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land surface hydrology in the european high resolution
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Land Surface Hydrology in the European High-resolution Regional - - PowerPoint PPT Presentation

Land Surface Hydrology in the European High-resolution Regional Reanalysis UERRA Patrick Le Moigne, A. Verrelle, S. Munier, E. Bazile R. Abida, C. Szczypta METEO-FRANCE - CNRM-UMR3589 International Symposium on Regional Reanalysis 2018, Bonn


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Land Surface Hydrology in the European High-resolution Regional Reanalysis UERRA

Patrick Le Moigne, A. Verrelle, S. Munier, E. Bazile

  • R. Abida, C. Szczypta

METEO-FRANCE - CNRM-UMR3589 International Symposium on Regional Reanalysis 2018, Bonn

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Outline

q Context and motivation q Modelling system q Water and Energy balance components q Hydrological evaluation

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Context and Motivation

q UERRA

– Development and production of an ensemble system of regional reanalysis – Estimation of ECVs and their uncertainties

q Motivation of the study

– To use the 1961-2015 55-yr high-resolution reanalysis over Europe – To setup a coupled hydro-meteorological modelling system

  • To assess the reanalysis qualityamong discharges (independent variables)

– For the main European rivers

  • To provide the users:

– An estimate of land surface water balance components » Applications: agriculture, droughts, irrigation, … – An evaluation of simulated discharges against measurements » To be compared to existing systems like EU-HYPE, EFAS for floods, …

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Hydro-meteorological Modelling System

DOWNSCALING @ 5.5km Land Surface Model SURFEX @5.5km

Surface ECVs soil moisture, snow, etc.

No feedback to atm.

ALADIN 3D-VAR 6h @ 11km 2m-Temperature 2m-Relative Humidity Total precipitation Solar radiation Infrared radiation Wind speed MESCAN @ 5.5km Surface Obs Hydrological Model CTRIP @ 0.5°

River discharge, Water table height, floodplain fraction

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ALADIN

Bubnova et al., 1995

MESCAN

Soci et al., 2013

SURFEX

Masson et al., 2013

CTRIP

Decharme et al., 2011

ALADIN is a LAM build from the French global ARPEGE model 3D-Var DA: 6-hourly, conventional obs

  • nly, ERA as 1st guess

Horizontal mesh: 11km MESCAN is a combination of MESAN (SMHI) and CANARI (MF) Surface analysis: obs T2M, RH2M,

  • RR24. Downscaled ALADIN as 1st

guess Horizontal mesh: 5.5km

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SURFEX Energy Budget: 1961-2015

NET RADIATION GROUND FLUX SENSIBLE HEAT FLUX LATENT HEAT FLUX

W/m2 W/m2 W/m2 W/m2

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SURFEX Water Budget: 1961-2015

PRECIPITATION EVAPORATION INFILTRATION RUNOFF

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SURFEX Water Budget: 1961-2015

P – E INFILTRATION / ( P – E ) RUNOFF RUNOFF / ( P – E ) SWE

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Hydrological Evaluation: 1961-2015

CTRIP Network @ 0.5

  • Gauge stations from:

GRDC ARCTICNET French national database Spanish national database

  • Selection criteria:

Min drainage area: 5000 km2 Min 3yr with available data

  • Total number of stations: 427

Drainage Area Future Network @ 1/12

Under development @ CNRM

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Hydrological Evaluation: 1961-2015

Distribution of discharge ratio

How to explain discharge underestimation? Physics of the system: Radiation overestimation, Underestimation of precipitation Human activity not accounted for in the model: Presence of dams

46% 0.5

Distribution of NSE NSE Qsim / Qobs

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Some examples

2015

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The Danube River

Danube river @ Zimnicea (Roumania, 658400km2) – Nash=0.65 Qsim/Qobs=0.97 Discharge (mm/day) Danube river @ Regensburg (Germany, 35400km2) – Nash=0.28 Qsim/Qobs=0.78 Discharge (mm/day)

A complex catchment area in terms of climate, morphology, human practices, etc.

2015 2015

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The Danube River

Typical of a mountainous area with a balance between rain and evaporation during summer, snow in winter, and increasing runoff and infiltration after melting Danube catchment area

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Summary

q A hydro-meteorological modelling system was set up to assess the UERRA reanalysis performance over Europe using independent variables q Production of a climatology of the water balance components: surface runoff, soil deep infiltration, soil moisture, evaporation, etc. q Comparisons over Europe highlight discharge underestimation, that can be attributed to human activity and system errors q Studying the 55-yr reanalysis will help understanding inter-annual variability of river discharge q SURFEX-CTRIP has provided a valuable dataset for users to study droughts, floods, etc. q 1961-2015 data is available in ECMWF MARS archiving system

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Summary

q A hydro-meteorological modelling system was set up to assess the UERRA reanalysis performance over Europe using independent variables q Production of a climatology of the water balance components: surface runoff, soil deep infiltration, soil moisture, evaporation, etc. q Comparisons over Europe highlight discharge underestimation, that can be attributed to human activity and system errors q Studying the 55-yr reanalysis will help understanding inter-annual variability of river discharge q SURFEX-CTRIP has provided a valuable dataset for users to study droughts, floods, etc. q 1961-2015 data is available in ECMWF MARS archiving system

Thank you for your attention