diff --git a/DESCRIPTION b/DESCRIPTION
index 49092a9318e430a89998bab146e616b8cdf1913f..0d2dcb6af8efa31b4c4491cfac60e3ae605ac07b 100644
--- a/DESCRIPTION
+++ b/DESCRIPTION
@@ -1,7 +1,7 @@
Package: airGR
Type: Package
Title: Suite of GR Hydrological Models for Precipitation-Runoff Modelling
-Version: 1.2.12.15
+Version: 1.2.12.16
Date: 2019-04-01
Authors@R: c(
person("Laurent", "Coron", role = c("aut", "trl"), comment = c(ORCID = "0000-0002-1503-6204")),
diff --git a/NEWS.rmd b/NEWS.rmd
index 3d117ae38ab6b93d8c62ad228ac0895ac44ca92c..d5e8270f6edbeda9d63b295cc92c0d52fa6dc49f 100644
--- a/NEWS.rmd
+++ b/NEWS.rmd
@@ -13,7 +13,7 @@ output:
-### 1.2.12.15 Release Notes (2019-04-01)
+### 1.2.12.16 Release Notes (2019-04-01)
diff --git a/man/CreateCalibOptions.Rd b/man/CreateCalibOptions.Rd
index be9b1c23bce1c03b4cbc23b8a20e13c69b553123..c4a446d6a984d5662a28b4f03cef9ebbc4e32e55 100644
--- a/man/CreateCalibOptions.Rd
+++ b/man/CreateCalibOptions.Rd
@@ -76,13 +76,12 @@ Creation of the \emph{CalibOptions} object required by the \code{Calibration*} f
\details{
Users wanting to use \code{FUN_MOD}, \code{FUN_CALIB} or \code{FUN_TRANSFO} functions that are not included in
-the package must create their own \code{CalibOptions} object accordingly.
+the package must create their own \code{CalibOptions} object accordingly. \cr
-##### CemaNeige version #####
-
-If \code{IsHyst = FALSE}, the original CemaNeige version from Valéry et al. (2014) is used. \cr
-If \code{IsHyst = TRUE}, the CemaNeige version from Riboust et al. (2019) is used. Compared to the original version, this version of CemaNeige needs two more parameters and it includes a representation of the hysteretic relationship between the Snow Cover Area (SCA) and the Snow Water Equivalent (SWE) in the catchment. The hysteresis included in airGR is the Modified Linear hysteresis (LH*); it is represented on panel b) of Fig. 3 in Riboust et al. (2019). Riboust et al. (2019) advise to use the LH* version of CemaNeige with parameters calibrated using an objective function combining 75 \% of KGE calculated on discharge simulated from a rainfall-runoff model compared to observed discharge and 5 \% of KGE calculated on SCA on 5 CemaNeige elevation bands compared to satellite (e.g. MODIS) SCA (see Eq. (18), Table 3 and Fig. 6). Riboust et al. (2019)'s tests were realized with GR4J as the chosen rainfall-runoff model. \cr \cr
+## ---- CemaNeige version
+If \code{IsHyst = FALSE}, the original CemaNeige version from Valéry et al. (2014) is used. \cr
+If \code{IsHyst = TRUE}, the CemaNeige version from Riboust et al. (2019) is used. Compared to the original version, this version of CemaNeige needs two more parameters and it includes a representation of the hysteretic relationship between the Snow Cover Area (SCA) and the Snow Water Equivalent (SWE) in the catchment. The hysteresis included in airGR is the Modified Linear hysteresis (LH*); it is represented on panel b) of Fig. 3 in Riboust et al. (2019). Riboust et al. (2019) advise to use the LH* version of CemaNeige with parameters calibrated using an objective function combining 75 \% of KGE calculated on discharge simulated from a rainfall-runoff model compared to observed discharge and 5 \% of KGE calculated on SCA on 5 CemaNeige elevation bands compared to satellite (e.g. MODIS) SCA (see Eq. (18), Table 3 and Fig. 6). Riboust et al. (2019)'s tests were realized with GR4J as the chosen rainfall-runoff model. \cr
}
@@ -134,16 +133,14 @@ OutputsCrit <- ErrorCrit_NSE(InputsCrit = InputsCrit, OutputsModel = OutputsMode
InputsCrit <- CreateInputsCrit(FUN_CRIT = ErrorCrit_KGE, InputsModel = InputsModel,
RunOptions = RunOptions, obs = BasinObs$Qmm[Ind_Run], varObs = "Q")
OutputsCrit <- ErrorCrit_KGE(InputsCrit = InputsCrit, OutputsModel = OutputsModel)
-
}
\author{
-Laurent Coron
+Laurent Coron, Olivier Delaigue, Guillaume Thirel
}
\seealso{
\code{\link{Calibration}}, \code{\link{RunModel}}
}
-
diff --git a/man/CreateRunOptions.Rd b/man/CreateRunOptions.Rd
index ad565f8f97cc3228fdf170ec95a972f9b3603e1e..cce6f59d226c4d4ad7d09123027da783029601cc 100644
--- a/man/CreateRunOptions.Rd
+++ b/man/CreateRunOptions.Rd
@@ -73,7 +73,7 @@ Creation of the RunOptions object required to the \code{RunModel*} functions.
Users wanting to use \code{FUN_MOD} functions that are not included in
the package must create their own \code{RunOptions} object accordingly.
-##### Initialisation options #####
+## ---- Initialisation options
The model initialisation options can either be set to a default configuration or be defined by the user.
@@ -108,11 +108,10 @@ However, it is also possible to perform a long-term initialisation if other indi
}
}
-##### CemaNeige version #####
+## ---- CemaNeige version
If \code{IsHyst = FALSE}, the original CemaNeige version from Valéry et al. (2014) is used. \cr
-If \code{IsHyst = TRUE}, the CemaNeige version from Riboust et al. (2019) is used. Compared to the original version, this version of CemaNeige needs two more parameters and it includes a representation of the hysteretic relationship between the Snow Cover Area (SCA) and the Snow Water Equivalent (SWE) in the catchment. The hysteresis included in airGR is the Modified Linear hysteresis (LH*); it is represented on panel b) of Fig. 3 in Riboust et al. (2019). Riboust et al. (2019) advise to use the LH* version of CemaNeige with parameters calibrated using an objective function combining 75 \% of KGE calculated on discharge simulated from a rainfall-runoff model compared to observed discharge and 5 \% of KGE calculated on SCA on 5 CemaNeige elevation bands compared to satellite (e.g. MODIS) SCA (see Eq. (18), Table 3 and Fig. 6). Riboust et al. (2019)'s tests were realized with GR4J as the chosen rainfall-runoff model. \cr \cr
-
+If \code{IsHyst = TRUE}, the CemaNeige version from Riboust et al. (2019) is used. Compared to the original version, this version of CemaNeige needs two more parameters and it includes a representation of the hysteretic relationship between the Snow Cover Area (SCA) and the Snow Water Equivalent (SWE) in the catchment. The hysteresis included in airGR is the Modified Linear hysteresis (LH*); it is represented on panel b) of Fig. 3 in Riboust et al. (2019). Riboust et al. (2019) advise to use the LH* version of CemaNeige with parameters calibrated using an objective function combining 75 \% of KGE calculated on discharge simulated from a rainfall-runoff model compared to observed discharge and 5 \% of KGE calculated on SCA on 5 CemaNeige elevation bands compared to satellite (e.g. MODIS) SCA (see Eq. (18), Table 3 and Fig. 6). Riboust et al. (2019)'s tests were realized with GR4J as the chosen rainfall-runoff model. \cr
}
@@ -157,6 +156,6 @@ Laurent Coron, Olivier Delaigue, Guillaume Thirel
\seealso{
-\code{\link{RunModel}}, \code{\link{CreateInputsModel}}, \code{\link{CreateInputsCrit}}, \code{\link{CreateCalibOptions}}, \code{\link{CreateIniStates}}
+\code{\link{RunModel}}, \code{\link{CreateInputsModel}}, \code{\link{CreateInputsCrit}},
+\code{\link{CreateCalibOptions}}, \code{\link{CreateIniStates}}
}
-
diff --git a/man/RunModel_CemaNeigeGR5J.Rd b/man/RunModel_CemaNeigeGR5J.Rd
index 5d4beb0439f96eb522ef0e2b2769cea737436437..7e8bd17a3623aa9985b52ef64f6865dcb3d1b5b8 100644
--- a/man/RunModel_CemaNeigeGR5J.Rd
+++ b/man/RunModel_CemaNeigeGR5J.Rd
@@ -35,41 +35,41 @@ CemaNeige X4 \tab (optional) percentage (between 0 and 1) of annual snowfall def
\value{
[list] list containing the function outputs organised as follows:
- \tabular{ll}{
- \emph{$DatesR } \tab [POSIXlt] series of dates \cr
- \emph{$PotEvap } \tab [numeric] series of input potential evapotranspiration [mm/d] \cr
- \emph{$Precip } \tab [numeric] series of input total precipitation [mm/d] \cr
- \emph{$Prod } \tab [numeric] series of production store level [mm] \cr
- \emph{$Pn } \tab [numeric] series of net rainfall [mm/d] \cr
- \emph{$Ps } \tab [numeric] series of the part of Pn filling the production store [mm/d] \cr
- \emph{$AE } \tab [numeric] series of actual evapotranspiration [mm/d] \cr
- \emph{$Perc } \tab [numeric] series of percolation (PERC) [mm/d] \cr
- \emph{$PR } \tab [numeric] series of PR=Pn-Ps+Perc [mm/d] \cr
- \emph{$Q9 } \tab [numeric] series of UH1 outflow (Q9) [mm/d] \cr
- \emph{$Q1 } \tab [numeric] series of UH2 outflow (Q1) [mm/d] \cr
- \emph{$Rout } \tab [numeric] series of routing store level [mm] \cr
- \emph{$Exch } \tab [numeric] series of potential semi-exchange between catchments [mm/d] \cr
- \emph{$AExch1 } \tab [numeric] series of actual exchange between catchments for branch 1 [mm/d] \cr
- \emph{$AExch2 } \tab [numeric] series of actual exchange between catchments for branch 2 [mm/d] \cr
- \emph{$AExch } \tab [numeric] series of actual exchange between catchments (1+2) [mm/d] \cr
- \emph{$QR } \tab [numeric] series of routing store outflow (QR) [mm/d] \cr
- \emph{$QD } \tab [numeric] series of direct flow from UH2 after exchange (QD) [mm/d] \cr
- \emph{$Qsim } \tab [numeric] series of simulated discharge [mm/d] \cr
- \emph{$CemaNeigeLayers} \tab [list] list of CemaNeige outputs (1 list per layer) \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Pliq } \tab [numeric] series of liquid precip. [mm/d] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Psol } \tab [numeric] series of solid precip. [mm/d] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$SnowPack } \tab [numeric] series of snow pack [mm] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$ThermalState } \tab [numeric] series of snow pack thermal state [°C] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Gratio } \tab [numeric] series of Gratio [0-1] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$PotMelt } \tab [numeric] series of potential snow melt [mm/d] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Melt } \tab [numeric] series of actual snow melt [mm/d] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$PliqAndMelt } \tab [numeric] series of liquid precip. + actual snow melt [mm/d] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Temp } \tab [numeric] series of air temperature [°C] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Gthreshold } \tab [numeric] series of melt threshold [mm] \cr
- \emph{$CemaNeigeLayers[[iLayer]]$Glocalmax } \tab [numeric] series of local melt threshold for hysteresis [mm] \cr
- \emph{$StateEnd} \tab [numeric] states at the end of the run: \cr\tab store & unit hydrographs levels [mm], CemaNeige states [mm & °C], \cr\tab see \code{\link{CreateIniStates}} for more details \cr
- }
- (refer to the provided references or to the package source code for further details on these model outputs)
+ \tabular{ll}{
+ \emph{$DatesR } \tab [POSIXlt] series of dates \cr
+ \emph{$PotEvap } \tab [numeric] series of input potential evapotranspiration [mm/d] \cr
+ \emph{$Precip } \tab [numeric] series of input total precipitation [mm/d] \cr
+ \emph{$Prod } \tab [numeric] series of production store level [mm] \cr
+ \emph{$Pn } \tab [numeric] series of net rainfall [mm/d] \cr
+ \emph{$Ps } \tab [numeric] series of the part of Pn filling the production store [mm/d] \cr
+ \emph{$AE } \tab [numeric] series of actual evapotranspiration [mm/d] \cr
+ \emph{$Perc } \tab [numeric] series of percolation (PERC) [mm/d] \cr
+ \emph{$PR } \tab [numeric] series of PR=Pn-Ps+Perc [mm/d] \cr
+ \emph{$Q9 } \tab [numeric] series of UH1 outflow (Q9) [mm/d] \cr
+ \emph{$Q1 } \tab [numeric] series of UH2 outflow (Q1) [mm/d] \cr
+ \emph{$Rout } \tab [numeric] series of routing store level [mm] \cr
+ \emph{$Exch } \tab [numeric] series of potential semi-exchange between catchments [mm/d] \cr
+ \emph{$AExch1 } \tab [numeric] series of actual exchange between catchments for branch 1 [mm/d] \cr
+ \emph{$AExch2 } \tab [numeric] series of actual exchange between catchments for branch 2 [mm/d] \cr
+ \emph{$AExch } \tab [numeric] series of actual exchange between catchments (1+2) [mm/d] \cr
+ \emph{$QR } \tab [numeric] series of routing store outflow (QR) [mm/d] \cr
+ \emph{$QD } \tab [numeric] series of direct flow from UH2 after exchange (QD) [mm/d] \cr
+ \emph{$Qsim } \tab [numeric] series of simulated discharge [mm/d] \cr
+ \emph{$CemaNeigeLayers} \tab [list] list of CemaNeige outputs (1 list per layer) \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Pliq } \tab [numeric] series of liquid precip. [mm/d] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Psol } \tab [numeric] series of solid precip. [mm/d] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$SnowPack } \tab [numeric] series of snow pack [mm] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$ThermalState } \tab [numeric] series of snow pack thermal state [°C] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Gratio } \tab [numeric] series of Gratio [0-1] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$PotMelt } \tab [numeric] series of potential snow melt [mm/d] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Melt } \tab [numeric] series of actual snow melt [mm/d] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$PliqAndMelt } \tab [numeric] series of liquid precip. + actual snow melt [mm/d] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Temp } \tab [numeric] series of air temperature [°C] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Gthreshold } \tab [numeric] series of melt threshold [mm] \cr
+ \emph{$CemaNeigeLayers[[iLayer]]$Glocalmax } \tab [numeric] series of local melt threshold for hysteresis [mm] \cr
+ \emph{$StateEnd} \tab [numeric] states at the end of the run: \cr\tab store & unit hydrographs levels [mm], CemaNeige states [mm & °C], \cr\tab see \code{\link{CreateIniStates}} for more details \cr
+ }
+ (refer to the provided references or to the package source code for further details on these model outputs)
}
diff --git a/man/SeriesAggreg.Rd b/man/SeriesAggreg.Rd
index f85c512d119273c86b380b13ab9f7b60fb76ccf8..3eb8dde62a9b86f1c0b90acf700a137b195e24e7 100644
--- a/man/SeriesAggreg.Rd
+++ b/man/SeriesAggreg.Rd
@@ -37,9 +37,9 @@ SeriesAggreg(TabSeries, TimeFormat, NewTimeFormat, ConvertFun,
\description{
Conversion of time series to another time step (aggregation only). \cr
Warning : on the aggregated outputs, the dates correspond to the beginning of the time step \cr
-(e.g. for daily time-series 01/03/2005 00:00 = value for period 01/03/2005 00:00 - 01/03/2005 23:59) \cr
-(e.g. for monthly time-series 01/03/2005 00:00 = value for period 01/03/2005 00:00 - 31/03/2005 23:59) \cr
-(e.g. for yearly time-series 01/03/2005 00:00 = value for period 01/03/2005 00:00 - 28/02/2006 23:59)
+(e.g. for daily time-series 2005-03-01 00:00 = value for period 2005-03-01 00:00 - 2005-03-01 23:59) \cr
+(e.g. for monthly time-series 2005-03-01 00:00 = value for period 2005-03-01 00:00 - 2005-03-31 23:59) \cr
+(e.g. for yearly time-series 2005-03-01 00:00 = value for period 2005-03-01 00:00 - 2006-02-28 23:59)
}
diff --git a/man/TransfoParam.Rd b/man/TransfoParam.Rd
index e3c70c7cf061b5c09b13e84ad7a3148d0ce34bcf..df754ac7cadf1ffac49bac9f8bd414fa60dfa8f5 100644
--- a/man/TransfoParam.Rd
+++ b/man/TransfoParam.Rd
@@ -52,8 +52,7 @@ Function which transforms model parameters using the provided function (from raw
\examples{
library(airGR)
-
-#### generic function
+## ---- generic function
## transformation Raw -> Transformed for the GR4J model
Xraw <- matrix(c(+221.41, -3.63, +30.00, +1.37,
@@ -70,7 +69,7 @@ Xtran <- matrix(c(+3.60, -2.00, +3.40, -9.10,
Xraw <- TransfoParam(ParamIn = Xtran, Direction = "TR", FUN_TRANSFO = TransfoParam_GR4J)
-#### specific function
+## ---- specific function
## transformation Raw -> Transformed for the GR4J model
Xraw <- matrix(c(+221.41, -3.63, +30.00, +1.37,
@@ -91,6 +90,3 @@ Xraw <- TransfoParam_GR4J(ParamIn = Xtran, Direction = "TR")
\author{
Laurent Coron, Olivier Delaigue
}
-
-
-
diff --git a/man/airGR.Rd b/man/airGR.Rd
index 9a5007b32d5e96f160edd92c80ec31b343c59ed2..9266747c028e71466efc8d159cc99b9e387e5a23 100644
--- a/man/airGR.Rd
+++ b/man/airGR.Rd
@@ -4,10 +4,10 @@
\encoding{UTF-8}
\title{Suite of GR Hydrological Models for Precipitation-Runoff Modelling}
\description{
-This package brings into R the hydrological modelling tools used at IRSTEA-Antony (HYCAR Research Unit, France), including rainfall-runoff models (\strong{GR4H}, \strong{GR4J}, \strong{GR5J}, \strong{GR6J}, \strong{GR2M}, \strong{GR1A}) and a snow accumulation and melt model (\strong{CemaNeige}). Each model core is coded in FORTRAN to ensure low computational time. The other package functions (i.e. mainly the calibration algorithm and the computation of the efficiency criteria) are coded in R. \cr
+This package brings into R the hydrological modelling tools used at IRSTEA-Antony (HYCAR Research Unit, France), including rainfall-runoff models (\strong{GR4H}, \strong{GR4J}, \strong{GR5J}, \strong{GR6J}, \strong{GR2M}, \strong{GR1A}) and a snow accumulation and melt model (\strong{CemaNeige}). Each model core is coded in FORTRAN to ensure low computational time. The other package functions (i.e. mainly the calibration algorithm and the computation of the efficiency criteria) are coded in R. \cr\cr
-##### Functions and objects #####
+## ---- Functions and objects
The airGR package has been designed to fulfil two major requirements: facilitate the use by non-expert users and allow flexibility regarding the addition of external criteria, models or calibration algorithms. The names of the functions and their arguments were chosen to this end.
@@ -16,37 +16,38 @@ The package is mostly based on three families of functions: \cr
- the functions belonging to the \code{\link{ErrorCrit}} family require two arguments: \emph{InputsCrit} and \emph{OutputsModel}; please refer to help pages \code{\link{CreateInputsCrit}} and \code{\link{RunModel}} for further details and examples; \cr
- the functions belonging to the \code{\link{Calibration}} family require four arguments: \emph{InputsModel}, \emph{RunOptions}, \emph{InputsCrit} and \emph{CalibOptions}; please refer to help pages \code{\link{CreateInputsModel}}, \code{\link{CreateRunOptions}}, \code{\link{CreateInputsCrit}} and \code{\link{CreateCalibOptions}} for further details and examples.
-In order to limit the risk of mis-use and increase the flexibility of these main functions, we imposed the structure of their arguments and defined their class. Most users will not need to worry about these imposed structures since functions are provided to prepare these arguments for them: \code{\link{CreateInputsModel}}, \code{\link{CreateRunOptions}}, \code{\link{CreateInputsCrit}}, \code{\link{CreateCalibOptions}}. However, advanced users wishing to supplement the package with their own models will need to comply with these imposed structures and refer to the package source codes to get all the specification requirements. \cr
+In order to limit the risk of mis-use and increase the flexibility of these main functions, we imposed the structure of their arguments and defined their class. Most users will not need to worry about these imposed structures since functions are provided to prepare these arguments for them: \code{\link{CreateInputsModel}}, \code{\link{CreateRunOptions}}, \code{\link{CreateInputsCrit}}, \code{\link{CreateCalibOptions}}. However, advanced users wishing to supplement the package with their own models will need to comply with these imposed structures and refer to the package source codes to get all the specification requirements. \cr\cr
-##### Models #####
+## ---- Models
Six hydrological models and one snow melt and accumulation model are implemented in airGR. The snow model can also be used alone or with the daily hydrological models, and each hydrological model can either be used alone or together with the snow model. \cr
These models can be called within airGR using the following functions: \cr
-- \code{\link{RunModel_GR4H}}: four-parameter hourly lumped hydrological model (Mathevet, 2005) \cr
-- \code{\link{RunModel_GR4J}}: four-parameter daily lumped hydrological model (Perrin \emph{et al.}, 2003) \cr
-- \code{\link{RunModel_GR5J}}: five-parameter daily lumped hydrological model (Le Moine, 2008) \cr
-- \code{\link{RunModel_GR6J}}: six-parameter daily lumped hydrological model (Pushpalatha \emph{et al.}, 2011) \cr
-- \code{\link{RunModel_GR2M}}: two-parameter monthly lumped hydrological model (Mouelhi, 2003 ; Mouelhi \emph{et al.}, 2006a) \cr
-- \code{\link{RunModel_GR1A}}: one-parameter yearly lumped hydrological model (Mouelhi, 2003 ; Mouelhi \emph{et al.}, 2006b) \cr
-- \code{\link{RunModel_CemaNeige}}: two-parameter degree-day snow melt and accumulation daily model (Valéry \emph{et al.}, 2014) \cr
-- \code{\link{RunModel_CemaNeigeGR4J}}: combined use of GR4J and CemaNeige \cr
-- \code{\link{RunModel_CemaNeigeGR5J}}: combined use of GR5J and CemaNeige \cr
-- \code{\link{RunModel_CemaNeigeGR6J}}: combined use of GR6J and CemaNeige \cr
+ - \code{\link{RunModel_GR4H}}: four-parameter hourly lumped hydrological model (Mathevet, 2005) \cr
+ - \code{\link{RunModel_GR4J}}: four-parameter daily lumped hydrological model (Perrin \emph{et al.}, 2003) \cr
+ - \code{\link{RunModel_GR5J}}: five-parameter daily lumped hydrological model (Le Moine, 2008) \cr
+ - \code{\link{RunModel_GR6J}}: six-parameter daily lumped hydrological model (Pushpalatha \emph{et al.}, 2011) \cr
+ - \code{\link{RunModel_GR2M}}: two-parameter monthly lumped hydrological model (Mouelhi, 2003 ; Mouelhi \emph{et al.}, 2006a) \cr
+ - \code{\link{RunModel_GR1A}}: one-parameter yearly lumped hydrological model (Mouelhi, 2003 ; Mouelhi \emph{et al.}, 2006b) \cr
+ - \code{\link{RunModel_CemaNeige}}: two-parameter degree-day snow melt and accumulation daily model (Valéry \emph{et al.}, 2014) \cr
+ - \code{\link{RunModel_CemaNeigeGR4J}}: combined use of GR4J and CemaNeige \cr
+ - \code{\link{RunModel_CemaNeigeGR5J}}: combined use of GR5J and CemaNeige \cr
+ - \code{\link{RunModel_CemaNeigeGR6J}}: combined use of GR6J and CemaNeige \cr\cr
-##### How to get started #####
+## ---- How to get started
To learn how to use the functions from the airGR package, it is recommended to follow the five steps described below: \cr
-1. refer to the help for \code{\link{RunModel_GR4J}} then run the provided example to assess how to make a simulation; \cr
-2. refer to the help for \code{\link{CreateInputsModel}} to understand how the inputs of a model are prepared/organised; \cr
-3. refer to the help for \code{\link{CreateRunOptions}} to understand how the run options of a model are parametrised/organised; \cr
-4. refer to the help for \code{\link{ErrorCrit_NSE}} and \code{\link{CreateInputsCrit}} to understand how the computation of an error criterion is prepared/made; \cr
-5. refer to the help for \code{\link{Calibration_Michel}}, run the provided example and then refer to the help for \code{\link{CreateCalibOptions}} to understand how a model calibration is prepared/made. \cr
+ 1. refer to the help for \code{\link{RunModel_GR4J}} then run the provided example to assess how to make a simulation; \cr
+ 2. refer to the help for \code{\link{CreateInputsModel}} to understand how the inputs of a model are prepared/organised; \cr
+ 3. refer to the help for \code{\link{CreateRunOptions}} to understand how the run options of a model are parametrised/organised; \cr
+ 4. refer to the help for \code{\link{ErrorCrit_NSE}} and \code{\link{CreateInputsCrit}} to understand how the computation of an error criterion is prepared/made; \cr
+ 5. refer to the help for \code{\link{Calibration_Michel}}, run the provided example and then refer to the help for \code{\link{CreateCalibOptions}} to understand how a model calibration is prepared/made. \cr
-For more information and to get started with the package, you can refer to the vignette (\code{vignette("airGR")}) and go on the \href{https://webgr.irstea.fr/airGR-website}{airGR website}.
+For more information and to get started with the package, you can refer to the vignette (\code{vignette("airGR")}) and go on the \href{https://hydrogr.github.io/airGR/}{airGR website}. \cr\cr
-##### References #####
+
+## ---- References
- Le Moine, N. (2008). Le bassin versant de surface vu par le souterrain : une voie d'amélioration des performances et du réalisme des modèles pluie-débit ?, PhD thesis (in French), UPMC - Cemagref Antony, Paris, France, 324 pp. \cr
- Mathevet, T. (2005). Quels modèles pluie-débit globaux pour le pas de temps horaire ? Développement empirique et comparaison de modèles sur un large échantillon de bassins versants, PhD thesis (in French), ENGREF - Cemagref Antony, Paris, France, 463 pp. \cr