Typhoon landslide risk analyzed systematically
The work of civil and environmental engineers has tremendous positive impact on the health and welfare of individuals and communities. One way to expand this impact in the developing world is to transfer technology and engineering expertise globally, while adapting it to local needs. This issue of On Balance looks at such a transfer of technology for hazard and risk assessment to help prevent typhoon-induced landslides, which pose a huge risk for Southeast Asia. Landslides cause thousands of deaths and billions of dollars in property damage each year. In 2006, a landslide destroyed the entire village of Guinsaugon, Philippines, killing most of its 1,857 residents. The mountainous region near Baguio City, Philippines, about 200 kilometers north of Manila, experienced some 65 recorded landslides between 1991 and 2004. Baguio sits 1,500 meters above sea level, has an annual rainfall of 3,648 millimeters, and holds the world record for most rainfall in 24 hours: 1,168 millimeters in July 1911. As a desirable tourist destination, Baguio has become increasingly populous and developed, leaving the area in greater danger of landslides and increasing the human and economic costs when they occur. Blasting for mining, and deforestation from logging and slash-and-burn farming also contribute to the problem, but no system exists for analyzing and managing the landslide risks.
Professor Herbert Einstein of the MIT Department of Civil and Environmental Engineering and graduate student Artessa Saldivar-Sali developed a simple system for determining a landslide risk rating based on commonly available data for a 50-square-kilometer area surrounding Baguio City. Using the area’s landslide history and hazard contributory factors—type of underlying bedrock, slope gradient and vegetation growth—they determined a hazard rating for each slope. They converted that into an overall landslide risk rating by using multipliers based on land use and population.
The researchers concluded that landslide hazard is determined by a combination of two factors: the underlying bedrock and the slope gradient. They found that landslides are less common in areas with limestone bedrock, even though these may be relatively steep. While roughly