• Aucun résultat trouvé

Empirical approach to hydrological modelling: a historical perspective in the case of the GR models

N/A
N/A
Protected

Academic year: 2021

Partager "Empirical approach to hydrological modelling: a historical perspective in the case of the GR models"

Copied!
2
0
0

Texte intégral

(1)

HAL Id: hal-02607860

https://hal.inrae.fr/hal-02607860

Submitted on 16 May 2020

HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

Empirical approach to hydrological modelling: a historical perspective in the case of the GR models

C. Perrin, Vazken Andréassian, M.H. Ramos, Guillaume Thirel, Pierre Nicolle, Olivier Delaigue

To cite this version:

C. Perrin, Vazken Andréassian, M.H. Ramos, Guillaume Thirel, Pierre Nicolle, et al.. Empirical approach to hydrological modelling: a historical perspective in the case of the GR models. EGU General Assembly 2018, Apr 2018, Vienna, Austria. pp.1, 2018. �hal-02607860�

(2)

Empirical approach to hydrological modelling:

a historical perspective in the case of the GR models

• Much research over the past decades on modelling the hydrological response of a catchment to climate variables

• Additional difficulty in the context of environmental change

• No single approach appears best in all cases

• Different modelling approaches have various advantages and drawbacks in different contexts

• Empirical modelling approach: a modelling approach among others

• Main idea: building model structures by testing a large number of hypotheses and options without a priori

• Keep only those which prove useful to improve the predictive power of models

• Resulting models: good compromise between data requirements, complexity, modelling efficiency and ease of use

Charles Perrin, Vazken Andréassian, Maria-Helena Ramos, Guillaume Thirel, Pierre Nicolle and Olivier Delaigue Hydrology Group – HYCAR Research Unit – Irstea, Antony, France

charles.perrin@irstea.fr http://webgr.irstea.fr

1. Why an empirical approach?

2. Start of the GR models

4. A few guidelines for empirical model development

 See our webiste for detailed references on the GR models: http://wegr.irstea.fr

 Implementation of the GR models in the airGR and airGRTeaching R packages:

https://webgr.irstea.fr/modeles/airgr/

 See also tomorrow (HS2.1.1, Fri, 13 Apr, 17:30–19:00, Poster session, Hall A, A.13) on GR models: Santos et al., On the use of a Nash cascade to improve the lag parameter

transposability at different time-steps in hydrological modelling

6. References

5. On the use of GR models This empirical approach was followed by the Catchment Hydrology

research group at Irstea (Antony, France). At the beginning of the 1980’s, Claude Michel started to develop a family of storage-type hydrological models, called GR (standing for ‘Génie rural’).

3. Example of evolution of the daily model structure Main objectives:

 To represent as efficiently as possible the main features of the rainfall-runoff transformation

 To robustly model flows at gauged and ungauged locations

 To enhance model applications for decision-making on risk anticipation and water management

(La Houille Blanche, 1983)

Result : suite of models running at various time steps ranging from sub-hourly to annual

E P

interception En

Pn-Ps Es

Pn

Ps

Q X1

X2 S

R

E P

interception En

Pn-Ps Es

Pn

Ps

0.9 0.1

SH1(X3) SH2(X3)

Q X1

X2

Q9

Qd Qr

S

R

E P

interception En

Pn-Ps Es

Pn

Ps

0.9 0.1

SH1(X3) SH2(X3)

Q X1

X2

F(X4) Q1 Q9

Qd Qr

S

R F(X4)

E P

interception En

Pn-Ps Es

Pn

Ps

0.9 0.1

SH1(X3) SH2(X3)

Q X1

X2

F(X4) Q1 Q9

Qd Qr

S

R F(X4)

Perc

E P

interception En

Pn-Ps Es

Pn

Ps

0.9 0.1

SH2(X3)

Q X1

X2

F(X4,X5) Q1 Q9

Qd Qr

S

R

Perc

F(X4,X5)

GR1-GR2 (Michel, 1983)

GR3

(Edijatno, 1991)

GR4

(Nascimento, 1995)

GR4

(Perrin, 2000)

GR5

(Mathevet, 2005;

Le Moine, 2008)

New formulations Additional UHs

Groundwater exchange function

Leakage from SMA store

Simplified routing Improved formulation of

IGF Interception

SMA store Routing store

GR6

(Pushpalatha, 2013)

Additional routing store

E P

interception En

Pn-Ps Es

Pn

Ps

0.9 0.1

SH2(X3)

Q X1

X2

F(X4,X5) Q1 Q91

Qd Qr1

S

R

Perc

F(X4,X5) Q92

X6 Qr2

 Using large sample of catchments to make models more general, i.e. improve their

transposability in space

 “Crash-testing” models with generalized split sample tests to detect problems of robustness (transposability in time)

 Accepting additional complexity only if it brings significant additional predictive

power (Occam’s razor principle)

 Searching for better models rather than

good models (which do not exist by nature) through systematic comparisons

 Searching for improved model consistency in time (across time steps) and space (with semi-

distributed schemes)

 Searching for flexible structures while avoiding mis- and over-

calibration

(Andréassian et al., HESS, 2009)

 More than 350 published studies using the GR models

 Gradual increase in the applications of the models over the last 30 years

 GR models applied over a wide range of conditions on all the continents

 Models included in various software, operational tools and decision-making systems

6. Conclusion and perspectives

 Empirically developing models provides efficient and versatile model structures.

 But this approach also has limitations (dependency to the testing scheme options, very close competing model structures, difficult to define structure realism, etc.).

 GR models may be seen as an attempt to produce “one-size-fits-all” structures. We know this is not a realistic goal. These models should rather be seen as robust

elementary building blocks from which more complex models can be designed.

 Community of end-users provides much valuable feedbacks to detect model failures.

EGU2018-15734

Références

Documents relatifs

Figure 5-14 Simulated particulate organic carbon (POC) percentage in total organic carbon (TOC) during 2003-2013 under natural and actual conditions: (a) mean monthly variations;

It covers the CODASYL Development Committee's Language Structure Group's report "An Information Algebra" in 1962, continues with the introduc- tion of the infological

In this sense, political correctness is perfectly in line with the new definition that has been given to the concept of politeness at the turn of the 20 th century when “[it]

Coron L., Perrin C., Delaigue O., Andréassian V., Thirel G., airGR: a suite of lumped hydrological models in an R-package, Environmental Modelling and software, in preparation. A

airGR: an R-package suitable for large sample hydrology presenting a suite of lumped hydrological models.. Guillaume Thirel, Olivier

Nous avions déterminé section 4.1.1.3 que le paramètre de maille mesuré pour des NPs d’Au dont la taille est comprise entre 1 et 4 nm augmente rapidement avec la taille des NPs,

The methodology involves using a high level assessment of the footprint that incorporates uncertainty in the inputs based on, for example, publicly available

Au cours de l’année 2012, dans les suites d’un travail de thèse et de mémoire en cours de rédaction (doctorant : Jérôme TISSERAND ; direction : Dr Aline WAGNER : chef