• DocumentCode
    3222030
  • Title

    Analyses on coupling correlation between landslides and rainfall and application in the early-warning and forecast

  • Author

    Gao, Huaxi

  • Author_Institution
    Sch. of Naval Archit. & Civil Eng., Zhejiang Ocean Univ., Zhoushan, China
  • fYear
    2011
  • fDate
    22-24 April 2011
  • Firstpage
    6432
  • Lastpage
    6436
  • Abstract
    Historical data of rainfall and region landslides in ShenZhen are researched in detail in this paper. And the partial correlation between landslides and rainfall, the correlation between landslides and rainfall intensity, and the correlation between landslide and rainfall season are analyzed. The results show: First, the partial correlation coefficient is highly between landslide action and the two days rainfall, and the sum of one rainfall. It means that the region landslides will appear when the rainfall is up to some numerical value. Second, the correlation between rainstorm and landslide is very intimate, and the correlation coefficient is beyond 0.85, especially the heavy rainstorm and the extraordinary rainstorm. They can straightly make the landslides occur. Third, the occurring time of landslides is correspond to the rainfall season, the more rainfall is, the more landslide number is. In addition, the occurring time of landslides accords with or lags behind rainstorm and heavy rainstorm, but the lagged time is less four days, and the landslides popularly arises at the same day and the second day when the rainstorm takes place.
  • Keywords
    geomorphology; rain; ShenZhen; coupling correlation analyses; early-warning; forecasting; landslides; rainfall; Correlation; Floods; Meteorology; Rocks; Soil; Terrain factors; early-warning and forecast; landslide; partial correlation coefficient; rain;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Electric Technology and Civil Engineering (ICETCE), 2011 International Conference on
  • Conference_Location
    Lushan
  • Print_ISBN
    978-1-4577-0289-1
  • Type

    conf

  • DOI
    10.1109/ICETCE.2011.5774557
  • Filename
    5774557