Overview
airGRteaching is an add-on package to the airGR package that
simplifies its use and is teaching-oriented. It allows to use with very
low programming skills the rainfall-runoff models
(GR4H, GR5H, GR4J,
GR5J, GR6J, GR2M,
GR1A) and a snow melt and accumulation model
(CemaNeige). This package also provides graphical devices to help
students to explore data and modelling results.
The airGRteaching package has been designed to fulfil a major
requirement: facilitating the use of the airGR
functionalities by students. The names of the functions and their
arguments were chosen to this end.
The package is mostly based on three families of functions:
- the functions that allow to complete very simply a hydrological
modelling exercise;
- plotting functions to help students to explore observed data and to
interpret the results of calibration and simulation of the GR
models;
- a function which runs a ‘Shiny’ graphical user interface that allows
for displaying in real-time model parameters impacts on
hydrographs.
This package brings into R the hydrological modelling tools developed
at INRAE-Antony (Catchment
Hydrology research group of the HYCAR Research Unit, France).
Installation
install.packages("airGRteaching")
This version of airGRteaching is designed to work with the package
htmlwidgets >= 1.5.2.9000 (troubles with the package dygraphs using
dyplot()
and ShinyGR()
) Install the latest
version of ‘htmlwidgets’ from GitHub with the following command
lines:
install.packages("remotes")
remotes::install_github("ramnathv/htmlwidgets")
Modelling Functions
Three functions allow to complete very simply a hydrological
modelling exercise:
- preparation of data:
PrepGR()
;
- calibration of the models:
CalGR()
;
- simulation with the models:
SimGR()
.
Plotting Functions
airGRteaching provides two types of plotting functions that allow to
produce static (plot()
) or dynamic (dyplot()
)
graphics (incl. mouse events and interactive graphics). The devices
allow to explore observed data and to interpret the results of
calibration and simulation of the GR models.
Graphical user interface
The package also provides the ShinyGR()
function, which
allows to launch a Shiny interface. Thus its is possible to perform:
- interactive flow simulations with parameters modifications;
- automatic calibration;
- display of internal variables evolution;
- time period selection.
A demonstrator of the graphical interface is available for free
online on the Sunshine
platform.
Models
The six hydrological models and the snow melt and accumulation model
already available in airGR are available in airGRteaching. These models
can be called within airGRteaching using the following model names (*:
available in the Shiny interface):
GR4H
: four-parameter hourly lumped hydrological model
(Mathevet, 2005)
GR5H
: five-parameter hourly lumped hydrological model
(Ficchi, 2017; Ficchi et al., 2019)
GR4J
*: four-parameter daily lumped hydrological model
(Perrin et al., 2003)
GR5J
*: five-parameter daily lumped hydrological model
(Le Moine, 2008)
GR6J
*: six-parameter daily lumped hydrological model
(Pushpalatha et al., 2011)
GR2M
*: two-parameter monthly lumped hydrological model
(Mouelhi, 2003; Mouelhi et al., 2006a)
GR1A
: one-parameter annual lumped hydrological model
(Mouelhi, 2003; Mouelhi et al., 2006b)
CemaNeige
: two-parameter degree-day snow melt and
accumulation daily model (combined with GR4H, GR5H, GR4J, GR5J or GR6J)
(Valéry et al., 2014)
For more information and to get started with the package, you can
refer to the vignette
(vignette("get_started", package = "airGRteaching")
) and go
on the airGRteaching
website.
References
- Coron, L., G. Thirel, O. Delaigue, C. Perrin and V. Andréassian
(2017). The Suite of Lumped GR Hydrological Models in an R Package.
Environmental Modelling and Software, 94, 166–171, doi: 10.1016/j.envsoft.2017.05.002.
- Ficchi, A. (2017). An adaptive hydrological model for multiple
time-steps: Diagnostics and improvements based on fluxes consistency.
PhD thesis, Irstea (Antony), GRNE (Paris), France.
- Ficchi, A., C. Perrin and V. Andréassian (2019). Hydrological
modelling at multiple sub-daily time steps: model improvement via
flux-matching. Journal of Hydrology, 575, 1308-1327, doi: 10.1016/j.jhydrol.2019.05.084.
- 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.
- 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.
- Mouelhi S. (2003). Vers une chaîne cohérente de modèles pluie-débit
conceptuels globaux aux pas de temps pluriannuel, annuel, mensuel et
journalier, PhD thesis (in French), ENGREF - Cemagref Antony, Paris,
France, 323 pp.
- Mouelhi, S., C. Michel, C. Perrin and V. Andréassian (2006a).
Stepwise development of a two-parameter monthly water balance model,
Journal of Hydrology, 318(1-4), 200-214, doi: 10.1016/j.jhydrol.2005.06.014.
- Mouelhi, S., C. Michel, C. Perrin. and V. Andreassian (2006b).
Linking stream flow to rainfall at the annual time step: the Manabe
bucket model revisited, Journal of Hydrology, 328, 283-296, doi: 10.1016/j.jhydrol.2005.12.022.
- Perrin, C., C. Michel and V. Andréassian (2003). Improvement of a
parsimonious model for streamflow simulation, Journal of Hydrology,
279(1-4), 275-289, doi: 10.1016/S0022-1694(03)00225-7.
- Pushpalatha, R., C. Perrin, N. Le Moine, T. Mathevet and V.
Andréassian (2011). A downward structural sensitivity analysis of
hydrological models to improve low-flow simulation, Journal of
Hydrology, 411(1-2), 66-76, doi: 10.1016/j.jhydrol.2011.09.034.
- Valéry, A., V. Andréassian and C. Perrin (2014). “As simple as
possible but not simpler”: What is useful in a temperature-based
snow-accounting routine? Part 2 - Sensitivity analysis of the Cemaneige
snow accounting routine on 380 catchments, Journal of Hydrology, 517(0):
1176-1187, doi: 10.1016/j.jhydrol.2014.04.058.