Non-Monotonic Relationships between Return Periods of Precipitation Surface Hazard Intensity

Hazardous surface processes such as floods and mass movements are often induced by a common trigger such as extreme precipitation. The relationship between the intensity of the trigger and the surface hazard is generally assumed to be monotonically increasing (increasing precipitation never decrease...

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Bibliographic Details
Main Authors: Jetten, V.G (Author), van den Bout, B. (Author), van Westen, C.J (Author)
Format: Article
Language:English
Published: MDPI 2022
Subjects:
Online Access:View Fulltext in Publisher
LEADER 02723nam a2200409Ia 4500
001 10.3390-w14091348
008 220706s2022 CNT 000 0 und d
020 |a 20734441 (ISSN) 
245 1 0 |a Non-Monotonic Relationships between Return Periods of Precipitation Surface Hazard Intensity 
260 0 |b MDPI  |c 2022 
856 |z View Fulltext in Publisher  |u https://doi.org/10.3390/w14091348 
520 3 |a Hazardous surface processes such as floods and mass movements are often induced by a common trigger such as extreme precipitation. The relationship between the intensity of the trigger and the surface hazard is generally assumed to be monotonically increasing (increasing precipitation never decreases hazard intensity). The validity of this assumption of complex multi-hazard events has not been thoroughly investigated. In this research, the relationship between cumulative precipitation and hazard intensity was investigated by a simulation of 50 return period precipitation events on the Carribean island Dominica. Here, several tropical hurricanes have induced events with (flash) floods, slope failure, debris flows and landslides within the past decades. Results show that complex multi-hazard interactions break the common assumption for the relationship between trigger and hazard intensity. In particular, landslide dam formation and mass movement dilution result in hazard intensities that are not a one-to-one increasing function of trigger intensity. Spatial variability in this behavior is quantified using a rank-order correlation coefficient between trigger return period and hazard return period. Since trigger and hazard return periods are, in the study case, not approximately equal, the hazard for a specific location can not be classified based on trigger return period. This has implications for risk calculation and decision making related to disaster risk reduction. © 2022 by the authors. Licensee MDPI, Basel, Switzerland. 
650 0 4 |a Cumulative precipitation 
650 0 4 |a Decision making 
650 0 4 |a Extreme precipitation 
650 0 4 |a floods 
650 0 4 |a Floods 
650 0 4 |a Hazards 
650 0 4 |a Hurricanes 
650 0 4 |a Landslides 
650 0 4 |a Mass movement 
650 0 4 |a Monotonics 
650 0 4 |a Multi-hazards 
650 0 4 |a Natural hazard 
650 0 4 |a natural hazards 
650 0 4 |a Precipitation (meteorology) 
650 0 4 |a Return periods 
650 0 4 |a Surface hazards 
650 0 4 |a Surface process 
650 0 4 |a tropical cyclone 
650 0 4 |a Tropical cyclone 
650 0 4 |a Tropical cyclone 
650 0 4 |a Tropics 
700 1 0 |a Jetten, V.G.  |e author 
700 1 0 |a van den Bout, B.  |e author 
700 1 0 |a van Westen, C.J.  |e author 
773 |t Water (Switzerland)