首页 | 本学科首页   官方微博 | 高级检索  
     检索      

四川省典型区域滑坡、泥石流致灾临界雨量阈值确定方法
引用本文:刘海知,马振峰,范广洲.四川省典型区域滑坡、泥石流致灾临界雨量阈值确定方法[J].水土保持通报,2017,37(4):126-131,224.
作者姓名:刘海知  马振峰  范广洲
作者单位:1. 国家气象中心,北京,100081;2. 四川省气候中心,四川成都,610072;3. 成都信息工程大学大气科学学院,四川成都,610225
基金项目:国家自然科学基金项目“华西秋雨年际变化规律及其形成机理研究”(41275097);四川省科技支撑计划项目(15C0098)
摘    要:目的]确定四川省滑坡泥石流典型区域各个子区最关键的降雨因子,建立典型区域各子区临界阈值模型,为该区对滑坡、泥石流灾害进行有效预报提供科学依据.方法]利用1999 2014年四川滑坡泥石流灾情资料,确定出滑坡、泥石流的典型区域,根据典型区域各个子区的气候和下垫面条件,比较不同降雨因子组合的阈值模型,得到各子区最关键的降雨因子,建立典型区域各子区临界阈值模型.结果]平均降雨强度和峰值降雨强度是典型区域滑坡、泥石流阈值模型中的重要指标;诱发雨量多作为滑坡典型区域致灾临界阈值模型雨量指标,激发雨量只作为泥石流典型区域致灾临界阈值模型雨量指标;有效雨量可以在滑坡、泥石流典型区域值模型中应用.典型区域多采用多因子预报模型,只有汶川震区采用单因子预报模型,其临界阈值在震后呈现上升趋势.结论]不同降雨参数对诱发滑坡泥石流灾害的作用不同,典型区域中各子区建立的预报模型及得出的临界阈值也不同.多因子预报模型考虑了多种降雨参数,比单因子模型更客观.

关 键 词:滑坡  泥石流  典型区域  降雨参数  阈值模型
收稿时间:2016/9/30 0:00:00
修稿时间:2016/12/12 0:00:00

Methods of Determining Rainfall Thresholds of Landslides and Debris Flows in Typical Region in Sichuan Province
LIU Haizhi,MA Zhenfeng and FAN Guangzhou.Methods of Determining Rainfall Thresholds of Landslides and Debris Flows in Typical Region in Sichuan Province[J].Bulletin of Soil and Water Conservation,2017,37(4):126-131,224.
Authors:LIU Haizhi  MA Zhenfeng and FAN Guangzhou
Institution:National Meteorological Centre, Beijing 100081, China,Sichuan Climat Center, Chengdu, Sichuan 610072, China and Atmospheric Sciences College, Chengdu University of Information Technology, Chengdu, Sichuan 610225, China
Abstract:Objective] We chose the most significant rainfall indicators of landslides and debris flows in typical regions and built a critical threshold model for each sub-region in typical regions to provide a scientific basis for effective prediction of landslide and debris flows.Methods] This study collected Sichuan''s geological disaster cases occurred in 1999-2014, to define the typical regions of landslides and debris flows in Sichuan Province. We compared the threshold models that are made up of different rainfall indicators in each typical region to construct our rainfall threshold models.Results] Average rainfall intensity and maximum rainfall intensity are used frequently as significant parameters in threshold models of landslides and debris flows in typical regions. Indirect rainfall is a precipitation indicator of landslides in typical region generally, direct rainfall is a precipitation indicator of debris flows just in typical region generally. Effective rainfall was adopted to the precipitation indicator both of landslides and debris flow threshold models in typical regions. Model with double factors were applied to most of typical regions of landslides and debris flows. Model with one factor was just applied to Wenchuan earthquake-stricken area, the critical threshold gradually raised from Wenchuan earthquake.Conclusion] Different rainfall factor has different effect on disasters, each typical region has its own optimum rainfall threshold model. Model with double factors is more objective than those with just one factor, as they contain more rainfall factors.
Keywords:landslides  debris flows  typical regions  rainfall parameters  threshold modes
本文献已被 万方数据 等数据库收录!
点击此处可从《水土保持通报》浏览原始摘要信息
点击此处可从《水土保持通报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号