Doppler Weather Radar System

Model: Radar Doppler Weather Compact DualPolarimetricX-band Weather Radaravailable inthemarket* Classi ed asoneofthesmallestandlightest * asofJune2013(DualPolarimetricDopplerWeather Radar) real-time 3Dmonitoringof meteorological phenomenaatamodestinvestment. Combining thetwotypesofWeather Radar, FURUNOdelivers“Multi-RadarSystem”capableofconducting Weather Radaravailableinthemarket. phase totheextentthatcanbeclassi edasoneofsmallestandlightestDualPolarimetricDoppler localised rainstormscanbepredicted. Moreover, theWR-2100hasbeendownsizedduringdevelopment structure aswellmovement ofacumulonimbus,whichcausesprecipitation, thedevelopmentofshort By conductinghighspatiotemporalresolution monitoringofthedevelopmentprocess, three-dimensional Weather Radargraspsomni-directional precipitation intensityin50-metre-mesh insix-second-intervals. With ultrahighde nitionspatiotemporalresolution capability, theWR-2100DualPolarimetricDoppler Doppler Weather RadarWR-2100andDopplerWeather RadarWR-50. theleadingmarketshareFURUNO, whichhasearned inmarineRadar, provides DualPolarimetricX-band and lightest DualPolarimetric Doppler Weather Radar availablein themarket. development phase totheextentthatcanbeclassi ed asoneofthesmallest their development. Moreover, the WR-2100 hasbeendownsized duringits movement ofacumulonimbus, whichcauses rainstormsinordertopredict monitors thedevelopmentprocess, three-dimensional structureaswell intensity in50-metre-meshsix-second-intervals. Also, the WR-2100 Dual PolarimetricDoppler Weather Radargraspsomni-directionalprecipitation With ultrahighde nitionspatiotemporal resolutioncapability, the WR-2100 Doppler Weather RadarWR-2100 Compact DualPolarimetric X-band WR-2100 meteorological monitoring. at modestcost, whichenables comprehensive, real-time Weather Radar, “Multi-Radar System” canbeconstructed When combinedwithDualPolarimetric X-bandDoppler Its compactunitfacilitateseaseof installation. The WR-50 detectsthenimbusandtracks itsmovement. Doppler Weather RadarWR-50 Compact X-band Model: Radar Doppler Weather Compact X-band WR-50 www.furuno.fr Bordeaux-Mérignac, France FURUNO FRANCES.A.S. www.furuno.co.uk Havant, Hampshire,U.K. FURUNO www.furunousa.com Camas, Washington,U.S.A. FURUNO U.S.A.,INC. www.furuno.com Nishinomiya, Hyogo,Japan FURUNO ELECTRICCO.,LTD. SPECIFICATIONS 65 kg144lb WR-2100 Doppler Weather Radar Compact DualPolarimetricX-band Power Consumption Power Supply Communication Port Data Correction Output Data Data Processing Unit Scan Modes Maximum Range Antenna Rotation Speed Scan Angle Vertical Peak OutputPower Beam Width Operating Frequency Antenna Polarity Model Name ( UK ) LIMITED 650 W max 650 W 100-240 VAC, SinglePhase, 50/60Hz - Suppression from ofsignalreturns land,Clutter suppression Distance attenuation, Rain attenuation, Excessive Dopplervelocity, Differential reflectivity factor ZDR,Rainfall intensityR(mm/h) KDP (deg/km),Correlation ρHV, polarizations coefficient two between (m/s), Cross difference polarization phaseφdp(deg),Specific differential phase Reflectivity factor Zh(dBZ),Dopplervelocity V (m/s),Dopplervelocity width W Externally arranged PPI, CAPPI, RHI(Sector Scanavailable) Approx. 30km 16 max. rpm (adjustable) -2 to 90degrees (adjustable) 100 beams) W (bothhorizontal andvertical 2.7 degrees beams) (bothhorizontal andvertical 9 GHzband (VerticalDual polarimetric andHorizontal), simultaneously transmitted/received WR-2100 www.furuno.se Västra Frölunda, Sweden FURUNO SVERIGEAB www.furuno.no Ålesund, Norway FURUNO NORGE A/S www.furuno.dk Hvidovre, Denmark FURUNO DANMARKA/S www.furuno.es Madrid, Spain FURUNO ESPAÑAS.A.

Compact X-bandDopplerWeather Radar Compact DualPolarimetric X-bandDoppler Weather Radar ▲ ▲ ▲ ▲ ▲ ▲ ▲ ▲ ▲ precipitation diameter ofprecipitationparticles aswelldiscriminatingtypesof Straightforward interface withpower supplycableandLANfordatacommunications ofnimbusatafast velocityofnimbusanddetectshorizontalmovement Outputs movement rate Compact, light-weightRadomeantenna of shortlocalisedrainstorm, whennetworkedinto “Multi-Radar System” Suitable forlocalisedmeteorologicalmonitoringaswell theverticalstructureofacumulonimbus 3D scantoobserve Outputs dualpolarimetricDopplerinformation velocityofnimbus Outputs moving High-precision, real-timemonitoringofprecipitationintensity Weather Radaravailable inthemarket Classi ed asoneofthesmallestandlightestDualPolarimetric Doppler weight: 65kg) 1024 204 (rain, snow, etc.) www.rico.com.sg Singapore RICO www.furuno.com.ru St. Petersburg,RussianFederation FURUNO EURUS LLC www.furuno.pl Gdynia, Poland FURUNO POLSKASp.Zo.o. www.furuno. Espoo, Finland FURUNO FINLANDOY ( ø1086 PTE ) LTD (Radome diameter:108cm, Radome (Radome diameter:60cm, Radomeweight:28kg) WR-50 Busan, Korea FURUNO KOREACO.,LTD. www.furuno.com.cy Limassol, Cyprus FURUNO (CYPRUS) LTD www.furuno.gr Piraeus, Greece FURUNO HELLASS.A. www.furuno.de Rellingen, Germany FURUNO DEUTSCHLANDGmbH (Zdr, Kdp) forcomputing 300 W max 300 W 100-240 VAC, SinglePhase, 50/60Hz LAN 100Base-TX×1port Suppression from ofsignalreturns land,Clutter suppression Distance attenuation, Rain attenuation, Excessive Dopplervelocity, Rainfall intensityR(mm/h) Reflectivity factor Zh(dBZ),Dopplervelocity V (m/s), Incorporated PPI, CAPPI Approx. 30km 16 max. rpm (adjustable) -2 to 90degrees (adjustable) 50 W 5.0 degrees 9GHz band Horizontal WR-50 28 kg62lb WR-50 Doppler Weather Radar Compact X-band WR-2100 (mm/h) minivand tothemonitoringlocation. The antennaunitcanbetuckedina Compact andlightweight! ø602 13103SK Printed inJapan Catalogue No. R-203 30 76 810 D -

One of the smallest oppler Solution for meteorological for Solution monitoring analysis and Model: WR-2100 Radar Doppler Weather Compact DualPolarimetricX-band

and lightest

W eather

R Model: Radar Doppler Weather Compact X-band adar WR-50

S ystem www.furuno.com - CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation High precision 3D meteorological monitoring of Compact Dual Polarimetric X-band Doppler Weather Radar by the WR-2100 by the WR-2100WR-2100 ▲ Classi edFURUNO Multi-Radaras one of the smallestSystem and lightest Data from the identical altitude isClassi ed to be extracted as one and of the monitored, smallest andsuitable lightest Dual VerticalPolarimetric cross-section Doppler scan on a cumulonimbus is conducted, FURUNO’s solution for meteorological for observing the development of Weathera cumulonimbus. Radar available (Altitude: in 1-9 the km) market (Radome diameter:suitable 108 cm, for Radome observing the development of a cumulonimbus. weight: 65 kg)

Sample images of 3D meteorological monitoring ▲ Weather Radar available in the market* High-precision, real-time monitoring of precipitation intensity (mm/h) ▲ monitoring and analysis Outputs moving velocity of nimbus ▲ Outputs dual polarimetric Doppler information (Zdr, Kdp) for computing FURUNO, which has earned the leading market share in marine Radar, provides Dual Polarimetric X-band diameter of precipitation particles as well as discriminating types of Doppler Weather Radar WR-2100 and Doppler Weather Radar WR-50. precipitation (rain, snow, etc.)

Utilising the technical expertise FURUNO has accumulated ▲ 3D scan to observe the vertical structure of a cumulonimbus ▲ through the development of marine Radar that has earned With ultra high de nition spatiotemporal resolution capability, the WR-2100 Dual Polarimetric Doppler Suitable for localised meteorological monitoring as well as for monitoring Compact and light weight! Weather Radar grasps omni-directional precipitation intensity in 50-metre-mesh in six-second-intervals. of short localised rainstorm, when networked into “Multi-Radar System” The antenna unit can be tucked in a the leading market share, FURUNO, in close collaboration By conducting high spatiotemporal resolution monitoring of the development process, three-dimensional minivand to the monitoring location. with universities and other business organisations, is now structure as well as movement of a cumulonimbus, which causes precipitation, the development of short Compact X-band Doppler Weather Radar WR-50 working on development of solution for meteorological localised rainstorms can be predicted. Moreover, the WR-2100 has been downsized during the development ▲ phaseIn order to theto predict extent the that development can be classi ed of short as localized one of the rainstorms, smallest following and lightest the abruptDual Polarimetric development Doppler of a Compact, light-weight Radome antenna (Radome diameter: 60 cm, Radome weight: 28 kg)

monitoring and analysis. FURUNO’s high quality compact ▲ Weathercumulonimbus, Radar available high spatiotemporal in the market. resolution monitoring of meteorological phenomena is required. Outputs movement velocity of nimbus and detects horizontal movement of nimbus at a fast rate

(July 6, 2013, 19:03 to 19:05) ▲ (August 6, 2013, 18:30 to 18:59) X-band Doppler Weather Radar is indispensable for localised By downsizing both Dual Polarimetric Doppler Weather Radar and Single Polarimetric Doppler Weather Straightforward interface with power supply cable and LAN cable for data communications Combining the two types of Weather Radar, FURUNO delivers “Multi-Radar System” capable of conducting On CAPPI observation, horizontal cross-section scans of a cumulonimbus are conducted On RHI observation, vertical cross-section scans of a cumulonimbus weather forecasting to materialise better safety in the Radar, FURUNO makes remarkable reduction on the deployment cost a possibility. Also, it has become real-timeeasier to 3D create monitoring “Multi-Radar of meteorological System” by combining phenomena both at Radara modest units. investment. at the equal altitudes. The altitude of a developed cumulonimbus top may exceed 10 km. are conducted, hence easily grasping development status of a Precipitation can be observed at higher altitude in a greatly developed cumulonimbus. cumulonimbus. This case example clearly shows the active society where the impact arising from the meteorological High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” * as of June 2013 (Dual Polarimetric Doppler Weather Radar) SPECIFICATIONS up-and-down movement of nimbus. makes possible the provision of precautious information about prospective sediment disasters as well as disasters can be diminished. Model Name WR-2100 WR-50 information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. Antenna Polarity Dual polarimetric (Vertical and Horizontal), simultaneously transmitted/received Horizontal Doppler Weather Radar System DopplerOperating Frequency velocity9 observationGHz band 9GHz band *The map data used in this page has been provided through Digital Japan Web System of Geospatial Information Authority of Japan. Beam Width 2.7 degrees (both horizontal and vertical beams) 5.0 degrees *The terrain elevation data of the background has been obtained from "Shuttle Radar Topography Mission (SRTM)", conducted by Jet Propulsion Laboratory, the US. byPeak the Output WR-2100 Power and the100 WR-50 W (both horizontal and vertical beams) 50 W -Solution for meteorological monitoring and analysis - Vertical Scan Angle -2 to 90 degrees (adjustable) -2 to 90 degrees (adjustable) SuitableAntenna Rotationfor monitoring Speed nimbus16 rpm max. movement (adjustable) velocity and wind eld. 16 rpm max. (adjustable) System Con guration Maximum Range Approx. 30 km Approx. 30 km Scan Modes PPI, CAPPI, RHI (Sector Scan available) PPI, CAPPI On Doppler observation, by monitoring Doppler velocity WR-2100 WR-50 Data Processing Unit Externally arranged Incorporated Output Data Reflectivity factor Zh (dBZ), Doppler velocity V (m/s), Doppler velocity width W Reflectivityof the factornimbus, Zh (dBZ),moving Doppler velocity velocity of the V nimbus, (m/s), namely, (m/s), Cross polarization difference phase φdp (deg), Specific differential phase Rainfallwind intensity speed R and (mm/h) direction, can be computed. In this Signal Processing Unit Radar Unit Radar Unit KDP (deg/km), Correlation coefficient between two polarizations ρHV, example, warm colors indicate the winds that that WR-2100-DP WR-50-RDU WR-50-RDU Differential reflectivity factor ZDR, Rainfall intensity R (mm/h) move away from the Radar antenna, while cold colours Soaring needs for Weather Radar that stem Data Correction Distance attenuation, Rain attenuation, Excessive Doppler velocity, Distance attenuation, Rain attenuation, Excessive Doppler velocity, Antenna Unit Suppression of signal returns from land, Clutter suppression Suppressionindicate of the signal winds returns that frommove land, towards Clutter the suppression Radar from intensifying extreme weather WR-2100-ATU Display Unit Display Unit Display Unit Communication Port - LAN 100Base-TX×1portantenna. The arrow lengths and direction indicate the Power Supply 100-240 VAC, Single Phase, 50/60 Hz 100-240 VAC, Single Phase, 50/60 Hz One of the smallest WR-2100-DPU WR-50-DPU WR-50-DPU wind speed and direction, respectively. A number of arguments on the global scale as to how to tackle problems Power Consumption 650 W max 300 W max and lightest arising from extreme weather, such as short localised rainstorms, tornados Compact Dual Polarimetric X-band Compact X-band and other adverse phenomena, have been taking place recently. Subsequently, Compact X-band Doppler Weather Radar ø1086 Doppler Weather Radar PC Internet WR-2100 WR-50 urgent needs have been recognised for the solution of localised weather Doppler Weather Radar 65 kg 144 lb 28 kg 62 lb (December 6, 2013, 10:00) Detailed nimbus movement and velocity forecasting as part of social infrastructure so as to protect human lives and Model: WR-50 assets from unexpected natural disasters, i.e., river oods, landslides, etc., CompactImage Dual Polarimetric of “Multi-Radar X-band System” hence delivering better safety and peace of mind to society. Doppler Weather Radar Approximately 30km PPI (Plan Position Indicator) observation 1024 810 Model: WR-2100 by the WR-2100 and the WR-50 Dual Polarimetric Doppler Weather Radar to Monitoring is to be conducted at a xated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. 76 contribute to prediction of occurrence of rainstorms 204 The antenna is rotated while xing its Compact Dual Polarimetric X-band Compact X-band elevation angle.ø602 PPI observation30 at low Dual Polarimetric Doppler Weather Radar simultaneously transmits and elevation angle generates rainfall amount on receives horizontally- and vertically-polarised radio waves. It is capable of Doppler Weather Radar WR-2100 Doppler Weather Radar WR-50 the ground. Also, when the rainfall amount computing the movement velocity of nimbus, as can be obtained from Single data is accumulated for the duration of 1 With ultra high de nition spatiotemporal resolution capability, the WR-2100 The WR-50 detects the nimbus and tracks its movement. hour, accumulated rainfall amount for 1 hour 3 mm 4 mm 5 mm Polarimetric Doppler Weather Radar using horizontally-polarised radio waves, Dual Polarimetric Doppler Weather Radar grasps omni-directional precipitation Its compact unit facilitates ease of installation. can be calculated. Also, by analysing the as well as precise precipitation intensity. intensity in 50-metre-mesh in six-second-intervals. Also, the WR-2100 Doppler velocity obtained by PPI observation Compact Dual Polarimetric X-band 13103SK Printed in Japan When combined with Dual Polarimetric X-band Doppler FURUNO ELECTRIC CO., LTD. FURUNO ESPAÑA S.A. FURUNO FINLAND OY FURUNO DEUTSCHLAND GmbHat low elevation angle, low-level wind shear Doppler Weather Radar monitors the development process, three-dimensional structure as well as Nishinomiya, Hyogo, Japan Madrid, Spain Espoo, Finland Rellingen, Germany Catalogue No. R-203 Shape of precipitation particles is horizontally-long oval, due to the effect from Weather Radar, “Multi-Radar System” can be constructed www.furuno.com www.furuno.es www.furuno. www.furuno.de can be obtained. Model: WR-2100 movement of a cumulonimbus, which causes rainstorms in order to predict FURUNO U.S.A., INC. FURUNO DANMARK A/S FURUNO POLSKA Sp. Z o.o. FURUNO HELLAS S.A. Compact X-band atmosphere and gravity. Using these characteristics, Dual Polarimetric Doppler at modest cost, which enables comprehensive, real-time Camas, Washington, U.S.A. Hvidovre, Denmark Gdynia, Poland Piraeus, Greece Doppler Weather Radar their development. Moreover, the WR-2100 has been downsized during its www.furunousa.com www.furuno.dk www.furuno.pl www.furuno.gr *The map data used in this page has been provided meteorological monitoring. ( ) Model: WR-50 Weather Radar obtains diameters of precipitation particles to compute precise 6 mm 7 mm 8 mm development phase to the extent that can be classi ed as one of the smallest FURUNO UK LIMITED FURUNO NORGE A/S FURUNO EURUS LLC FURUNO (CYPRUS) LTD through Digital Japan Web System of Geospatial Compact Dual Polarimetric X-band Doppler Weather Radar Havant, Hampshire, U.K. Ålesund, Norway St. Petersburg, Russian Federation Limassol, Cyprus precipitation intensity. www.furuno.co.uk(Rainfall amount observation / Junewww.furuno.no 26, 2013, 14:00 to 15:00) www.furuno.com.ru(Precipitation intensity observationwww.furuno.com.cy / November 13, 2012, 17:26) Information Authority of Japan. Compactand X-band lightest Doppler Dual Weather Polarimetric Radar Doppler Weather Radar available in the market. FURUNO FRANCE S.A.S. FURUNO SVERIGE AB RICO (PTE) LTD FURUNO KOREA CO., LTD. www.furuno.com Bordeaux-Mérignac, France Västra Frölunda, Sweden Singapore Busan, Korea www.furuno.fr www.furuno.se www.rico.com.sg CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation High precision 3D meteorological monitoring of CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation High precision 3D meteorological monitoring of by the WR-2100 Compact Dual Polarimetric X-band Doppler Weather Radarby the WR-2100 by the WR-2100 by the WR-2100WR-2100 Data from the identical altitude is to be extracted and monitored, suitable Vertical cross-section scan on a cumulonimbus is conducted, FURUNO Multi-Radar System ▲ Data from the identical altitude is to be extracted and monitored, suitable Vertical cross-section scan on a cumulonimbus is conducted, Classi edFURUNO Multi-Radaras one of the smallestSystem and lightest for observing the developmentClassi ed of a cumulonimbus. as one of the (Altitude: smallest 1-9 and km) lightest Dual Polarimetricsuitable for Doppler observing the development of a cumulonimbus. FURUNO’s solution for meteorological for observing the development of Weathera cumulonimbus. Radar available (Altitude: in 1-9 the km) market (Radome diameter:suitable 108 cm, for Radome observing the development of a cumulonimbus. Sample images of 3D meteorological monitoring weight: 65 kg)

Utilising the technical expertise FURUNO has accumulated ▲ 3D scan to observe the vertical structure of a cumulonimbus ▲ through the development of marine Radar that has earned With ultra high de nition spatiotemporal resolution capability, the WR-2100 Dual Polarimetric Doppler Suitable for localised meteorological monitoring as well as for monitoring Compact and light weight! Weather Radar grasps omni-directional precipitation intensity in 50-metre-mesh in six-second-intervals. of short localised rainstorm, when networked into “Multi-Radar System” The antenna unit can be tucked in a the leading market share, FURUNO, in close collaboration By conducting high spatiotemporal resolution monitoring of the development process, three-dimensional minivand to the monitoring location. with universities and other business organisations, is now structure as well as movement of a cumulonimbus, which causes precipitation, the development of short Compact X-band Doppler Weather Radar WR-50 localised rainstorms can be predicted. Moreover, the WR-2100 has been downsized during the development working on development of solution for meteorological In order to predict the development of short localized rainstorms, following the abrupt development of a ▲ phaseIn ordercumulonimbus, to theto predict extent the highthat development spatiotemporalcan be classi ed of short resolution as localized one ofmonitoring the rainstorms, smallest of meteorological following and lightest the abruptDualphenomena Polarimetric development is required. Doppler of a Compact, light-weight Radome antenna (Radome diameter: 60 cm, Radome weight: 28 kg) monitoring and analysis. FURUNO’s high quality compact ▲ Weathercumulonimbus, Radar available high spatiotemporal in the market. resolution monitoring of meteorological phenomena is required. (July 6, 2013, 19:03 to 19:05) Outputs movement velocity of nimbus and detects horizontal(August 6, movement 2013, 18:30 of to nimbus18:59) at a fast rate

By downsizing both Dual Polarimetric Doppler Weather Radar and Single Polarimetric Doppler Weather (July 6, 2013, 19:03 to 19:05) ▲ (August 6, 2013, 18:30 to 18:59) X-band Doppler Weather Radar is indispensable for localised By Radar,downsizing FURUNO both makes Dual Polarimetric remarkable Dopplerreduction Weather on the Radardeployment and Single cost aPolarimetric possibility. Also,Doppler it has Weather become On CAPPI observation, horizontal cross-sectionStraightforward scans ofinterface a cumulonimbus with power are conducted supply cable andOn LAN RHI cableobservation, for data vertical communications cross-section scans of a cumulonimbus Combining the two types of Weather Radar, FURUNO delivers “Multi-Radar System” capable of conducting On CAPPI observation, horizontal cross-section scans of a cumulonimbus are conducted On RHI observation, vertical cross-section scans of a cumulonimbus weather forecasting to materialise better safety in the Radar,easier FURUNO to create makes “Multi-Radar remarkable System” reduction by combiningon the deployment both Radar cost units. a possibility. Also, it has become at the equal altitudes. The altitude of a developed cumulonimbus top may exceed 10 km. are conducted, hence easily grasping development status of a real-timeeasier to 3D create monitoring “Multi-Radar of meteorological System” by combining phenomena both at Radara modest units. investment. at thePrecipitation equal altitudes. can beThe observed altitude atof highera developed altitude cumulonimbus in a greatly developed top may exceed cumulonimbus. 10 km. are conducted,cumulonimbus. hence This easily case grasping example development clearly shows status the active of a High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” Precipitation can be observed at higher altitude in a greatly developed cumulonimbus. cumulonimbus. This case example clearly shows the active society where the impact arising from the meteorological High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” up-and-down movement of nimbus. * as ofmakes June 2013possible (Dual the Polarimetric provision Doppler of precautious Weather Radar)information about prospective sediment disasters as well as SPECIFICATIONS up-and-down movement of nimbus. makes possible the provision of precautious information about prospective sediment disasters as well as disasters can be diminished. information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. Model Name WR-2100 WR-50 information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. AntennaDoppler Polarity velocityDual polarimetricobservation (Vertical and Horizontal), simultaneously transmitted/received Horizontal Doppler Weather Radar System *The map data used in this page has been provided through Digital Japan Web System of Geospatial Information Authority of Japan. DopplerOperating Frequency velocity9 observationGHz band 9GHz band *The *Themap terraindata used elevation in this data page of has the beenbackground provided has through been obtainedDigital Japan from Web "Shuttle System Radar of GeospatialTopography Information Mission (SRTM)", Authority conducted of Japan. by Jet Propulsion Laboratory, the US. Beamby Widththe WR-2100 and2.7 the degrees WR-50 (both horizontal and vertical beams) 5.0 degrees *The terrain elevation data of the background has been obtained from "Shuttle Radar Topography Mission (SRTM)", conducted by Jet Propulsion Laboratory, the US. byPeak the Output WR-2100 Power and the100 WR-50 W (both horizontal and vertical beams) 50 W -Solution for meteorological monitoring and analysis - VerticalSuitable Scan Anglefor monitoring-2 to nimbus 90 degrees movement (adjustable) velocity and wind field. -2 to 90 degrees (adjustable) System Configuration SuitableAntenna Rotationfor monitoring Speed nimbus16 rpm max. movement (adjustable) velocity and wind eld. 16 rpm max. (adjustable) System Con guration Maximum Range Approx. 30 km Approx. 30 km Scan Modes PPI, CAPPI, RHI (Sector Scan available) PPI, CAPPIOn Doppler observation, by monitoring Doppler velocity WR-2100 WR-50 On Doppler observation, by monitoring Doppler velocity WR-2100 WR-50 Data Processing Unit Externally arranged Incorporatedof the nimbus, moving velocity of the nimbus, namely, Output Data Reflectivity factor Zh (dBZ), Doppler velocity V (m/s), Doppler velocity width W Reflectivityof thewind factornimbus, speed Zh (dBZ),moving and direction,Doppler velocity velocity canof the be V nimbus, computed.(m/s), namely, In this Signal Processing Unit Radar Unit Radar Unit (m/s), Cross polarization difference phase φdp (deg), Specific differential phase Rainfallwind intensityexample, speed R and (mm/h) warm direction, colors canindicate be computed. the winds Inthat this move SignalWR-2100-DP Processing Unit RadarWR-50-RDU Unit RadarWR-50-RDU Unit KDP (deg/km), Correlation coefficient between two polarizations ρHV, example, warm colors indicate the winds that that WR-2100-DP WR-50-RDU WR-50-RDU Differential reflectivity factor ZDR, Rainfall intensity R (mm/h) away from the Radar antenna, while cold colours move away from the Radar antenna, while cold colours Antenna Unit Data Correction Distance attenuation, Rain attenuation, Excessive Doppler velocity, Distance attenuation,indicate the Rain winds attenuation, that move Excessive towards Doppler the Radar velocity, Soaring needs for Weather Radar that stem indicate the winds that move towards the Radar AntennaWR-2100-ATU Unit Display Unit Display Unit Display Unit Suppression of signal returns from land, Clutter suppression Suppressionantenna. of signal The returns arrow from lengths land, and Clutter direction suppression indicate the WR-2100-ATU Communication Port - LAN 100Base-TX×1portantenna. The arrow lengths and direction indicate the from intensifying extreme weather DisplayWR-2100-DPU Unit DisplayWR-50-DPU Unit DisplayWR-50-DPU Unit wind speed and direction, respectively. Power Supply 100-240 VAC, Single Phase, 50/60 Hz 100-240 VAC, Single Phase, 50/60 Hz One of the smallest WR-2100-DPU WR-50-DPU WR-50-DPU wind speed and direction, respectively. A number of arguments on the global scale as to how to tackle problems Power Consumption 650 W max 300 W max and lightest arising from extreme weather, such as short localised rainstorms, tornados Compact Dual Polarimetric X-band Compact X-band and other adverse phenomena, have been taking place recently. Subsequently, PC CompactInternet X-band Doppler Weather Radar ø1086 Doppler Weather Radar PC Internet WR-2100 WR-50 urgent needs have been recognised for the solution of localised weather Doppler Weather Radar 65 kg 144 lb (December 6, 2013, 10:00) Detailed nimbus movement and velocity 28 kg 62 lb (December 6, 2013, 10:00) Detailed nimbus movement and velocity forecasting as part of social infrastructure so as to protect human lives and Image of “Multi-Radar System” Model: WR-50 assets from unexpected natural disasters, i.e., river oods, landslides, etc., CompactImage Dual Polarimetric of “Multi-Radar X-band System” PPI (Plan Position Indicator) observation hence delivering better safety and peace of mind to society. Doppler Weather Radar Approximately 30km Approximately 30km PPI (Plan Position Indicator) observation by the WR-2100 and the WR-501024 by the WR-2100 and the WR-50 810 Model: WR-2100 Monitoring is to be conducted at a fixated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. Dual Polarimetric Doppler Weather Radar to Monitoring is to be conducted at a xated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. The antenna is rotated while fixing its 76 contribute to prediction of occurrence of rainstorms 204 The elevationantenna isangle. rotated PPI while observation xing its at low Compact Dual Polarimetric X-band Compact X-band elevationelevation angle.ø602 angle PPI generatesobservation 30 rainfall at low amount on Dual Polarimetric Doppler Weather Radar simultaneously transmits and elevation angle generates rainfall amount on Doppler Weather Radar WR-2100 Doppler Weather Radar WR-50 the ground. Also, when the rainfall amount receives horizontally- and vertically-polarised radio waves. It is capable of the ground.data is accumulatedAlso, when the for rainfall the duration amount of 1 data is accumulated for the duration of 1 computing the movement velocity of nimbus, as can be obtained from Single With ultra high de nition spatiotemporal resolution capability, the WR-2100 The WR-50 detects the nimbus and tracks its movement. hour, accumulated rainfall amount for 1 hour hour,can accumulated be calculated. rainfall Also, amount by analysing for 1 hour the Polarimetric Doppler Weather Radar using horizontally-polarised radio waves, 3 mm 4 mm 5 mm Dual Polarimetric Doppler Weather Radar grasps omni-directional precipitation Its compact unit facilitates ease of installation. can Dopplerbe calculated. velocity Also, obtained by analysing by PPI observationthe as well as precise precipitation intensity. intensity in 50-metre-mesh in six-second-intervals. Also, the WR-2100 Doppler velocity obtained by PPI observation Compact Dual Polarimetric X-band at low elevation angle,13103SK low-level Printed wind inshear Japan When combined with Dual Polarimetric X-band Doppler FURUNO ELECTRIC CO., LTD. FURUNO ESPAÑA S.A. FURUNO FINLAND OY FURUNO DEUTSCHLAND GmbHat low elevation angle, low-level wind shear Doppler Weather Radar monitors the development process, three-dimensional structure as well as Nishinomiya, Hyogo, Japan Madrid, Spain Espoo, Finland Rellingen, Germany can be obtained. Catalogue No. R-203 Shape of precipitation particles is horizontally-long oval, due to the effect from Weather Radar, “Multi-Radar System” can be constructed www.furuno.com www.furuno.es www.furuno. www.furuno.de can be obtained. Model: WR-2100 movement of a cumulonimbus, which causes rainstorms in order to predict FURUNO U.S.A., INC. FURUNO DANMARK A/S FURUNO POLSKA Sp. Z o.o. FURUNO HELLAS S.A. Compact X-band atmosphere and gravity. Using these characteristics, Dual Polarimetric Doppler at modest cost, which enables comprehensive, real-time Camas, Washington, U.S.A. Hvidovre, Denmark Gdynia, Poland Piraeus, Greece *The map data used in this page has been provided Doppler Weather Radar their development. Moreover, the WR-2100 has been downsized during its www.furunousa.com www.furuno.dk www.furuno.pl www.furuno.gr *The throughmap data Digital used Japanin this Webpage System has been of Geospatialprovided meteorological monitoring. ( ) Model: WR-50 Weather Radar obtains diameters of precipitation particles to compute precise 6 mm 7 mm 8 mm developmentCompact Dual Polarimetric phase to X-band the extent Doppler thatWeather can Radar be classi ed as one of the smallest FURUNO UK LIMITED FURUNO NORGE A/S FURUNO EURUS LLC FURUNO (CYPRUS) LTD throughInformation Digital Japan Authority Web ofSystem Japan. of Geospatial CompactCompact Dual X-bandPolarimetric Doppler X-band Weather Doppler Radar Weather Radar Havant, Hampshire,(Rainfall U.K. amount observation Ålesund,/ June 26,Norway 2013, 14:00 to 15:00)St. Petersburg,(Precipitation Russian Federation intensity observationLimassol, /Cyprus November 13, 2012, 17:26) precipitation intensity. www.furuno.co.uk(Rainfall amount observation / Junewww.furuno.no 26, 2013, 14:00 to 15:00) www.furuno.com.ru(Precipitation intensity observationwww.furuno.com.cy / November 13, 2012, 17:26) Information Authority of Japan. Compactand X-band lightest Doppler Dual Weather Polarimetric Radar Doppler Weather Radar available in the market. FURUNO FRANCE S.A.S. FURUNO SVERIGE AB RICO (PTE) LTD FURUNO KOREA CO., LTD. www.furuno.com Bordeaux-Mérignac, France Västra Frölunda, Sweden Singapore Busan, Korea www.furuno.fr www.furuno.se www.rico.com.sg CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation High precision 3D meteorological monitoring of CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation by the WR-2100 by the WR-2100 High precision 3D meteorological monitoring of Compact Dual Polarimetric X-band Doppler Weather Radar by the WR-2100 by the WR-2100WR-2100 Data from the identical altitude is to be extracted and monitored, suitable Vertical cross-section scan on a cumulonimbus is conducted, FURUNO Multi-Radar System ▲ Data from the identical altitude is to be extracted and monitored, suitable Vertical cross-section scan on a cumulonimbus is conducted, for observing the development of a cumulonimbus. (Altitude: 1-9 km) suitable for observing the development of a cumulonimbus. Classi edFURUNO Multi-Radaras one of the smallestSystem and lightest Classi ed as one of the smallest and lightest Dual Polarimetric Doppler FURUNO’s solution for meteorological for observing the development of Weathera cumulonimbus. Radar available (Altitude: in 1-9 the km) market (Radome diameter:suitable 108 cm, for Radome observing the development of a cumulonimbus. Sample images of 3D meteorological monitoring weight: 65 kg)

Utilising the technical expertise FURUNO has accumulated ▲ 3D scan to observe the vertical structure of a cumulonimbus ▲ through the development of marine Radar that has earned With ultra high de nition spatiotemporal resolution capability, the WR-2100 Dual Polarimetric Doppler Suitable for localised meteorological monitoring as well as for monitoring Compact and light weight! Weather Radar grasps omni-directional precipitation intensity in 50-metre-mesh in six-second-intervals. of short localised rainstorm, when networked into “Multi-Radar System” The antenna unit can be tucked in a the leading market share, FURUNO, in close collaboration By conducting high spatiotemporal resolution monitoring of the development process, three-dimensional minivand to the monitoring location. with universities and other business organisations, is now structure as well as movement of a cumulonimbus, which causes precipitation, the development of short Compact X-band Doppler Weather Radar WR-50 localised rainstorms can be predicted. Moreover, the WR-2100 has been downsized during the development In order to predict the development of short localized rainstorms, following the abrupt development of a working on development of solution for meteorological ▲ cumulonimbus, high spatiotemporal resolution monitoring of meteorological phenomena is required. phaseIn order to theto predict extent the that development can be classi ed of short as localized one of the rainstorms, smallest following and lightest the abruptDual Polarimetric development Doppler of a Compact, light-weight Radome antenna (Radome diameter: 60 cm, Radome weight: 28 kg) monitoring and analysis. FURUNO’s high quality compact ▲ (July 6, 2013, 19:03 to 19:05) (August 6, 2013, 18:30 to 18:59) Weathercumulonimbus, Radar available high spatiotemporal in the market. resolution monitoring of meteorological phenomena is required. Outputs movement velocity of nimbus and detects horizontal movement of nimbus at a fast rate

By downsizing both Dual Polarimetric Doppler Weather Radar and Single Polarimetric Doppler Weather (July 6, 2013, 19:03 to 19:05) ▲ (August 6, 2013, 18:30 to 18:59) Radar, FURUNO makes remarkable reduction on the deployment cost a possibility. Also, it has become On CAPPI observation, horizontal cross-section scans of a cumulonimbusX-band are conducted Doppler WeatherOn RHI observation, Radar verticalis indispensable cross-section scans for of a cumulonimbuslocalised By downsizing both Dual Polarimetric Doppler Weather Radar and Single Polarimetric Doppler Weather Straightforward interface with power supply cable and LAN cable for data communications Combining the two types of Weather Radar, FURUNO delivers “Multi-Radar System” capable of conducting On CAPPI observation, horizontal cross-section scans of a cumulonimbus are conducted On RHI observation, vertical cross-section scans of a cumulonimbus easier to create “Multi-Radar System” by combining both Radar units. at the equal altitudes. The altitude of a developed cumulonimbus topweather may exceed forecasting10 km. are toconducted, materialise hence easily better grasping safety development in statusthe of a Radar, FURUNO makes remarkable reduction on the deployment cost a possibility. Also, it has become Precipitation can be observed at higher altitude in a greatly developed cumulonimbus. cumulonimbus. This case example clearly shows the active real-timeeasier to 3D create monitoring “Multi-Radar of meteorological System” by combining phenomena both at Radara modest units. investment. at the equal altitudes. The altitude of a developed cumulonimbus top may exceed 10 km. are conducted, hence easily grasping development status of a High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” Precipitation can be observed at higher altitude in a greatly developed cumulonimbus. cumulonimbus. This case example clearly shows the active society where the impactup-and-down arising movement from of nimbus. the meteorological High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” makes possible the provision of precautious information about prospective sediment disasters as well as * as of June 2013 (Dual Polarimetric Doppler Weather Radar) SPECIFICATIONS up-and-down movement of nimbus. makes possible the provision of precautious information about prospective sediment disasters as well as information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. disasters can be diminished. Model Name WR-2100 WR-50 Doppler velocity observation information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. Antenna Polarity Dual polarimetric (Vertical and Horizontal), simultaneously transmitted/received Horizontal Doppler Weather Radar System *The map data used in this page has been provided through Digital Japan Web System of Geospatial Information Authority of Japan. DopplerOperating Frequency velocity9 observationGHz band 9GHz band *The terrain elevation data of the background has been obtained from "Shuttle Radar Topography Mission (SRTM)", conducted by Jet Propulsion Laboratory, the US. by the WR-2100 and the WR-50 *The map data used in this page has been provided through Digital Japan Web System of Geospatial Information Authority of Japan. Beam Width 2.7 degrees (both horizontal and vertical beams) 5.0 degrees *The terrain elevation data of the background has been obtained from "Shuttle Radar Topography Mission (SRTM)", conducted by Jet Propulsion Laboratory, the US. byPeak the Output WR-2100 Power and the100 WR-50 W (both horizontal and vertical beams) 50 W -Solution for meteorological monitoring and analysis - Suitable for monitoring nimbus movement velocity and wind field. Vertical Scan Angle -2 to 90 degrees (adjustable) -2 to 90 degrees (adjustable) System Configuration SuitableAntenna Rotationfor monitoring Speed nimbus16 rpm max. movement (adjustable) velocity and wind eld. 16 rpm max. (adjustable) System Con guration Maximum Range Approx. 30 km Approx. 30 km On Doppler observation, by monitoring Doppler velocity Scan Modes PPI, CAPPI, RHI (Sector Scan available) PPI, CAPPI WR-2100 WR-50 On Doppler observation, by monitoring Doppler velocity of the nimbus, moving velocity of the nimbus, namely, WR-2100 WR-50 Data Processing Unit Externally arranged Incorporated wind speed and direction, can be computed. In this Output Data Reflectivity factor Zh (dBZ), Doppler velocity V (m/s), Doppler velocity width W Reflectivityof the factornimbus, Zh (dBZ),moving Doppler velocity velocity of the V nimbus, (m/s), namely, Signal Processing Unit Radar Unit Radar Unit example, warm colors indicate the winds that move (m/s), Cross polarization difference phase φdp (deg), Specific differential phase Rainfallwind intensity speed R and (mm/h) direction, can be computed. In this WR-2100-DP WR-50-RDU WR-50-RDU Signal Processing Unit Radar Unit Radar Unit KDP (deg/km), Correlation coefficient between two polarizations ρHV, example, warm colors indicate the winds that that away from the Radar antenna, while cold colours WR-2100-DP WR-50-RDU WR-50-RDU Differential reflectivity factor ZDR, Rainfall intensity R (mm/h) move away from the Radar antenna, while cold colours Antenna Unit indicate the winds that move towards the Radar Data Correction Distance attenuation, Rain attenuation, Excessive Doppler velocity, Distance attenuation, Rain attenuation, Excessive Doppler velocity, Soaring needs for Weather Radar that stem indicate the winds that move towards the Radar WR-2100-ATU Display Unit Display Unit Display Unit antenna. The arrow lengths and direction indicate the Antenna Unit Suppression of signal returns from land, Clutter suppression Suppression of signal returns from land, Clutter suppression WR-2100-ATU Communication Port - LAN 100Base-TX×1portantenna. The arrow lengths and direction indicate the WR-2100-DPU WR-50-DPU WR-50-DPU from intensifying extreme weather wind speed and direction, respectively. Display Unit Display Unit Display Unit Power Supply 100-240 VAC, Single Phase, 50/60 Hz 100-240 VAC, Single Phase, 50/60 Hz One of the smallest WR-2100-DPU WR-50-DPU WR-50-DPU wind speed and direction, respectively. A number of arguments on the global scale as to how to tackle problems Power Consumption 650 W max 300 W max and lightest arising from extreme weather, such as short localised rainstorms, tornados Compact Dual Polarimetric X-band Compact X-band PC Internet and other adverse phenomena, have been taking place recently. Subsequently, Compact X-band Doppler Weather Radar ø1086 Doppler Weather Radar PC Internet WR-2100 WR-50 urgent(December needs 6, have 2013, been 10:00) recognised for the solutionDetailed of nimbuslocalised movement weather and velocity Doppler Weather Radar 65 kg 144 lb 28 kg 62 lb (December 6, 2013, 10:00) Detailed nimbus movement and velocity forecasting as part of social infrastructure so as to protect human lives and Image of “Multi-Radar System” Model: WR-50 assets from unexpected natural disasters, i.e., river oods, landslides, etc., CompactImage Dual Polarimetric of “Multi-Radar X-band System” PPI (Plan Position Indicator) observation Approximately 30km hence delivering better safety and peace of mind to society. Doppler Weather Radar Approximately 30km PPI (Plan Position Indicator) observation by the WR-2100 and the WR-50 1024 by the WR-2100 and the WR-50 810 Monitoring is to be conducted at a fixated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. Model: WR-2100 Dual Polarimetric Doppler Weather Radar to Monitoring is to be conducted at a xated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. The antenna is rotated while fixing its 76 contribute to prediction of occurrence of rainstorms elevation angle. PPI observation at low 204 The antenna is rotated while xing its elevation angle generates rainfall amount on Compact Dual Polarimetric X-band Compact X-band elevation angle.ø602 PPI observation30 at low Dual Polarimetric Doppler Weather Radar simultaneously transmits and elevation angle generates rainfall amount on the ground. Also, when the rainfall amount Doppler Weather Radar WR-2100 Doppler Weather Radar WR-50 receives horizontally- and vertically-polarised radio waves. It is capable of data is accumulated for the duration of 1 the ground. Also, when the rainfall amount data is accumulated for the duration of 1 computing the movement velocity of nimbus, as can be obtained from Single hour, accumulated rainfall amount for 1 hour With ultra high de nition spatiotemporal resolution capability, the WR-2100 The WR-50 detects the nimbus and tracks its movement. can be calculated. Also, by analysing the hour, accumulated rainfall amount for 1 hour Polarimetric Doppler Weather Radar using horizontally-polarised radio waves, 3 mm 4 mm 5 mm Dual Polarimetric Doppler Weather Radar grasps omni-directional precipitation Its compact unit facilitates ease of installation. Doppler velocity obtained by PPI observation can be calculated. Also, by analysing the as well as precise precipitation intensity. intensity in 50-metre-mesh in six-second-intervals. Also, the WR-2100 Doppler velocity obtained by PPI observation Compact Dual Polarimetric X-band at low elevation angle, low-level wind shear 13103SK Printed in Japan When combined with Dual Polarimetric X-band Doppler FURUNO ELECTRIC CO., LTD. FURUNO ESPAÑA S.A. FURUNO FINLAND OY FURUNO DEUTSCHLAND GmbHat low elevation angle, low-level wind shear Doppler Weather Radar can be obtained. monitors the development process, three-dimensional structure as well as Nishinomiya, Hyogo, Japan Madrid, Spain Espoo, Finland Rellingen, Germany Catalogue No. R-203 Shape of precipitation particles is horizontally-long oval, due to the effect from Weather Radar, “Multi-Radar System” can be constructed www.furuno.com www.furuno.es www.furuno. www.furuno.de can be obtained. Model: WR-2100 movement of a cumulonimbus, which causes rainstorms in order to predict FURUNO U.S.A., INC. FURUNO DANMARK A/S FURUNO POLSKA Sp. Z o.o. FURUNO HELLAS S.A. Compact X-band atmosphere and gravity. Using these characteristics, Dual Polarimetric Doppler *The map data used in this page has been provided at modest cost, which enables comprehensive, real-time Camas, Washington, U.S.A. Hvidovre, Denmark Gdynia, Poland Piraeus, Greece Doppler Weather Radar through Digital Japan Web System of Geospatial their development. Moreover, the WR-2100 has been downsized during its www.furunousa.com www.furuno.dk www.furuno.pl www.furuno.gr *The map data used in this page has been provided meteorological monitoring. ( ) Model: WR-50 Compact Dual Polarimetric X-band Doppler Weather Radar Weather Radar obtains diameters of precipitation particles to compute precise 6 mm Information Authority7 mm of Japan. 8 mm development phase to the extent that can be classi ed as one of the smallest FURUNO UK LIMITED FURUNO NORGE A/S FURUNO EURUS LLC FURUNO (CYPRUS) LTD through Digital Japan Web System of Geospatial Compact X-band Doppler Weather Radar (Rainfall amount observation / June 26, 2013, 14:00 to 15:00) (Precipitation intensity observation / November 13, 2012, 17:26) Compact Dual Polarimetric X-band Doppler Weather Radar Havant, Hampshire, U.K. Ålesund, Norway St. Petersburg, Russian Federation Limassol, Cyprus precipitation intensity. www.furuno.co.uk(Rainfall amount observation / Junewww.furuno.no 26, 2013, 14:00 to 15:00) www.furuno.com.ru(Precipitation intensity observationwww.furuno.com.cy / November 13, 2012, 17:26) Information Authority of Japan. Compactand X-band lightest Doppler Dual Weather Polarimetric Radar Doppler Weather Radar available in the market. FURUNO FRANCE S.A.S. FURUNO SVERIGE AB RICO (PTE) LTD FURUNO KOREA CO., LTD. www.furuno.com Bordeaux-Mérignac, France Västra Frölunda, Sweden Singapore Busan, Korea www.furuno.fr www.furuno.se www.rico.com.sg CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation High precision 3D meteorological monitoring of CAPPI (Constant Altitude Plan Position Indicator) observation RHI (Range Height Indicator) observation by the WR-2100 by the WR-2100 High precision 3D meteorological monitoring of Compact Dual Polarimetric X-band Doppler Weather Radar by the WR-2100 by the WR-2100WR-2100 Data from the identical altitude is to be extracted and monitored, suitable Vertical cross-section scan on a cumulonimbus is conducted, FURUNO Multi-Radar System ▲ Data from the identical altitude is to be extracted and monitored, suitable Vertical cross-section scan on a cumulonimbus is conducted, for observing the development of a cumulonimbus. (Altitude: 1-9 km) suitable for observing the development of a cumulonimbus. Classi edFURUNO Multi-Radaras one of the smallestSystem and lightest Classi ed as one of the smallest and lightest Dual Polarimetric Doppler FURUNO’s solution for meteorological for observing the development of Weathera cumulonimbus. Radar available (Altitude: in 1-9 the km) market (Radome diameter:suitable 108 cm, for Radome observing the development of a cumulonimbus. Sample images of 3D meteorological monitoring weight: 65 kg)

Utilising the technical expertise FURUNO has accumulated ▲ 3D scan to observe the vertical structure of a cumulonimbus ▲ through the development of marine Radar that has earned With ultra high de nition spatiotemporal resolution capability, the WR-2100 Dual Polarimetric Doppler Suitable for localised meteorological monitoring as well as for monitoring Compact and light weight! Weather Radar grasps omni-directional precipitation intensity in 50-metre-mesh in six-second-intervals. of short localised rainstorm, when networked into “Multi-Radar System” The antenna unit can be tucked in a the leading market share, FURUNO, in close collaboration By conducting high spatiotemporal resolution monitoring of the development process, three-dimensional minivand to the monitoring location. with universities and other business organisations, is now structure as well as movement of a cumulonimbus, which causes precipitation, the development of short Compact X-band Doppler Weather Radar WR-50 localised rainstorms can be predicted. Moreover, the WR-2100 has been downsized during the development In order to predict the development of short localized rainstorms, following the abrupt development of a working on development of solution for meteorological ▲ cumulonimbus, high spatiotemporal resolution monitoring of meteorological phenomena is required. phaseIn order to theto predict extent the that development can be classi ed of short as localized one of the rainstorms, smallest following and lightest the abruptDual Polarimetric development Doppler of a Compact, light-weight Radome antenna (Radome diameter: 60 cm, Radome weight: 28 kg) monitoring and analysis. FURUNO’s high quality compact ▲ (July 6, 2013, 19:03 to 19:05) (August 6, 2013, 18:30 to 18:59) Weathercumulonimbus, Radar available high spatiotemporal in the market. resolution monitoring of meteorological phenomena is required. Outputs movement velocity of nimbus and detects horizontal movement of nimbus at a fast rate

By downsizing both Dual Polarimetric Doppler Weather Radar and Single Polarimetric Doppler Weather (July 6, 2013, 19:03 to 19:05) ▲ (August 6, 2013, 18:30 to 18:59) Radar, FURUNO makes remarkable reduction on the deployment cost a possibility. Also, it has become On CAPPI observation, horizontal cross-section scans of a cumulonimbusX-band are conducted Doppler WeatherOn RHI observation, Radar verticalis indispensable cross-section scans for of a cumulonimbuslocalised By downsizing both Dual Polarimetric Doppler Weather Radar and Single Polarimetric Doppler Weather Straightforward interface with power supply cable and LAN cable for data communications Combining the two types of Weather Radar, FURUNO delivers “Multi-Radar System” capable of conducting On CAPPI observation, horizontal cross-section scans of a cumulonimbus are conducted On RHI observation, vertical cross-section scans of a cumulonimbus easier to create “Multi-Radar System” by combining both Radar units. at the equal altitudes. The altitude of a developed cumulonimbus topweather may exceed forecasting10 km. are toconducted, materialise hence easily better grasping safety development in statusthe of a Radar, FURUNO makes remarkable reduction on the deployment cost a possibility. Also, it has become Precipitation can be observed at higher altitude in a greatly developed cumulonimbus. cumulonimbus. This case example clearly shows the active real-timeeasier to 3D create monitoring “Multi-Radar of meteorological System” by combining phenomena both at Radara modest units. investment. at the equal altitudes. The altitude of a developed cumulonimbus top may exceed 10 km. are conducted, hence easily grasping development status of a High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” Precipitation can be observed at higher altitude in a greatly developed cumulonimbus. cumulonimbus. This case example clearly shows the active society where the impactup-and-down arising movement from of nimbus. the meteorological High spatiotemporal resolution 3D monitoring of meteorological phenomena by “Multi-Radar System” makes possible the provision of precautious information about prospective sediment disasters as well as * as of June 2013 (Dual Polarimetric Doppler Weather Radar) SPECIFICATIONS up-and-down movement of nimbus. makes possible the provision of precautious information about prospective sediment disasters as well as information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. disasters can be diminished. Model Name WR-2100 WR-50 Doppler velocity observation information about evacuation routes, shelter location, etc., in case of foreseen rainstorms in real-time. Antenna Polarity Dual polarimetric (Vertical and Horizontal), simultaneously transmitted/received Horizontal Doppler Weather Radar System *The map data used in this page has been provided through Digital Japan Web System of Geospatial Information Authority of Japan. DopplerOperating Frequency velocity9 observationGHz band 9GHz band *The terrain elevation data of the background has been obtained from "Shuttle Radar Topography Mission (SRTM)", conducted by Jet Propulsion Laboratory, the US. by the WR-2100 and the WR-50 *The map data used in this page has been provided through Digital Japan Web System of Geospatial Information Authority of Japan. Beam Width 2.7 degrees (both horizontal and vertical beams) 5.0 degrees *The terrain elevation data of the background has been obtained from "Shuttle Radar Topography Mission (SRTM)", conducted by Jet Propulsion Laboratory, the US. byPeak the Output WR-2100 Power and the100 WR-50 W (both horizontal and vertical beams) 50 W -Solution for meteorological monitoring and analysis - Suitable for monitoring nimbus movement velocity and wind field. Vertical Scan Angle -2 to 90 degrees (adjustable) -2 to 90 degrees (adjustable) System Configuration SuitableAntenna Rotationfor monitoring Speed nimbus16 rpm max. movement (adjustable) velocity and wind eld. 16 rpm max. (adjustable) System Con guration Maximum Range Approx. 30 km Approx. 30 km On Doppler observation, by monitoring Doppler velocity Scan Modes PPI, CAPPI, RHI (Sector Scan available) PPI, CAPPI WR-2100 WR-50 On Doppler observation, by monitoring Doppler velocity of the nimbus, moving velocity of the nimbus, namely, WR-2100 WR-50 Data Processing Unit Externally arranged Incorporated wind speed and direction, can be computed. In this Output Data Reflectivity factor Zh (dBZ), Doppler velocity V (m/s), Doppler velocity width W Reflectivityof the factornimbus, Zh (dBZ),moving Doppler velocity velocity of the V nimbus, (m/s), namely, Signal Processing Unit Radar Unit Radar Unit example, warm colors indicate the winds that move (m/s), Cross polarization difference phase φdp (deg), Specific differential phase Rainfallwind intensity speed R and (mm/h) direction, can be computed. In this WR-2100-DP WR-50-RDU WR-50-RDU Signal Processing Unit Radar Unit Radar Unit KDP (deg/km), Correlation coefficient between two polarizations ρHV, example, warm colors indicate the winds that that away from the Radar antenna, while cold colours WR-2100-DP WR-50-RDU WR-50-RDU Differential reflectivity factor ZDR, Rainfall intensity R (mm/h) move away from the Radar antenna, while cold colours Antenna Unit indicate the winds that move towards the Radar Data Correction Distance attenuation, Rain attenuation, Excessive Doppler velocity, Distance attenuation, Rain attenuation, Excessive Doppler velocity, Soaring needs for Weather Radar that stem indicate the winds that move towards the Radar WR-2100-ATU Display Unit Display Unit Display Unit antenna. The arrow lengths and direction indicate the Antenna Unit Suppression of signal returns from land, Clutter suppression Suppression of signal returns from land, Clutter suppression WR-2100-ATU Communication Port - LAN 100Base-TX×1portantenna. The arrow lengths and direction indicate the WR-2100-DPU WR-50-DPU WR-50-DPU from intensifying extreme weather wind speed and direction, respectively. Display Unit Display Unit Display Unit Power Supply 100-240 VAC, Single Phase, 50/60 Hz 100-240 VAC, Single Phase, 50/60 Hz One of the smallest WR-2100-DPU WR-50-DPU WR-50-DPU wind speed and direction, respectively. A number of arguments on the global scale as to how to tackle problems Power Consumption 650 W max 300 W max and lightest arising from extreme weather, such as short localised rainstorms, tornados Compact Dual Polarimetric X-band Compact X-band PC Internet and other adverse phenomena, have been taking place recently. Subsequently, Compact X-band Doppler Weather Radar ø1086 Doppler Weather Radar PC Internet WR-2100 WR-50 urgent(December needs 6, have 2013, been 10:00) recognised for the solutionDetailed of nimbuslocalised movement weather and velocity Doppler Weather Radar 65 kg 144 lb 28 kg 62 lb (December 6, 2013, 10:00) Detailed nimbus movement and velocity forecasting as part of social infrastructure so as to protect human lives and Image of “Multi-Radar System” Model: WR-50 assets from unexpected natural disasters, i.e., river oods, landslides, etc., CompactImage Dual Polarimetric of “Multi-Radar X-band System” PPI (Plan Position Indicator) observation Approximately 30km hence delivering better safety and peace of mind to society. Doppler Weather Radar Approximately 30km PPI (Plan Position Indicator) observation by the WR-2100 and the WR-50 1024 by the WR-2100 and the WR-50 810 Monitoring is to be conducted at a fixated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. Model: WR-2100 Dual Polarimetric Doppler Weather Radar to Monitoring is to be conducted at a xated elevation angle, suitable for rainfall amount on the ground and low-level wind shear observation. The antenna is rotated while fixing its 76 contribute to prediction of occurrence of rainstorms elevation angle. PPI observation at low 204 The antenna is rotated while xing its elevation angle generates rainfall amount on Compact Dual Polarimetric X-band Compact X-band elevation angle.ø602 PPI observation30 at low Dual Polarimetric Doppler Weather Radar simultaneously transmits and elevation angle generates rainfall amount on the ground. Also, when the rainfall amount Doppler Weather Radar WR-2100 Doppler Weather Radar WR-50 receives horizontally- and vertically-polarised radio waves. It is capable of data is accumulated for the duration of 1 the ground. Also, when the rainfall amount data is accumulated for the duration of 1 computing the movement velocity of nimbus, as can be obtained from Single hour, accumulated rainfall amount for 1 hour With ultra high de nition spatiotemporal resolution capability, the WR-2100 The WR-50 detects the nimbus and tracks its movement. can be calculated. Also, by analysing the hour, accumulated rainfall amount for 1 hour Polarimetric Doppler Weather Radar using horizontally-polarised radio waves, 3 mm 4 mm 5 mm Dual Polarimetric Doppler Weather Radar grasps omni-directional precipitation Its compact unit facilitates ease of installation. Doppler velocity obtained by PPI observation can be calculated. Also, by analysing the as well as precise precipitation intensity. intensity in 50-metre-mesh in six-second-intervals. Also, the WR-2100 Doppler velocity obtained by PPI observation Compact Dual Polarimetric X-band at low elevation angle, low-level wind shear 13103SK Printed in Japan When combined with Dual Polarimetric X-band Doppler FURUNO ELECTRIC CO., LTD. FURUNO ESPAÑA S.A. FURUNO FINLAND OY FURUNO DEUTSCHLAND GmbHat low elevation angle, low-level wind shear Doppler Weather Radar can be obtained. monitors the development process, three-dimensional structure as well as Nishinomiya, Hyogo, Japan Madrid, Spain Espoo, Finland Rellingen, Germany Catalogue No. R-203 Shape of precipitation particles is horizontally-long oval, due to the effect from Weather Radar, “Multi-Radar System” can be constructed www.furuno.com www.furuno.es www.furuno. www.furuno.de can be obtained. Model: WR-2100 movement of a cumulonimbus, which causes rainstorms in order to predict FURUNO U.S.A., INC. FURUNO DANMARK A/S FURUNO POLSKA Sp. Z o.o. FURUNO HELLAS S.A. Compact X-band atmosphere and gravity. Using these characteristics, Dual Polarimetric Doppler *The map data used in this page has been provided at modest cost, which enables comprehensive, real-time Camas, Washington, U.S.A. Hvidovre, Denmark Gdynia, Poland Piraeus, Greece Doppler Weather Radar through Digital Japan Web System of Geospatial their development. Moreover, the WR-2100 has been downsized during its www.furunousa.com www.furuno.dk www.furuno.pl www.furuno.gr *The map data used in this page has been provided meteorological monitoring. ( ) Model: WR-50 Compact Dual Polarimetric X-band Doppler Weather Radar Weather Radar obtains diameters of precipitation particles to compute precise 6 mm Information Authority7 mm of Japan. 8 mm development phase to the extent that can be classi ed as one of the smallest FURUNO UK LIMITED FURUNO NORGE A/S FURUNO EURUS LLC FURUNO (CYPRUS) LTD through Digital Japan Web System of Geospatial Compact X-band Doppler Weather Radar (Rainfall amount observation / June 26, 2013, 14:00 to 15:00) (Precipitation intensity observation / November 13, 2012, 17:26) Compact Dual Polarimetric X-band Doppler Weather Radar Havant, Hampshire, U.K. Ålesund, Norway St. Petersburg, Russian Federation Limassol, Cyprus precipitation intensity. www.furuno.co.uk(Rainfall amount observation / Junewww.furuno.no 26, 2013, 14:00 to 15:00) www.furuno.com.ru(Precipitation intensity observationwww.furuno.com.cy / November 13, 2012, 17:26) Information Authority of Japan. Compactand X-band lightest Doppler Dual Weather Polarimetric Radar Doppler Weather Radar available in the market. FURUNO FRANCE S.A.S. FURUNO SVERIGE AB RICO (PTE) LTD FURUNO KOREA CO., LTD. www.furuno.com Bordeaux-Mérignac, France Västra Frölunda, Sweden Singapore Busan, Korea www.furuno.fr www.furuno.se www.rico.com.sg Model: Radar Doppler Weather Compact DualPolarimetricX-band Weather Radaravailable inthemarket* Classi ed asoneofthesmallestandlightest * asofJune2013(DualPolarimetricDopplerWeather Radar) real-time 3Dmonitoringof meteorological phenomenaatamodestinvestment. Combining thetwotypesofWeather Radar, FURUNOdelivers“Multi-RadarSystem”capableofconducting Weather Radaravailableinthemarket. phase totheextentthatcanbeclassi edasoneofsmallestandlightestDualPolarimetricDoppler localised rainstormscanbepredicted. Moreover, theWR-2100hasbeendownsizedduringdevelopment structure aswellmovement ofacumulonimbus,whichcausesprecipitation, thedevelopmentofshort By conductinghighspatiotemporalresolution monitoringofthedevelopmentprocess, three-dimensional Weather Radargraspsomni-directional precipitation intensityin50-metre-mesh insix-second-intervals. With ultrahighde nitionspatiotemporalresolution capability, theWR-2100DualPolarimetricDoppler Doppler Weather RadarWR-2100andDopplerWeather RadarWR-50. theleadingmarketshareFURUNO, whichhasearned inmarineRadar, provides DualPolarimetricX-band and lightest DualPolarimetric Doppler Weather Radar availablein themarket. development phase totheextentthatcanbeclassi ed asoneofthesmallest their development. Moreover, the WR-2100 hasbeendownsized duringits movement ofacumulonimbus, whichcauses rainstormsinordertopredict monitors thedevelopmentprocess, three-dimensional structureaswell intensity in50-metre-meshsix-second-intervals. Also, the WR-2100 Dual PolarimetricDoppler Weather Radargraspsomni-directionalprecipitation With ultrahighde nitionspatiotemporal resolutioncapability, the WR-2100 Doppler Weather RadarWR-2100 Compact DualPolarimetric X-band WR-2100 meteorological monitoring. at modestcost, whichenables comprehensive, real-time Weather Radar, “Multi-Radar System” canbeconstructed When combinedwithDualPolarimetric X-bandDoppler Its compactunitfacilitateseaseof installation. The WR-50 detectsthenimbusandtracks itsmovement. Doppler Weather RadarWR-50 Compact X-band Model: Radar Doppler Weather Compact X-band WR-50 www.furuno.fr Bordeaux-Mérignac, France FURUNO FRANCES.A.S. www.furuno.co.uk Havant, Hampshire,U.K. FURUNO www.furunousa.com Camas, Washington,U.S.A. FURUNO U.S.A.,INC. www.furuno.com Nishinomiya, Hyogo,Japan FURUNO ELECTRICCO.,LTD. SPECIFICATIONS 65 kg144lb WR-2100 Doppler Weather Radar Compact DualPolarimetricX-band Power Consumption Power Supply Communication Port Data Correction Output Data Data Processing Unit Scan Modes Maximum Range Antenna Rotation Speed Scan Angle Vertical Peak OutputPower Beam Width Operating Frequency Antenna Polarity Model Name ( UK ) LIMITED 650 W max 650 W 100-240 VAC, SinglePhase, 50/60Hz - Suppression from ofsignalreturns land,Clutter suppression Distance attenuation, Rain attenuation, Excessive Dopplervelocity, Differential reflectivity factor ZDR,Rainfall intensityR(mm/h) KDP (deg/km),Correlation ρHV, polarizations coefficient two between (m/s), Cross difference polarization phaseφdp(deg),Specific differential phase Reflectivity factor Zh(dBZ),Dopplervelocity V (m/s),Dopplervelocity width W Externally arranged PPI, CAPPI, RHI(Sector Scanavailable) Approx. 30km 16 max. rpm (adjustable) -2 to 90degrees (adjustable) 100 beams) W (bothhorizontal andvertical 2.7 degrees beams) (bothhorizontal andvertical 9 GHzband (VerticalDual polarimetric andHorizontal), simultaneously transmitted/received WR-2100 www.furuno.se Västra Frölunda, Sweden FURUNO SVERIGEAB www.furuno.no Ålesund, Norway FURUNO NORGE A/S www.furuno.dk Hvidovre, Denmark FURUNO DANMARKA/S www.furuno.es Madrid, Spain FURUNO ESPAÑAS.A.

Compact DualPolarimetric X-bandDoppler Weather Radar Compact X-bandDopplerWeather Radar ▲ ▲ ▲ ▲ ▲ ▲ ▲ ▲ ▲ precipitation diameter ofprecipitationparticles aswelldiscriminatingtypesof Straightforward interface withpower supplycableandLANfordatacommunications ofnimbusatafast velocityofnimbusanddetectshorizontalmovement Outputs movement rate Compact, light-weightRadomeantenna Outputs moving velocityofnimbus Outputs moving High-precision, real-timemonitoringofprecipitationintensity Weather Radaravailable inthemarket Classi ed asoneofthesmallestandlightestDualPolarimetric Doppler of shortlocalisedrainstorm, whennetworkedinto “Multi-Radar System” Suitable forlocalisedmeteorologicalmonitoringaswell theverticalstructureofacumulonimbus 3D scantoobserve Outputs dualpolarimetricDopplerinformation weight: 65kg) 1024 204 (rain, snow, etc.) www.rico.com.sg Singapore RICO www.furuno.com.ru St. Petersburg,RussianFederation FURUNO EURUS LLC www.furuno.pl Gdynia, Poland FURUNO POLSKASp.Zo.o. www.furuno. Espoo, Finland FURUNO FINLANDOY ( ø1086 PTE ) LTD (Radome diameter:108cm, Radome (Radome diameter:60cm, Radomeweight:28kg) WR-50 Busan, Korea FURUNO KOREACO.,LTD. www.furuno.com.cy Limassol, Cyprus FURUNO (CYPRUS) LTD www.furuno.gr Piraeus, Greece FURUNO HELLASS.A. www.furuno.de Rellingen, Germany FURUNO DEUTSCHLANDGmbH (Zdr, Kdp) forcomputing 300 W max 300 W 100-240 VAC, SinglePhase, 50/60Hz LAN 100Base-TX×1port Suppression from ofsignalreturns land,Clutter suppression Distance attenuation, Rain attenuation, Excessive Dopplervelocity, Rainfall intensityR(mm/h) Reflectivity factor Zh(dBZ),Dopplervelocity V (m/s), Incorporated PPI, CAPPI Approx. 30km 16 max. rpm (adjustable) -2 to 90degrees (adjustable) 50 W 5.0 degrees 9GHz band Horizontal WR-50 28 kg62lb WR-50 Doppler Weather Radar Compact X-band WR-2100 (mm/h) minivand tothemonitoringlocation. The antennaunitcanbetuckedina Compact andlightweight! ø602 13103SK Printed inJapan Catalogue No. R-203 30 76 810 D -

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