models: a geospatial investigation Mark Bernhofen PhD Student - - - PowerPoint PPT Presentation

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models: a geospatial investigation Mark Bernhofen PhD Student - - - PowerPoint PPT Presentation

River size representation in global flood models: a geospatial investigation Mark Bernhofen PhD Student - University of Leeds cn13mvb@leeds.ac.uk GFP Conference, Guangzhou. Session 3 12 June, 2019 Overview Follows on from the global


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River size representation in global flood models: a geospatial investigation

Mark Bernhofen

PhD Student - University of Leeds cn13mvb@leeds.ac.uk

GFP Conference, Guangzhou. Session 3 – 12 June, 2019

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SLIDE 2

Overview

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How do the Global Flood Model river size thresholds affect exposure estimates?

  • Follows on from the global flood model intercomparison work (Trigg et al, 2016).
  • Study found 30-40% agreement between 6 global flood models in Africa.
  • Difficult to quantify the significance of river size representation on model

disagreement using different global flood models.

  • Need some independent (from GFMs) measure of flood extent.
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SLIDE 3

Global Model Thresholds: Nigeria

Drainage Thresholds Global Model 50 km2 Fathom 500 km2 U-Tokyo, ECMWF 1000 km2 CIMA-UNEP 5000 km2 JRC Slide 2/12

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Global Model Thresholds: Nigeria

Drainage Thresholds Global Model 50 km2 Fathom 500 km2 U-Tokyo, ECMWF 1000 km2 CIMA-UNEP 5000 km2 JRC 5000 km2 threshold Slide 2/12

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SLIDE 5

Global Model Thresholds: Nigeria

Drainage Thresholds Global Model 50 km2 Fathom 500 km2 U-Tokyo, ECMWF 1000 km2 CIMA-UNEP 5000 km2 JRC 1000 km2 threshold Slide 2/12

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SLIDE 6

Global Model Thresholds: Nigeria

Drainage Thresholds Global Model 50 km2 Fathom 500 km2 U-Tokyo, ECMWF 1000 km2 CIMA-UNEP 5000 km2 JRC 500 km2 threshold Slide 2/12

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SLIDE 7

Global Model Thresholds: Nigeria

Drainage Thresholds Global Model 50 km2 Fathom 500 km2 U-Tokyo, ECMWF 1000 km2 CIMA-UNEP 5000 km2 JRC 50 km2 threshold Slide 2/12

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SLIDE 8

Global Model Thresholds: Nigeria

Drainage Thresholds Global Model 50 km2 Fathom 500 km2 U-Tokyo, ECMWF 1000 km2 CIMA-UNEP 5000 km2 JRC 5 km2 threshold Slide 2/12

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SLIDE 9
  • Terrain model developed by Nobre et al. (2011)
  • Needs only terrain derived datasets as inputs:
  • Digital Elevation Model (DEM)
  • Drainage directions
  • River upstream drainage area
  • Has been successfully used in studies as a quasi
  • r (0 dimensional) flood model.
  • Quick to run at large-scales.
  • Easily produce an auxiliary dataset of river size

(upstream drainage area)

Height Above Nearest Drainage (H (HAND)

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from Nobre et al. (2011)

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HAND Model Setup

Slide 4/12 Strahler Stream Order HAND height 1 2 m 2 2 m 3 3 m 4 4 m 5 5 m 6 6 m 7 7 m 8 8 m 9 10 m 10 12 m 11 12 m

  • Using MERIT Hydro data
  • HAND heights were “calibrated” using 100y flood

maps in Nigeria and the UK.

  • For rivers with Strahler Stream Orders >=6, JRC’s

100 year flood map was used in Nigeria.

  • JRC’s model was the best of the GFMs in a previous

validation study in Nigeria (Bernhofen et al, 2018)

  • For smaller rivers with stream orders <=7 the

Environment Agency’s 100 year flood zone map for the UK was used.

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HAND Model Quality

Slide 5/12 HAND Model Aggregated GFMs (from Trigg et al, 2015)

Models in Agreement

1m 12m HAND Height

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HAND Model Quality

Slide 5/12 Good Fairly good Fair Fairly poor Poor HAND Model Performance Koppen-Geiger Climate Classifications

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Exposure Data

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  • Using Facebook and Columbia University’s

High Resolution Settlement Layer (HRSL) (30m resolution) in the 22 countries it is available.

  • Use WorldPop data (100m resolution) in all

countries.

  • Can compare results to see how population

data affects the exposure estimates.

HRSL availability

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SLIDE 14

Flood Exposure - Afr frica

Slide 7/12 “%” relates to total population

19% 15% 11% 9% 7% 50 100 150 200 250 5< 50< 500< 1000< 5000<

Population

Millions

Minimum Drainage Area Threshold (km2)

Population Exposed to Flooding (WorldPop)

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SLIDE 15

Flood Exposure - Afr frica

Slide 7/12 “%” relates to total population

12% 9% 6% 5% 4% 20 40 60 80 100 5< 50< 500< 1000< 5000<

Population

Millions

Minimum Drainage Area Threshold (km2)

Population Exposed to Flooding (WorldPop)

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HRSL vs. . WorldPop

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  • 28%
  • 29%
  • 31%
  • 35%
  • 12%
  • 40%
  • 35%
  • 30%
  • 25%
  • 20%
  • 15%
  • 10%
  • 5%

0% 5-50 50-500 500-1000 1000-5000 5000< Percentage Change River Drainage Area Thresholds (km2)

Percentage change in exposure estimates when using HRSL vs. WorldPop Results correspond with Smith et al (2019) Nature Comms.

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Flood Exposure – HRSL

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11% 8% 6% 5% 4% 10 20 30 40 50 60 5< 50< 500< 1000< 5000<

Population

Millions

Minimum Drainage Area Threshold (km2)

Population Exposed to Flooding (HRSL)

“%” relates to total population

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SLIDE 18

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In Interesting Countries

11% 8% 5% 4% 1%

0.5 1 1.5 2 2.5 3 5< 50< 500< 1000< 5000<

Population

Millions

Minimum Drainage Area Threshold (km2) Population Exposed to Flooding (HRSL)

Madagascar

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SLIDE 19

12% 10% 9% 9% 3%

0.2 0.4 0.6 0.8 1 1.2 1.4 5< 50< 500< 1000< 5000<

Population

Millions

Minimum Drainage Area Threshold (km2) Population Exposed to Flooding (HRSL)

In Interesting Countries

Benin

Slide 10/12

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8% 7% 6% 6% 6%

0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 1.8 2 5< 50< 500< 1000< 5000<

Population

Millions

Minimum Drainage Area Threshold (km2) Population Exposed to Flooding (HRSL)

In Interesting Countries

Ivory Coast

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  • Different GFM minimum threshold river sizes result in significantly different

exposure estimates (on average, up to a factor of 2.0).

  • Certain country’s exposure estimates are more sensitive to river size

representation than others.

  • Improving river representation beyond current GFM limits could

incorporate an additional 30% of potential exposed population into the modelling frameworks

  • WorldPop population data overestimates exposure compared to Facebook

High Resolution Settlement Layer, especially on smaller rivers.

Conclusions

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  • Fine tune the HAND model calibration to include different climate zones.
  • Expand study globally
  • Global picture of flood exposure from different size rivers.
  • Can inform global flood modelling community about where it’s important

to consider river size representation and which countries would benefit from improved representation

Next xt Steps

Slide 12/12

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Thanks for listening.