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High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

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Matthias B. Schmidt 3 Motivation [http://www.spiegel.de/fotostrecke/unwetter-ueberschwemmung-in-hamburg-hagel-in-bayern-fotostrecke html] Extreme Flooding Examples from June 2011

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Page 1: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

High-Res. Flash Flooding Estimation

TroposLeipzig

26. January 2016

-Or why do we measure precipitation?

Page 2: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 2

Motivation

Extreme FloodingExamples from June 2011

[http://www.altona.info/2011/06/07/gewitter-regen-hagel-land-unter-in-hamburg/]

Page 3: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 3

Motivation

[http://www.spiegel.de/fotostrecke/unwetter-ueberschwemmung-in-hamburg-hagel-in-bayern-fotostrecke-68908-2.html]

Extreme FloodingExamples from June 2011

Page 4: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 4

What can we do?

Change weather?Fortunately we can’t

Estimate flooding possibility?We might!

Page 5: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 5

X-Band Radars

High spatial resolution (60m)

High temporal resolution (30s)

[http://pattern.zmaw.de/Hamburg.2106.0.html]

Page 6: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 7

Masterthesis - Goals

Hydrology: Higher resolution (X-Band) better?

Flash flooding forecasting possible?

Calculation of flooding probability

Page 7: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 8

Masterthesis - Tools

Shetran“a physically-based spatially-distributed hydrological model“ (J. Ewen et al. (2000))

Radar EnsembleCovariance (U. Germann et al. (2008))

Fractals

Page 8: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 9

Masterthesis - Shetran

Water Flow componentCanopy interception

Evaporation and transpiration

Surface run-off

Transfer between subsurface and river water

Storage and flow in VSS

Page 9: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 10

“spatially-distributed“

Page 10: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 11

Masterthesis - Shetran

“physically based”Conservation of mass

Saint-Venant Eq. (a.k.a. Shallow Water Eq.)

Penman-Monteith Eq.

Boussinesq and Richards Eq.

Numerically solvedImplicit, finite differences

Page 11: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 12

Statistical Model

Example hydrological model

Inflow I Storage Storage Outflow

Inflow II

∑𝒊

𝑵𝒇 𝒊 (𝒙 𝒊 ) ∑

𝒊

𝑵𝒇 𝒊 (𝒙 𝒊 )

∑𝒊

𝑵𝒇 𝒊 (𝒙 𝒊 )

∑𝒊

𝑵𝒇 𝒊 (𝒙 𝒊 )

Page 12: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 13

Masterthesis – Shetran

Page 13: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 14

Masterthesis – Shetran

Page 14: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 15

Masterthesis – Model Output

Input

Vege

tatio

n

Soil

/

VSS

Run-Off/

Overflow/

Saturation

Page 15: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 16

Masterthesis – Model Experiments

What is more severe?In terms of hydrology

Precipitation event 1High intensity

Short duration

Precipitation event 2Low intensity

Long duration

Time (5*30min)

1

2

Same Precipitation Amount

Page 16: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 17

Masterthesis – Model Output

Page 17: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 18

Masterthesis – Radar Ensemble

Statistically based Radar Ensemble GeneratorCovariance approach

Page 18: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 19

Masterthesis – Radar Ensemble

3 mm/h

2.5 mm/h2 mm/h

Page 19: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 20

Masterthesis – Radar Ensemble

3 mm/h

2.5 mm/h2 mm/h

1 mm/h

4 mm/h

2.2 mm/h

Page 20: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 21

Masterthesis – Radar Ensemble

3 mm/h

2.5 mm/h2 mm/h

1 mm/h

4 mm/h

2.2 mm/h

[01 11

⋯ 0110

⋮ ⋮ ⋱ ⋮ ⋮1100

⋯ 0101]

𝑪=𝑳 ⋅𝑳𝑻

Page 21: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 22

Masterthesis – Radar Ensemble

[01 11

⋯ 0110

⋮ ⋮ ⋱ ⋮ ⋮1100

⋯ 0101]⋅

Page 22: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 23

Masterthesis – Radar Ensemble

Page 23: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 24

Early-Warning System

Concept demonstrationImplementation beyond scope of masterthesis

Page 24: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 25

Early-Warning System

Houston

“Hamburg, do we have a problem?”[http://

texasstormchasers.com/tag/squall-line/]

Page 25: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 26

Early-Warning System

[01 11

⋯ 0110

⋮ ⋮ ⋱ ⋮ ⋮1100

⋯ 0101]⋅

Precipitation Ensemble

Ensemble Generator

Page 26: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 27

Early-Warning System

Shetran

Discharge Ensemble

Page 27: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 28

Early-Warning System

Shetran

Discharge Ensemble

Page 28: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 29

Early-Warning System

Houston

“Hamburg, do we have a problem?”[http://

texasstormchasers.com/tag/squall-line/]

“15 out of 25 members issue a warning!”

Page 29: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 30

Summing Up

Higher Resolution has an impact on results

Time (5*30min)

Page 30: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 31

Summing Up

Higher Resolution has an impact on results

Flooding estimation might become possible

Page 32: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 33

5. Germann, U., Berenguer, M., Sempere-Torres, D., Zappa, M. (2008)

6. SHETRAN water flow equations (

http://research.ncl.ac.uk/shetran/water%20flow%20equations.pdf)

7. Ewen, J., Parkin, G. and O'Connell, P.E. (2000). SHETRAN:

Distributed River Basin Flow and Transport Modelling System. ASCE

J. Hydrologic Eng., 5, 250-258. (

http://research.ncl.ac.uk/shetran/SHETRAN_ASCE_paper.pdf)

Literature & Sources

Page 33: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 34

Page 34: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 35

Appendix

Page 35: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 36

Student Research

Real-time Radar calibrationBased on single pulse data

Dynamic Clutter detectionWithout Doppler and Polarimetry

Page 36: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 37

Student Research – Radar calibration

Single-Pulse dataTime-critical code necessary

Fortran core

real-time calibration possible

Page 37: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 38

Student Research – clutter detection

Difficult: No Doppler, no dual pol

Statistical approachNot only clutter map

Not much recent research (everybody has Doppler)

Page 38: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 39

Student Research – clutter detection

Page 39: High-Res. Flash Flooding Estimation Tropos Leipzig 26. January 2016 - Or why do we measure precipitation?

Matthias B. Schmidt 40