1970
DOI: 10.2151/jmsj1965.48.2_103
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Precipitation Bands of Typhoon Vera in 1959 (Part II)

Abstract: A detailed comparison is made between the rainfall distribution over land at intervals of 20 minutes and the radar echoes which were associated with Typhoon Vera in September 1959. Even at this short time scale, the association of the isohyet pattern with the radar echo distribution is not easily seen because the rainfall amount is very much enhanced in the mountain range and the orographic rain is not well detected by radars. An analysis of time changes of the 20-min rainfall amount reveals the existence of z… Show more

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Cited by 10 publications
(1 citation statement)
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“…The impact of topography on landfalling TCs is more significant than roughness variation, especially in mountainous areas (Chang 1982). Observations (Brunt 1968;Hamuro et al 1969) have confirmed that high correlations exist between the areas of maximum rainfall during TC landfall and the mountainous terrain of the region. Brand and Blelloch (1974) found that topographical effects, if not properly accounted for, can cause significant errors in the forecasting of a TCs motion.…”
Section: Introductionmentioning
confidence: 99%
“…The impact of topography on landfalling TCs is more significant than roughness variation, especially in mountainous areas (Chang 1982). Observations (Brunt 1968;Hamuro et al 1969) have confirmed that high correlations exist between the areas of maximum rainfall during TC landfall and the mountainous terrain of the region. Brand and Blelloch (1974) found that topographical effects, if not properly accounted for, can cause significant errors in the forecasting of a TCs motion.…”
Section: Introductionmentioning
confidence: 99%