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dc.contributor.authorNickerson, E. C.
dc.date.accessioned2017-06-09T17:40:09Z
dc.date.available2017-06-09T17:40:09Z
dc.date.copyright1979/09/01
dc.date.issued1979
dc.identifier.issn0021-8952
dc.identifier.otherams-9759.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233282
dc.description.abstractAn examination of hourly rainfall within areas designated small outside (SO) and large outside (LO) reveals that prior to the introduction of a new seeding device (NEI) in 1975, average peninsular rainfall on seed (S) days outside the Florida Area Cumulus Experiment (FACE) target area was slightly less than rainfall on no-seed (NS) days. However, during the NEI period, average station rainfall within the SO area yields S/NS ratios as high as 3 for the 6 h period following the release of the first flare. Moreover, during the 3 h period prior to the time of the first seed, average SO station rainfall on seed days exceeded the rainfall on no-seed days by approximately 60%. The large S/NS ratios that occurred outside the FACE target area during the NEI period were not associated with anomalously high rainfall on seed days, but rather with anomalously low rainfall on no-seed days. For the SO area, differences between seed and no-seed samples are highly significant, with one-tailed P values as low as 0.001 as determined from a Wilcoxon (Mann-Whitney) test. Natural variability therefore appears to account for statistically significant differences between area-wide rainfall on seed and no-seed days.
dc.publisherAmerican Meteorological Society
dc.titleFACE Rainfall Results: Seeding Effect or Natural Variability?
dc.typeJournal Paper
dc.journal.volume18
dc.journal.issue9
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1979)018<1097:FRRSEO>2.0.CO;2
dc.journal.fristpage1097
dc.journal.lastpage1105
dc.treeJournal of Applied Meteorology:;1979:;volume( 018 ):;issue: 009
dc.contenttypeFulltext


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