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Published byLeon Cox Modified over 9 years ago
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The Tokyo First snow observed by MRR Tomoki Koshida Research fellow of OKI/KANAE lab 1/11’05
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Today’s topics What defines a hydrometer? Synoptic condition Surface condition Observation results Discussion
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Specification of MRR Transmit frequency24.1GHz Transmit power50mW Receive-transmitter antennaOffset parabolic,0.6m diameter Beam width2degree(35m at 1km) ModulationFMCW Height resolution10 – 200m Averaging time10 – 3600s Height range29range gate (e.g..50-1500m at 50m-res) Observation location 35 39’38”N 139 41’6”E
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Snow falling scene 2004/12/29 rain => snow 2004/12/31 snow => rain
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What defines a hydrometer? *hydrometer is a particle of water in the air. For example, cloud particle, rain, snow, hail and so on. Ice melts to water at the degree of 0.
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Example of threshold snowflake Rain snow diagram sleet rain Relative humidity Temperature02-3
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Example
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Weather map surface
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Weather map upper level
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Surface condition Time series of T and RH Wet sleet period Dry sleet period
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Vertical profile of T 2004/ 12/29 9JST
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MRR observation Z(2004 12/29) TH cross section
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MRR observation W(2004 12/29)
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Bright band
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Reflectivity index
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Image of Snow observation
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Vertical profile of MRR Wet sleetdry sleet
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Doppler spectrum 2004/12/29 wet Spectrum graph Formation ice phase Accrete phase Shrink phase
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Doppler spectrum 2004/12/29 dry Formation ice phase melting phase Shrink phase
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Limit of MRR observation TH of failure time
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Picture of accumulating snow
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Micro wave absorption A Chinese bean-jam bun will be hotter in contents than shells.
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Conclusion 1 MRR observed snow & melting snow The result is consistent in previous study And more, precise structure of bright band given Too much snow and melting water prevents us from snow observation.
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Weather map surface 2004/ 12/31 15JST Synoptic situation
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Weather map upper level 2004 12/31 21JST
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Surface condition 2004/12/31 Dry snow Rain
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TH diagram of Z 2004/12/31 TH Vertical profile Z spectrum Speculation
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TH diagram of W 2004/12/31
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Vertical profile of Z,W 2004/12/31 snow rain
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Vertical profile of T 2004/ 12/31 15JST GPV initial
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Vertical profile of T,RH 2004/ 12/31 15JST GPV initial 0%50%
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Doppler spectrum 2004/12/31 snow snow Formation ice phase Shrink ice phase
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Doppler spectrum 2004/12/31 rain rain Formation ice phase Melting ice Shrink but growth Rain
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Z spectrum 2004/12/31
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conclusion MRR observed Doppler spectrum The spectrum will consist in qualitative analysis MRR could investigate precipitation system
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