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Qaagi - Book of Why

Causes

Effects

ex - Tropical Cyclone Debbie , 31st March 2017 | Springer for Research & Development(passive) caused byRainfall - induced shallow landslides

seasonal rainfall patterns(passive) strongly influenced byrainfall - induced

increased pore pressures and seepage forces during the periods of intense rainfall(passive) are caused byrainfall induced landslides

Using a small flume , a series of tests has been conductedto causerainfall - induced flowslides

two tropical storms(passive) triggered byRain - induced landslides

cumulative precipitation ranging from 743 to 844 mm in several localities during a 4-day period(passive) were triggered byRainfall - induced landslides

two previous tropical storms , injured or killed several people in the Philippines(passive) triggered byRain - induced landslides

The mechanismleadingto rainfall - induced landslides

due to the rise of pore water pressure within the soil that reduces its normal effective stress(passive) are mainly causedRainfall - induced landslides

the rainfall events(passive) triggered byrainfall - induced landslides

single storms(passive) caused byrainfall - induced landslides

the intesnse rainfall event(passive) triggered byrainfall - induced landslides

reduction of effective stress and(passive) are caused byEEG.2014.47.1.49 Rainfall - induced landslides

expected average damage per hectare and year(passive) caused byexpected average damage per hectare and year

significant damage and fatality worldwidecausesignificant damage and fatality worldwide

in streams and rivers carrying significantly larger sediment loads which produce much larger than normal flood impactsresultsin streams and rivers carrying significantly larger sediment loads which produce much larger than normal flood impacts

the closure of Highway 14 between Paterson and Goldendalecausedthe closure of Highway 14 between Paterson and Goldendale

from different soil failure mechanisms each leading to slope instabilities characterized by varying times and depths of occurrencecan resultfrom different soil failure mechanisms each leading to slope instabilities characterized by varying times and depths of occurrence

T1 - Effect of wetting front suction loss on stability of unsaturated soil slopes(passive) are causedT1 - Effect of wetting front suction loss on stability of unsaturated soil slopes

large increases of flood peaks in the Alpine headwaters(passive) are caused bylarge increases of flood peaks in the Alpine headwaters

rills to form in the soil that was unprotected , while soil under the Curlex blankets was held in placecausedrills to form in the soil that was unprotected , while soil under the Curlex blankets was held in place

75 % cases(passive) triggered by75 % cases

significant damage involving loss of life and propertycausesignificant damage involving loss of life and property

minor damage to infrastructure and residential propertycausingminor damage to infrastructure and residential property

to loss of life and significant damage to private and public properties , transportation systems , etccan leadto loss of life and significant damage to private and public properties , transportation systems , etc

slope failures and reduced the stream carrying capacity , resulting in problematic flooding and property loss for the residents in close proximity to the brookshas causedslope failures and reduced the stream carrying capacity , resulting in problematic flooding and property loss for the residents in close proximity to the brooks

a coastal alluvial fan in eastern Taiwan(passive) caused bya coastal alluvial fan in eastern Taiwan

in Baguio Citytriggeredin Baguio City

rail transport(passive) caused byrail transport

up - slope of the BMP to be evaluatedis createdup - slope of the BMP to be evaluated

fatalities and large economic damagecausefatalities and large economic damage

a considerable damage to societycausea considerable damage to society

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