| contributor author | Lyman, Ryan E. | |
| contributor author | Schroeder, Thomas A. | |
| contributor author | Barnes, Gary M. | |
| date accessioned | 2017-06-09T17:34:59Z | |
| date available | 2017-06-09T17:34:59Z | |
| date copyright | 2005/08/01 | |
| date issued | 2005 | |
| identifier issn | 0882-8156 | |
| identifier other | ams-87553.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4231235 | |
| description 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. | |
| publisher | American Meteorological Society | |
| title | The Heavy Rain Event of 29 October 2000 in Hana, Maui | |
| type | Journal Paper | |
| journal volume | 20 | |
| journal issue | 4 | |
| journal title | Weather and Forecasting | |
| identifier doi | 10.1175/WAF868.1 | |
| journal fristpage | 397 | |
| journal lastpage | 414 | |
| tree | Weather and Forecasting:;2005:;volume( 020 ):;issue: 004 | |
| contenttype | Fulltext | |
