• Aucun résultat trouvé

Cross-referencing catchment data: how R can provide essential tools for the development of hydrological models for flood prediction

N/A
N/A
Protected

Academic year: 2021

Partager "Cross-referencing catchment data: how R can provide essential tools for the development of hydrological models for flood prediction"

Copied!
2
0
0

Texte intégral

(1)

HAL Id: hal-02609958

https://hal.inrae.fr/hal-02609958

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.

Cross-referencing catchment data: how R can provide essential tools for the development of hydrological

models for flood prediction

B. Génot, Olivier Delaigue, L. Lebecherel

To cite this version:

B. Génot, Olivier Delaigue, L. Lebecherel. Cross-referencing catchment data: how R can provide essential tools for the development of hydrological models for flood prediction. 15th edition of the International R User Conference, Jul 2019, Toulouse, France. pp.1, 2019. �hal-02609958�

(2)

Cross-referencing catchment data:

how R can provide essential tools for the development of hydrological models for flood prediction

Benoˆıt G´enot1, Olivier Delaigue1, Laure Lebecherel1,2

1 IRSTEA – Hydrology Research Group (HYCAR) – Antony, France

2 Now at Ministery of ecology (Water and Biodiversity Direction) – Paris, France

Hydrologists seek to better understand the processes involved in the catchment response to meteorological events using hydrological models. Model development requires databases combining hydrological, climatic and physical data. Large catchment databases have been developed at Irstea (Antony, France) over the last 30 years. A project was launched in the last years to automate the construction of these databases.

Building hydrological database

I Extracting water flow data from online databases I Checking the location of hydrometric stations

I Delineating catchments boundaries using topographic information

I Aggregating data (climate, morphology) at the catchment scale I Synthesis production (plots, metadata, summary sheets)

I Maintaining data ready to use for modeling applications Processing chain with involved R packages

Location

of hydrometric stations Digital elevation model

Catchments boundaries

Climate Morphology

Landcover National hydrological database

Data at basin scale

Dynamic graphs Modeling Static graphs

rgrass7

raster

httr

dygraphs

statistics

Shiny app for checking the location of stations

I Leaflet maps and upstream drainage are linked with common coordinates in a shiny app which greatly facilitates the process of detecting errors in the spatial location of gauging stations

Dynamic visualization

I Dynamic plots provided thanks to dygraphs facilitate the visual analysis of long times series

I Simultaneous analysis of several variables over a period thanks to links between graphs

Synthetic information

I Production of synthetic sheets showing the main characteristics on the hydrology, topography and climate of the catchment

I Approximately four thousand catchments over France available online at

https://webgr.irstea.fr/en/activities/database-1-2/

I Widely used by various stakeholders in the field of hydrology

References

I Delaigue, O., G´enot, B., Lebecherel, L., Brigode, P., Bourgin, P.Y. (2019).

Hydroclimatic database at the scale of France. IRSTEA, UR HYCAR, Hydrology group, Antony. URL:

https://webgr.irstea.fr/en/activities/database-1-2/

National Research Institute of Science and Technology for Environment and Agriculture

HYDRO

Beno^ıt G´enot <benoit.genot@irstea.fr> https://webgr.irstea.fr useR! 2019 - Toulouse (France)

Références

Documents relatifs

A plot of thé variations of thé coefficient of anisotropy (À) against time at Birling Gap is shown in Figure 4. A cliff fall occurred between 5 * March and 23 rd April 2002 and

Characterization of catchment behaviour and rainfall selection for flash flood hydrological model calibration: catchments of the eastern Pyrenees.. Hydrological Sciences Journal,

uncertainty with flux transport modeling (e.g., such as the uncer- tainties in the meridional drift or di ff erent rotation rates or lack of observations on the solar far-side), the

Moreover, the historical evolution of urban landscape spatial patterns was used to further detail the urbanization process in terms of extent and fragmentation of

Following the GDPR’s revamped interest for pictograms as trans- parency-enhancing means and taking stock of the lessons derived from the few previous attempts to design privacy

• 5 simulations in 1 - for a fixed value of δ, 5 simulations are performed successively for the same plant, for each type of control considered: continuous-time , emulated, first

In an effort to alter the inequities, planners are currently advo- cating the development of small and intermediate towns; these are urban places (of varying population

It is shown here that in the case of coupling groundwater flow and hydrological models – in particular on the regional scale – it is very impor- tant to find a common definition