The Heavy Rain Event of 29 October 2000 in Hana, Maui*
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Abstract On 29 October 2000, the Hana region of Maui received 700 mm of rain in 7 h. Radar analyses revealed that the storm consisted of seven cells that were initiated along the southeast slope of Haleakala volcano. One of these cells survived for nearly 4 h and was responsible for 80% of the volumetric rainout from the storm. The interaction of low-level flow distorted by the island of Hawaii located farther east, the passage of a trough, and the topographic forcing caused by Haleakala volcano were major factors responsible for the evolution of the storm.
2003 ◽
Vol 129
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pp. 495-522
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2013 ◽
Vol 10
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pp. 2767-2790
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2006 ◽
Vol 81
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pp. 187-205
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2020 ◽
Vol 76
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pp. I_201-I_210
2018 ◽
Vol 32
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pp. 598-611
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