Modelling human interventions in the Rhine basin using the - - PowerPoint PPT Presentation

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Modelling human interventions in the Rhine basin using the - - PowerPoint PPT Presentation

Modelling human interventions in the Rhine basin using the hydrological model SIMGRO Erik Querner Contents Introduction framework of the study Simgro model application to the Rhine basin Climate and land use scenarios


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Modelling human interventions in the Rhine basin using the hydrological model SIMGRO

Erik Querner

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Contents

  • Introduction

framework of the study

  • Simgro model application to the Rhine

basin Climate and land use scenarios

  • Adaptation measures
  • Conclusions
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Objective of the study

  • How does a physical based hydrological model

perform for a basin as the Rhine (snow module)

  • Quantify the effect of land use and climate

change on river flows

  • What are the changes on droughts or low flows
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Hydrological model SIMGRO

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Aim of model SIMGRO

  • Physical based model
  • For practical problems

and hydrological research

DTM

Model area Subcatchments Nodes

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Modelling the Rhine basin

Basin area: 160 000 km2

Mainly Switzerland, Germany, France, Luxemburg, Belgium >> Netherlands

Finite element network: 5 x 5 km ; 8144 cells Surface water: Larger rivers > 400 km2 630 sub catchments Groundwater: data Rhine Commission (CHR) Land use: CORINE Soil map FAO

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Drainage network is derived from DTM (Voigt e.a., 2007) Important for interaction groundwater – surface water

Surface water

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& & & & & & & & & & & &

Bern Köln Nancy Basel Trier Zürich Koblenz Mannheim Freiburg Duisburg Stuttgart Strasbourg

& & & & & & & & & & & &

Bern Köln Nancy Basel Trier Zürich Koblenz Mannheim Freiburg Duisburg Stuttgart Strasbourg

SW: sub catchments GW: transmissivity

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42 gauging stations used Procedure to compare calculated-measured discharges in term of Nash- Sutcliffe model efficiency

Gauging stations

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Lobith – compare measured and calculated

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Lobith 0.90 Main 0.74 Neckar 0.65 Moselle 0.79 Switzerland (5 stat) 0.30

  • Downstr. Switzerl. (13 stat)

0.79 Nash-Sutcliffe modelling efficiency

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Scenarios

  • Land use change (extreme)

all crops to grass ~ 33% area changed all crops to forest ,,

  • Climate change

scenarios from Dutch Meteorological Institute (standardized)

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Climate scenarios for the Netherlands Moderate Warm Extreme scenario conform IPCC

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Climate scenarios: some details

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Lower than threshold: 88 days 139 153 Threshold (navigation, water use agric., etc)

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Scenario – land use

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  • Picture landuse and climat scen

year 1992

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Is it acceptation or adaptation Note the mark on high water levels (Moselle)

Strategy to follow

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In the past: use of flood levees

There is an end in raising dikes

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  • Reduce floods and droughts

Strategy: analysis concept

In time

Rive r flow

Reduced range is also favourable in terms of WFD

  • Further implications of climate change
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  • Make use of the groundwater system (retain water in the

ground) Before the wet season have enough storage cap. available to cope with peak flows After the wet period save water for the dry period

  • Natural flood defenses

The Ecoflood report gives guidelines

  • n how to restore flood plains
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  • SIMGRO model: has the ability to model practical

situations (scenarios like land use and climate change)

  • Climate change has a much larger impact on discharges

and droughts than extreme changes in land use

  • Consider natural flood defence measures

Conclusions

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Is this the challenge we are facing?

Is this Acceptation or Adaptation ?

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Thank you