Rainfall nowcasting using Burgers equation GyuWon Lee, Soorok Ryu - - PowerPoint PPT Presentation

rainfall nowcasting using burgers equation
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Rainfall nowcasting using Burgers equation GyuWon Lee, Soorok Ryu - - PowerPoint PPT Presentation

Rainfall nowcasting using Burgers equation GyuWon Lee, Soorok Ryu Kyungpook National University, Daegu, Korea(ROK) R ADAR - BASED NOWCASTING 1. Motion fields of precip. Ex) MAPLE (Variational Echo Tracking: VET) Constant-vector forward


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SLIDE 1

Rainfall nowcasting using Burgers’ equation

GyuWon Lee, Soorok Ryu

Kyungpook National University, Daegu, Korea(ROK)

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SLIDE 2

Constant-vector forward scheme

  • 1. Motion fields of precip.

(Variational Echo Tracking: VET)

RADAR-BASED NOWCASTING

  • Growth/decay (scale of predictability)
  • Non-stationary motion fields

Germann and Zawadzki (2002)

  • 2. Advect precip. fields:

Semi-Lagrangian backward

  • 3. Verification

(compare fcst w/ obs) Observed field Predicted field

Ex) MAPLE

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SLIDE 3

METHODOLOGY

Lagrangian extrapolation (advection) OR Conservation equation We solved this simple advection equation(AE) directly : Type 1 Add diffusion term for spatial filtering (smoothing): advection diffusion equation (ADE) : Type 2

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SLIDE 4

METHODOLOGY However, above two equations assume that the motion vector field is stationary in time (constant motion vectors for entire forecast time) Introduce Burgers’ equation: to allow non-stationarity of motion vectors. The s controls the degree of the smoothness.

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SLIDE 5

METHODOLOGY

Semi-Lagrangian extrapolation (S-L): Ty Type 1 pe 1: advection equation(AE) Ty Type 2 pe 2: advection diffusion equation(ADE) Ty Type 3 pe 3: advection equation(AE) + Burgers’ equation Ty Type 4 pe 4: advection diffusion equation(ADE) + Burgers’ equation

+ +

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SLIDE 6

METHODOLOGY

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SLIDE 7

DATA

1.

  • 1. Cas

ases es

  • 6 events, 2.5 min CAPPI

composite from 3 radars

  • 15 min nowcasting up to 3h

2.

  • 2. Com
  • mput

putation

  • n dom

domai ain

  • Southeast area in South Korea
  • 312 km x 312 km at 0.25 km

resolution (1248 x 1248 pixels)

  • Motion vectors : 10 km resolution
  • Verification domain: 250 km x 250

km (red box)

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SLIDE 8

Forecast Obs R>=Rth R <Rth R >=Rth Hit (a) Miss (c) R< Rth False alarm (b) Correct negative (d)

 2D Contingency table Verification score Formula Probability of detection (POD) a/(a+c) False alarm ratio (FAR) b/(a+b) Critical success index (CSI) a/(a+b+c) Equitable threat score (ETS) (a-w)/(a+b+c-w), w=(a+b)(a+c)/(a+b+c+d)  Categorical scores

SKILL SCORES, ERROR STATISTICS

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SLIDE 9

0300 LST 30 June 2012

Type 1 Advection eq MAPLE

MAPLE VS. AE + DIFFUSION

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SLIDE 10

NON-STATIONARY MOTION VECTORS

Burgers’ equation

initial

VET w/ OBS Vectors w/ Burgers’ eq.

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SLIDE 11

MAPLE VS. AE + NON-STATIONARY +DIFFUSION

3

MAPLE Type 3 s=0.2

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SLIDE 12

MAPLE

MAPLE VS. AE + NON-STATIONARY +DIFFUSION

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SLIDE 13

Skill scores Rth = 0.1mm/h MAPLE Type 4

MAPLE VS. AE + NON-STATIONARY +DIFFUSION

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SLIDE 14

Average skill scores: 6 events “Type 3, 4”

MAPLE VS. AE + NON-STATIONARY +DIFFUSION

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SLIDE 15

Average skill scores: 6 events

  • Lifetime : Type 4( >3h) > Type 3 (around 3h) > Type 2 (2.5h) > MAPLE

(2h) = Type 1

MAPLE VS. AE + NON-STATIONARY +DIFFUSION

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SLIDE 16

Sensitivity to diffusion

Type pe 2: 2: dif iffusion Type pe 4 4: dif iffusion+ n+Bur urgers rs’ e ’ eq. Ave Average ge correlati tion Ave Average ge CSI

MAPLE VS. AE + NON-STATIONARY +DIFFUSION

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SLIDE 17

NON-STATIONARY MOTION VECTORS

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SLIDE 18

NON-STATIONARY MOTION VECTORS

Non-stationarity?

2 3 2 3 2 3 2 3 2 3

Type 3, 4 (inclusion of Burgers’ equation) outperform

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SLIDE 19

NON-STATIONARY MOTION VECTORS

Type 2, 4 (inclusion of diffusion equation) perform better

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SLIDE 20
  • Introd
  • duc

uced ed nowc wcas asti ting ng based o ed on advec ecti tion (

  • n (diffus

fusion)

  • n)

equat ation w with B Burgers’ e equ quation

  • Perfor

formanc ance: e: MAPLE LE ~ ~ Adv dvec ecti tion e

  • n eq. < Adv

dvec ecti tion e

  • n eq. + Burger

gers e eq. (S (S-L ~ ~ Ty Type1 < < Ty Type2 < < Ty Type 3 3 < < Ty Type 4 4)

  • Use o
  • f diffusion t

term rm and n non-stati tationar

  • nary moti

tion

  • n v

vector tor improv

  • ves

es f forec ecas asti ting ng s skill s scor

  • res

es

  • When nons

nsta tati tionar

  • narity

ty of motion

  • n f

fiel elds ds i is s strong,

  • ng, t

the pre recipitation f fore recasts u using B Burg urgers rs’ e equa uation (Ty (Type pe3, Type 4 4) show s

  • w signi

gnifi ficant ant i impr prov

  • vem

ement ent. .

SUMMARY