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Three-dimensional Fine Structure of Localized Heavy Rainfalls Measured by Phased Array Weather Radar Shinsuke Satoh 1 , Tomoo Ushio 2 , Shigeharu Shimamura 2 , Koichi Maruo 2 , Fumihiko Mizutani 3 , Masakazu Wada 3 , Hiroshi Hanado 1 , Seiji Kawamura 1 , Seiho Uratsuka 1 and Toshio Iguchi 1 1 NICT, Japan ([email protected]) 2 Osaka University, Japan 3 Toshiba Corporation, Japan 1. Introduction In Japan, severe weather disasters caused by localized heavy rainfalls or tornadoes have occurred frequently in the last several years. Although it is important to measure three dimensional structure of the rapidly developed severe storms, a volume scan by a parabolic antenna requires substantial time of more than 5 minutes. Flash flood in the Toga river, Kobe 28 July 2008 Small radar network observation Invisible region Invisible region Big radar observation F2 tornado in Tsukuba 6 may 2012 The observation area of MLIT C-band radar and X-band MP radar (small blue circles). 2. 3-dim precipitation distribution in isolated cumulonimbus (July 26, 2012) 3-1. PAWR Observation Range 3-2. Back-building localized heavy rainfalls around Uji (Aug 14, 2012) We showed some localized heavy rainfall events observed phased array weather radar using 3-dim visualization. We have developed real-time data processing system and are at work on creating the web page. 5. Summary 17:38: 16 17:40: 16 17:42: 16 17:44:16JS T 17:30: 16 17:32: 16 17:34: 16 17:36: 16 10 km 5 km Detailed 10 sec. 300 range×320 sector AZ ×110 angle EL ×2 byte 20.3 MB / file Total size (13 files) 275 MB / 10sec (~ 2.4TB/day 220 Mbps Normal 30sec. 600 range×300 sector AZ ×110 angle EL ×2 byte 37.8 MB / file Total size (13 files) 493 MB / 30sec (~ 1.4TB/day 131 Mbps Data conversio n section (GPGP U) Data accumul ation section NAS 14.5TB) Offline collecti on section Offline processin g section Monitoring control section IQ data after DBF processing ( ~1 Gbps IQ data before DBF processing (~ 6 Gbps Data after radar processing 220 Mbps DAS (12TB) RAID Antenna Equipment 220 Mbps Handa i AP Serve r RAID 63TB ) Data Transla te Server RAID 42TB) Osaka Univ. JGN-X Access Point (L2 Switch) L3 Switch ssh ssh Petabyte storage (Keihanna) HUB Gb E) 220 Mbps JGN-X NICT NW) Private NW Osaka Univ. NW Osaka Univ. LAN NICT Science Cloud Data release server Kogane i Data analysis server Kogane i 12 km 40 km Kyoto 60 km (radius) Osaka Bay Suita Akashi Kansai Airport Nara Uji Kobe 0400JST 3-3. Stationary line-shaped rain- falls (18:51:20JST, July 22, 2012) 0400JST, Aug 14 2012 4-1. Data processing system 4-2. Publication (http://pawr.nict.go.jp) < Real-time data > < Observation mode and data size / data rate > < Past data > < Evolution of cumulonimbus > 3-dim measurement using phased array radar (10- 30 sec) 3-dim measurement using a parabolic antenna (5-10 min)

1 NICT, Japan ([email protected]) 2 Osaka University, Japan 3 Toshiba Corporation, Japan

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Data after radar processing ( 220 Mbps ). IQ data after DBF processing ( ~1 Gbps ). Three-dimensional Fine Structure of Localized Heavy Rainfalls Measured by Phased Array Weather Radar. Data accumulation section. Data conversion section (GPGPU). Osaka Univ. JGN-X Access Point - PowerPoint PPT Presentation

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Page 1: 1  NICT, Japan  (satoh@nict.go.jp) 2  Osaka University, Japan 3  Toshiba Corporation, Japan

Three-dimensional Fine Structure of Localized Heavy Rainfalls Measured by Phased Array Weather Radar

Shinsuke Satoh 1 , Tomoo Ushio 2, Shigeharu Shimamura 2, Koichi Maruo 2, Fumihiko Mizutani 3, Masakazu Wada 3, Hiroshi Hanado 1, Seiji Kawamura 1, Seiho Uratsuka 1 and Toshio Iguchi 1

1 NICT, Japan ([email protected])2 Osaka University, Japan3 Toshiba Corporation, Japan

1. Introduction ・ In Japan, severe weather

disasters caused by localized heavy rainfalls or tornadoes have occurred frequently in the last several years.

・ Although it is important to measure three dimensional structure of the rapidly developed severe storms, a volume scan by a parabolic antenna requires substantial time of more than 5 minutes.

Flash flood in the Toga river, Kobe ( 28 July 2008 )

Small radar network observation

Invisible regionInvisibleregion

Big radar observation

F2 tornado in Tsukuba ( 6 may 2012 )

The observation area of MLIT C-band radar and X-band MP radar (small blue circles).

2. 3-dim precipitation distribution in isolated cumulonimbus (July 26, 2012)

3-1. PAWR Observation Range

3-2. Back-building localized heavy rainfalls around Uji (Aug 14, 2012)

• We showed some localized heavy rainfall events observed phased array weather radar using 3-dim visualization.

• We have developed real-time data processing system and are at work on creating the web page.

5. Summary17:38:16 17:40:16 17:42:16 17:44:16JST

17:30:16 17:32:16 17:34:16 17:36:16

10 km

5 km

Detailed( 10 sec. )

300 range×320 sector ( AZ ) ×110 angle ( EL ) ×2 byte = 20.3 MB / fileTotal size (13 files) : 275 MB / 10sec (~ 2.4TB/day ⇒ ) 220 Mbps

Normal( 30sec.)

600 range×300 sector ( AZ ) ×110 angle ( EL ) ×2 byte = 37.8 MB / fileTotal size (13 files) : 493 MB / 30sec (~ 1.4TB/day ⇒ ) 131 Mbps

Data conversion section(GPGPU)

Data accumulation section

NAS(14.5TB)

Offline collection section

Offline processing section

Monitoring control section

IQ data after DBF processing ( ~1 Gbps )

IQ data before DBF processing(~ 6 Gbps )

Data after radar processing( 220 Mbps )

DAS(12TB) RAID

Antenna Equipment

( 220 Mbps )

Handai APServer

RAID( 63TB)

Data Translate Server

RAID(42TB)

Osaka Univ. JGN-X Access Point (L2 Switch)

L3 Switch

ssh

ssh

Petabyte storage (Keihanna)

HUB ( GbE)

( 220 Mbps )

JGN-X ( NICT NW)Private NWOsaka Univ. NW

Osaka Univ.LAN

NICTScience Cloud

Data release server( Koganei )

Data analysis server( Koganei )

12 km

40 km

Kyoto60 km (radius)

Osaka Bay

SuitaAkashi

Kansai Airport

Nara

Uji

Kobe

0400JST

3-3. Stationary line-shaped rain- falls (18:51:20JST, July 22, 2012)

0400JST, Aug 14

2012

4-1. Data processing system

4-2. Publication (http://pawr.nict.go.jp)< Real-time data >

< Observation mode and data size / data rate >

< Past data >

< Evolution of cumulonimbus >

3-dim measurement using phased array

radar (10-30 sec)

3-dim measurement using a parabolic

antenna (5-10 min)