| contributor author | Herbert B. Osborn | |
| contributor author | Kenneth G. Renard | |
| date accessioned | 2017-05-08T20:46:52Z | |
| date available | 2017-05-08T20:46:52Z | |
| date copyright | February 1988 | |
| date issued | 1988 | |
| identifier other | %28asce%290733-9437%281988%29114%3A1%28195%29.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl/handle/yetl/26946 | |
| description abstract | Small watershed storm runoff in the southwestern United States is dominated by intense, short-duration convective rains of limited areal extent. Most commonly, flood peak estimates are based on rainfall predictions found in the National Oceanic and Atmospheric Administration (NOAA) Atlas 2, a precipitation-frequency atlas for the Western United States. Records of short-duration rainfall (5 to 30 min. duration) from a dense network of recording rain gauges in southeastern Arizona indicate that flood peaks based on NOAA Atlas 2 for less frequent events (50-yr. and 100-yr. frequencies) for small watersheds are underestimated. | |
| publisher | American Society of Civil Engineers | |
| title | Rainfall Intensities for Southeastern Arizona | |
| type | Journal Paper | |
| journal volume | 114 | |
| journal issue | 1 | |
| journal title | Journal of Irrigation and Drainage Engineering | |
| identifier doi | 10.1061/(ASCE)0733-9437(1988)114:1(195) | |
| tree | Journal of Irrigation and Drainage Engineering:;1988:;Volume ( 114 ):;issue: 001 | |
| contenttype | Fulltext | |
