| dc.contributor.author | C. R. Chhorn | |
| dc.contributor.author | G. Kim | |
| dc.contributor.author | C. Y. Yune | |
| dc.contributor.author | S. W. Lee | |
| dc.date.accessioned | 2017-05-08T22:30:53Z | |
| dc.date.available | 2017-05-08T22:30:53Z | |
| dc.date.copyright | November 2015 | |
| dc.date.issued | 2015 | |
| dc.identifier.other | 47763494.pdf | |
| dc.identifier.uri | http://yetl.yabesh.ir/yetl/handle/yetl/81851 | |
| dc.description.abstract | Different magnitude of debris flows causes different damages to the surrounding environment. It is important to know its volume in order to be able to be aware of its run-out length and potential damage level. Many researchers have tried to develop regression models for estimating debris flow magnitude, yet they cannot be used in a general context. A research on debris flow in the eastern Italian Alps, for example, a regression equation to determine debris flow magnitude based only on the slope gradient ( | |
| dc.publisher | American Society of Civil Engineers | |
| dc.title | Analysis of the Magnitude of Debris Flows in Korea | |
| dc.type | Journal Paper | |
| dc.journal.volume | 16 | |
| dc.journal.issue | 4 | |
| dc.journal.title | Natural Hazards Review | |
| dc.identifier.doi | 10.1061/(ASCE)NH.1527-6996.0000175 | |
| dc.tree | Natural Hazards Review:;2015:;Volume ( 016 ):;issue: 004 | |
| dc.contenttype | Fulltext | |
