Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1175/JAS-D-17-0168.1 |
Stratiform Precipitation Processes in Cyclones Passing over a Coastal Mountain Range | |
Zagrodnik, Joseph P.1; McMurdie, Lynn A.1; Houze, Robert A., Jr.1,2 | |
2018-03-01 | |
发表期刊 | JOURNAL OF THE ATMOSPHERIC SCIENCES |
ISSN | 0022-4928 |
EISSN | 1520-0469 |
出版年 | 2018 |
卷号 | 75期号:3页码:983-1004 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | The Olympic Mountains Experiment (OLYMPEX) documented precipitation and drop size distributions (DSDs) in landfalling midlatitude cyclones with gauges and disdrometers located at various distances from the coast and at different elevations on the windward side of the mountain range. Statistics of the drop size and gauge data for the season and case study analysis of a high-rainfall-producing storm of the atmospheric river type show that DSDs during stratiform raining periods exhibit considerable variability in regions of complex terrain. Seasonal statistics show that different relative proportions of drop sizes are present, depending on synoptic and mesoscale conditions, which vary within a single storm. The most frequent DSD regime contains modest concentrations of both small and large drops with synoptic factors near their climatological norms and moderate precipitation enhancement on the lower windward slopes. The heaviest rains are the most strongly enhanced on the lower slope and have DSDs marked by large concentrations of small to medium drops and varying concentrations of large drops. During the heavy-rain period of the case examined here, the low-level flow was onshore and entirely up terrain, the melting level was similar to 2.5 km, and stability moist neutral so that large amounts of small raindrops were produced. At the same time, melting ice particles produced at upper levels contributed varying amounts of large drops to the DSD, depending on the subsynoptic variability of the storm structure. When the low-level flow is directed downslope and offshore, small-drop production at low altitudes is reduced or eliminated. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000429576900016 |
WOS关键词 | RAINDROP SIZE DISTRIBUTION ; OROGRAPHIC PRECIPITATION ; ATMOSPHERIC RIVERS ; MIDLATITUDE CYCLONES ; NORTHERN CALIFORNIA ; RADAR DATA ; MESOSCALE ; RAINFALL ; DISTRIBUTIONS ; MICROPHYSICS |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/29290 |
专题 | 地球科学 |
作者单位 | 1.Univ Washington, Seattle, WA 98195 USA; 2.Pacific Northwest Natl Lab, Richland, WA USA |
推荐引用方式 GB/T 7714 | Zagrodnik, Joseph P.,McMurdie, Lynn A.,Houze, Robert A., Jr.. Stratiform Precipitation Processes in Cyclones Passing over a Coastal Mountain Range[J]. JOURNAL OF THE ATMOSPHERIC SCIENCES,2018,75(3):983-1004. |
APA | Zagrodnik, Joseph P.,McMurdie, Lynn A.,&Houze, Robert A., Jr..(2018).Stratiform Precipitation Processes in Cyclones Passing over a Coastal Mountain Range.JOURNAL OF THE ATMOSPHERIC SCIENCES,75(3),983-1004. |
MLA | Zagrodnik, Joseph P.,et al."Stratiform Precipitation Processes in Cyclones Passing over a Coastal Mountain Range".JOURNAL OF THE ATMOSPHERIC SCIENCES 75.3(2018):983-1004. |
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