd(sim=lsim, obs=lobs)
#> [1] -0.4378264
##################
# Example 5: rd for simulated values equal to observations plus random noise
# on the first half of the observed values and applying (natural)
# logarithm to 'sim' and 'obs' and adding the Pushpalatha2012 constant
# during computations
rd(sim=sim, obs=obs, fun=log, epsilon.type="Pushpalatha2012")
#> [1] 0.1939582
# Verifying the previous value, with the epsilon value following Pushpalatha2012
eps <- mean(obs, na.rm=TRUE)/100
lsim <- log(sim+eps)
lobs <- log(obs+eps)
rd(sim=lsim, obs=lobs)
#> [1] 0.1939582
##################
# Example 6: rd for simulated values equal to observations plus random noise
# on the first half of the observed values and applying (natural)
# logarithm to 'sim' and 'obs' and adding a user-defined constant
# during computations
eps <- 0.01
rd(sim=sim, obs=obs, fun=log, epsilon.type="otherValue", epsilon.value=eps)
#> [1] -0.3509093
# Verifying the previous value:
lsim <- log(sim+eps)
lobs <- log(obs+eps)
rd(sim=lsim, obs=lobs)
#> [1] -0.3509093
##################
# Example 7: rd for simulated values equal to observations plus random noise
# on the first half of the observed values and applying (natural)
# logarithm to 'sim' and 'obs' and using a user-defined factor
# to multiply the mean of the observed values to obtain the constant
# to be added to 'sim' and 'obs' during computations
fact <- 1/50
rd(sim=sim, obs=obs, fun=log, epsilon.type="otherFactor", epsilon.value=fact)
#> [1] 0.3871943
# Verifying the previous value:
eps <- fact*mean(obs, na.rm=TRUE)
lsim <- log(sim+eps)
lobs <- log(obs+eps)
rd(sim=lsim, obs=lobs)
#> [1] 0.3871943
##################
# Example 8: rd for simulated values equal to observations plus random noise
# on the first half of the observed values and applying a
# user-defined function to 'sim' and 'obs' during computations
fun1 <- function(x) {sqrt(x+1)}
rd(sim=sim, obs=obs, fun=fun1)
#> [1] 0.8333152
# Verifying the previous value, with the epsilon value following Pushpalatha2012
sim1 <- sqrt(sim+1)
obs1 <- sqrt(obs+1)
rd(sim=sim1, obs=obs1)
#> [1] 0.8333152