| dc.contributor.author | Hindman, Edward E. | |
| dc.date.accessioned | 2017-06-09T14:00:58Z | |
| dc.date.available | 2017-06-09T14:00:58Z | |
| dc.date.copyright | 1986/02/01 | |
| dc.date.issued | 1986 | |
| dc.identifier.issn | 0733-3021 | |
| dc.identifier.other | ams-10953.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4146127 | |
| dc.description.abstract | The flow of moisture through a ?slab? of air, upwind and over the Park Range in northwest Colorado, was estimated from wintertime meteorological measurements. On average, 6?14% of the inflow moisture precipitated onto the barrier (86 to 94% flowed over the barrier). Because such a small amount of the moisture precipitates, snowfall augmentation activities on the upwind Park Range barrier should not significantly affect the moisture reaching the downwind Front Range barrier. | |
| dc.publisher | American Meteorological Society | |
| dc.title | An Atmospheric Water Balance over a Mountain Barrier | |
| dc.type | Journal Paper | |
| dc.journal.volume | 25 | |
| dc.journal.issue | 2 | |
| dc.journal.title | Journal of Climate and Applied Meteorology | |
| dc.identifier.doi | 10.1175/1520-0450(1986)025<0180:AAWBOA>2.0.CO;2 | |
| dc.journal.fristpage | 180 | |
| dc.journal.lastpage | 183 | |
| dc.tree | Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 002 | |
| dc.contenttype | Fulltext | |
