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- W2234291248 abstract "Results of radar observations of thunderstorms that occurred in the western Kanto district on 14 August 1956 are described. It was found that in general the isobronts preceded radar echoes by about 20 km. Detailed observations of an anvil cloud which drifted eastward from the mother thunderstorm were made with PHI scope. Ice particles or snowflakes falling from the anvil top formed trail patterns and a well-defined bright band as in the case of warm-front type precipitation. Downward protuberances or “ stalactites ”, probably caused by the evaporative cooling of snowflakes falling into dry air, were found at the base of the anvil. They extended downward across the bright band and formed streaking rain patterns under the band. Judging from the slope and the movement of rain patterns and the observed variation of raindrop size-distribution with time, the generating sources of the rain patterns may be ascribed to the stalactites. A lowering of the bright band, of about 200 to 300 m, was also found at its leading edge." @default.
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- W2234291248 date "1957-01-01" @default.
- W2234291248 modified "2023-09-25" @default.
- W2234291248 title "Radar Study of a Dissipating Thunderstorm" @default.
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- W2234291248 doi "https://doi.org/10.2467/mripapers1950.8.1_81" @default.
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