Aircraft Traverses in a Growing Mountain Cumulus Cloud

Todd, Clement J.

doi:10.1175/1520-0469(1964)021<0529:atiagm>2.0.co;2

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Fig I Instrumentation Layout Around the Catalina Mountains1

Introduction1

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1973

2020

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Cited by 3 publications

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“…Several observational studies in the desert Southwest have addressed orographic circulations and/or cumulus dynamics (Braham et al 1951;Braham and Draginis 1960;Fujita et al 1962;Todd 1964;Raymond andWilkening 1980,1982;Dye et al 1989;Raymond and Blyth 1989;Blyth and Latham 1993). None achieved CuPIDO's in situ and remote data density and none studied the onset of the first cumulus.…”

Section: Fig I Instrumentation Layout Around the Catalina Mountainsmentioning

confidence: 99%

The Cumulus, Photogrammetric, In Situ, and Doppler Observations Experiment of 2006

Damiani¹,

Zehnder²,

Geerts³

et al. 2008

Bulletin of the American Meteorological Society

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Section: Fig I Instrumentation Layout Around the Catalina Mountainsmentioning

confidence: 99%

The Cumulus, Photogrammetric, In Situ, and Doppler Observations Experiment of 2006

Damiani¹,

Zehnder²,

Geerts³

et al. 2008

Bulletin of the American Meteorological Society

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“…The formation of convective clouds over mountains was studied by observational works (Braham and Dragnis, 1960: Fosberg, 1967: Todd, 1964 and by numerical modelling (Orville, 1965, 1968: Orville and Sloan, 1970 typhoon and the distribution of total rainfall amount from 00 LST to 24 LST on the 5th. Heavy rainfall more than 300mm is found only in the southeastern part in the peninsula.…”

Section: Introductionmentioning

confidence: 99%

Modification of Typhoon 7002 Rainfall by Orographic Effect

Sakakibara

Takeda

1973

Journal of the Meteorological Society of Japan

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A case study of the rainfall during the passage of Typhoon 7002 over the Kii Peninsula is made on the assumption that the rainfall R(x,y,t) at each station (x,y) should be interpreted as k(x,y)*f(x,y,t), where f(x,y,t) is the rainfall which would be caused at the station by the traverse of a disturbance if there were no orographic effect and k(x,y) is the amplification factor of the rainfall which would be dependent upon the topographic features around the station and the direction and strength of prevailing wind. The results of analysis show that the distribution of h(x,y,t) whish is roughly proportional to f(x,y,t) and its behavior have a good correspondence to the distribution of moving radar echoes, while the distribution of R (x, y,t) is considerably controlled by topographic features over the peninsula. Examples of the pattern of k(x,y) and f(x,y,t) over the peninsula are presented.

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