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Published byEmil Charles Miller Modified over 9 years ago
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InterPlanetary Scintillation IPS induced Pluripotent Stem cell iPS
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What is the InterPlanetary Scintillation (IPS)? Why is the IPS a useful and powerful tool for space weather forecast?
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Interplanetary Scintillation V & △ Ne
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1964 Discovery of interplanetary scintillation Antony Hewish
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1min
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81.5 MHz 36000 m 2 Large aperture (high gain) antenna Short-time constant receiver
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5 years later after IPS discovery IPS observations were begun in Japan.
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STEL Radiotelescope Array dedicated for IPS Observations Kiso Sugadaira Fuji Toyokawa Data Solar Wind Speed Scintillation level (g-value) Frequency 327MHz Aperture Size = ~ 2000 or ~ 3400 ㎡
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STEL IPS Antennas as Viewed in Google Earth Fuji IPS Telescope (FIT)Kiso IPS Telescope (KIT)
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Toyokawa Observatory SWIFT
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Solar Wind Imaging Facility at Toyokawa 327 MHz EW40m×NS106m
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a z Fresnel filter E Radio source weight
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Radio source size E weight Radio source z a
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Solar wind electron distribution ★ E E Sun weight Radio source
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Line of sight less weighted by Fresnel filter and lower SW density less weighted by radio source size effect and lower SW density Highest SW density
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Fresnel filter z o =2πa 2 /λ Radio source a/z o >θ z o =1 AU =1.5×10 8 km λ=1 m ⇒ a=150 km θ<0.2 arcsec
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after Coles (1978) IPS vs. in situ
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cross-correlation functions
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Heliocentric Distance (Rs)Scintillation index
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It can observe the near Sun region. It has wide spatial coverage of 3D space. Interplanetary Scintillation It can observe high latitude regions. It can observe vast space in a short time. Complementary observations to spacecraft
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Major issues on solar wind
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Complementary to spacecraft measurements
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Ulysses First and only one Solar polar orbiter
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bimodal Velocity gradient NS asymmetry
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V B Plasma density distribution, IPS diffraction pattern
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cross-correlation functions
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VLA
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