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Research on Lightning Nowcasting and Warning System and Its Application Wen Yao Chinese Academy of Meteorological Sciences Beijing, China yaowen@camscma.cn 2016.07 1 CONTENTS 1 Lightning Hazards 2 System Introduction 3 System


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Research on Lightning Nowcasting and Warning System and Its Application

Chinese Academy of Meteorological Sciences Beijing, China yaowen@camscma.cn 2016.07

Wen Yao

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CONTENTS

Lightning Hazards 1

System Introduction

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System Application

3 Future Work 4

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Lightning hazards

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About 1000 people,

  • n average, have been dead or

injured by lightning strikes every year in China.

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200 400 600 800 1000 1200 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015

Fatalities Injuries

Lightning hazards

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Lightning Lightning-attributed attributed Forest fire Forest fire

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Oil depot Explosion Oil depot Explosion

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Power failures Power failures

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Lightning hazards

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Traffic Loss Traffic Loss

Aviation Loss Aviation Loss

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Tree, 1.80%

Microelectronics devices,

34.50% Home and office appliances , 23.10% Factory equipment, 6% Electric power equipment , 24.80% Building and structures, 7.80% Others, 2%

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Loss types of lightning-caused

  • bjects

Lightning hazards

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CONTENTS

Lightning Hazards 1

System Introduction

2

System Application

3 Future Work 4

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The Lightning Nowcasting and Warning System (CAMS_LNWS) was developed by Chinese Academy

  • f

Meteorological Sciences (CAMS). The system proposed a lightning characteristic diagnose and nowcasting scheme in typical regions, and adopted a multi-data, multi-parameter and multi- algorithm lightning nowcasting method. The CAMS_LNWS work 24 hours every day and renew the warning products every 15 minutes automatically, which can realize 0-1 hours , 1 × 1 km of lightning forecasting.

System Introduction

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Method

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 Establish the diagnostic indicators of lightning forecasting  Analyze the lightning activity in different areas of China  Obtain the relationship of the lightning frequency and location with the radar, satellite and other observations during a thunderstorm

System Introduction

analysis of lightning between and satellite data

Characteristics of lightning activity at different stages. (Lightning Initiation、 development、 Ending)

analysis of lightning space- time distribution characteristics analysis of lightning between and Radar Data analysis of lightning between and Surface Electric Field Data

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Diagnostic Indicators

System Introduction

 Height of Radar strong echoes  Maximum thickness of 35dBz  Proportion of radar strong echoes  Maximum reflectivity within 14km around first stroke of stratiform CG

 Horizontal gradient of composite reflectivity

 Distribution of vertical velocity  Echo volume per flash  Volume per frequency  Black-Body Temperature(TBB) of satellite  Electromagnetic signal threshold  …

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Concerns:  Lightning Initiation  Lightning Ending  Stratiform Regions Lightning

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Key Method

  • Lightning Initiation- Echo top height of 40dBz ≥ -10℃ stratification height

Echo top heights of 30、 35 40dBz and 0℃ stratification height in different isolated cells Echo top heights of 30 35 40dBz and -10℃ stratification height in different isolated cells

Thunderstorm Non-Thunderstorm Thunderstorm Non-Thunderstorm

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Key Method

  • Lightning Initiation- P value should be used for subsidiary discrimination

P= Volume (Reflectivity ≥40dBz and Height ≥ 0 ℃ height) Volume (Reflectivity ≥25dBz and Height ≥ 0 ℃ height) × 100%

First lightning

P>5%

Echo top

  • f 40dBz

≥ 0℃ height Echo top

  • f 40dBz

≥ -10℃ height Non-thunderstorm p ≥5% And Keep above for two radar scan time Thunderstorm Lightning will occur in 15 minutes

No Yes Yes No Yes No

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  • Lightning Ending

③ Echo top height of 40dBz < -20℃ height

  • Volume30-15

(Reflectivity ≥30dBz and Height ≥ -15 ℃ height) <230km3 Volume30-15/ Volume18 < 1%

We can combine the conditions of , , to forecast lightning ending.

Key Method

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  • Stratiform regions Lightning

Most researches aimed at the lightning activity in the convective region some statiform region with higher reflectivity are corresponding to the weak lightning activity Higher fault alarm rate in statiform region

Statiform regions lightning

Key Method

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1 2 3 4 5 6 7 8 9 10 50 100 150 200 250

Cloud-to-ground lightning (flashes) Height (km)

Height of maximum reflectivity within 14 km around first stroke point of stratiform CG 10 20 30 40 50 60 70 80 50 100 150 200

Cloud-to-ground lightning (flashes) Reflectivity (dBZ)

Maximum reflectivity above first stroke point of stratiform CG Maximum reflectivity within 14 km around first strok point of stratiform CG

Key Method

Analyze the Height and maximum reflectivity of stratiform CGs strike the ground at or near the edge of a region, and refer to the distinguish method of stratiform and convective region proposed by Steiner et al. (1995), and later improved by Biggerstaff and Listemaa, zhong, Xiao et al (2007), We adopt identify algorithm to forecast the lightning activity in the stratiform and convective regions.

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10:00-15:00 Jun 29,2015 Observation Before using the identify method After using the identify method

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Technology (?) Product (?) Evaluate (?) Input Data (?) Technology

Design Scheme

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Technology

Large temporal

  • spatial scale

Small temporal

  • spatial scale

Integrated Forecasting Technology

Statistical analysis of archival data. Lightning occurrence probability in 0-24 h based on synoptic situation forecasting products

  • Temporal Resolution: 12 h
  • Spatial Resolution: 200km× 200 km
  • Parameters: several instability parameters
  • Products: Lightning occurrence probability in this region during 0~12 h
  • Input: Sounding Data
  • Temporal Resolution: 12h
  • Spatial Resolution: 200 km× 200 km
  • Model: 2D Electrification-Discharge Thunderstorm Model
  • Product: Lightning occurrence probability in this region during 0~12 h
  • Temporal Resolution: 30min-1h
  • Spatial Resolution: 10× 10 km
  • Parameters: TBB et. al.
  • Product: Lightning occurrence probability in each grid during 0~2 h
  • Temporal Resolution: 6 min
  • Spatial Resolution: 1 km× 1 km
  • Parameters: Echo Intensity and its Variability Rate, Echo Tops et. al.
  • Product: Lightning occurrence probability in each grid during 0~2 h
  • To identify and track lightning activity area with real-time data from lightning location system.
  • To forecast potential lightning activity area
  • Observation by single station or network. Real-time detection of ground electric field and lightning activity.
  • To forecast lightning occurrence probability in the vicinal region

建立了均 Multi-source observation data: sounding data, satellite, radar, lightning, surface electric field data and so on.(from large temporal spatial scale to small temporal spatial scale)

Input Data

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Synoptic Situation Sounding Data Model Products Satellite Data Radar Data Lightning Detection Data Surface Electric Field Data

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Technology

 The system was designed in framework and modularization.  Based on algorithm of area identification, tracing and extrapolation algorithm and decision trees algorithm  Considering different data situation, the system can not only use single data application module to produce forecasting result for different temporal and special scales, but also synthesis different application module to generate products through weight combination method.

23 Model Forecasting Application Module Sounding Data Application Module Satellite Data Application Module Radar Data Application Module Ground Electric Field Data Application Module Lightning Data Application Module

Synthesis Forecast

  • ing

Module

Decision Tree

Region recognition, tracing, extrapolation

Potential Forecasting for Lightning Activity

Voice alarm Forecasting Products for Different Temporal and Special Scales

Lightning Occurrence Probability Moving Trend of Lightning Activity Area Lightning Occurrence Probability of Key Area

Technology

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Technology

Product

Lightning Occurrence Probability Moving Trend of Lightning Activity Area Lightning Occurrence Probability

  • f Key Area

Evalution of pruducts in real time

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In order to meet the different needs of public meteorological service and special meteorological service, three kinds of Lightning nowcasting and warning products were showed. In order to make an objective assessment of result, we also evaluate the accuracy of the warning products by Probability of Detection (POD), Fault Alarm Rate (FAR) and Threat Score (Ts).

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CONTENTS

Lightning Hazards 1

System Introduction

2

System Application

3 Future Work 4

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Mean value Sample number POD 0.81 36 FAR 0.67 TS 0.31

Tianjin: 11:00-20:00, June 16, 2009 . Severe weather hit Tianjin, with thunder storms, heavy rainfall and strong winds. Forecast results in 15minutes intervals

Evaluation results

Case of Tianjin CAMS_LNWS Application

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Guangdong:16:00-23:45, July 18, 2009.

Case of Guangdong in Southern China

CAMS_LNWS Application

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Case of Henan in central of China

CAMS_LNWS Application

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29 0~15min 15~30min 30~45min 45~60min

Case of Shanghai during the World Expo2010.

Key Region Moving trend

CAMS_LNWS Application

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CAMS_LNWS Application

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 Lightning nowcasting and warning products

Public services

 Electric power  forestry  Tourism  Telecom

Special service

 ……

Application in forestry department Application in electric power department Application for public meteorological service

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CONTENTS

Lightning Hazards 1

System Introduction

2

System Application

3 Future Work 4

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Regional lightning nowcasting index and algorithm should be improved further to decrease FAR.

0~2h lightning nowcasting 0 6h lightning short-term forecast

Developing the coupling

  • f

charge-discharge model of thunderclouds with meso-scale model to develop a 0~6 hour numerical forecasting method.

Future Work

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6h 18h 6h 18h 6h 18h 2h

Lightning nowcasting and warning system

2h

Lightning numerical Prediction system Lightning potential forecasting system

Future Work

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