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Articles

How much does an extreme rainfall event cost? Material damage and relationships between insurance, rainfall, land cover and urban flooding

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Pages 673-689 | Received 24 May 2018, Accepted 19 Jan 2019, Published online: 18 Apr 2019

Figures & data

Table 1. Statistical data of the municipalities in the LMA. Built-up areas (2007); buildings, dwellings and inhabitants (2011).

Figure 1. Location of the study area, showing the raingauge locations and the municipalities of the Lisbon Municipal Area (LMA).

Figure 1. Location of the study area, showing the raingauge locations and the municipalities of the Lisbon Municipal Area (LMA).

Table 2. Definitions of the concepts used in this research.

Figure 2. Large-scale atmospheric circulation and dynamic features of the extreme event of 18 February 2008: (a) 500 mb geopotential heights (dam), (b) sea-level pressure (mb), (c) total column water vapour (mm), (d) convective available potential energy (J kg−1). All panels refer to 12:00 h UTC on 17 February 2008. Source of reanalysis data: www.ecmwf.int.

Figure 2. Large-scale atmospheric circulation and dynamic features of the extreme event of 18 February 2008: (a) 500 mb geopotential heights (dam), (b) sea-level pressure (mb), (c) total column water vapour (mm), (d) convective available potential energy (J kg−1). All panels refer to 12:00 h UTC on 17 February 2008. Source of reanalysis data: www.ecmwf.int.

Figure 3. Spatial representation of the 24-h maximum rainfall during the 2008 event in the LMA.

Figure 3. Spatial representation of the 24-h maximum rainfall during the 2008 event in the LMA.

Figure 4. High-magnitude rainfall in the LMA at the São Julião do Tojal raingauge: (a) annual maximum daily rainfall for the period 1938/39–2011/12 and (b) IDF curves for several return periods and for the 1967, 1983 and 2008 rainfall events.

Figure 4. High-magnitude rainfall in the LMA at the São Julião do Tojal raingauge: (a) annual maximum daily rainfall for the period 1938/39–2011/12 and (b) IDF curves for several return periods and for the 1967, 1983 and 2008 rainfall events.

Figure 5. Temporal evolution of APS claims and payouts in the LMA (2000–2011): (a) number of APS claims and payouts, (b) accumulated APS claims and payouts.

Figure 5. Temporal evolution of APS claims and payouts in the LMA (2000–2011): (a) number of APS claims and payouts, (b) accumulated APS claims and payouts.

Figure 6. Annual and monthly values of insurance data in the LMA (2000–2011) and the weight of the 2008 event: (a) number of APS claims per year, (b) payouts per year, (c) APS claims per month and (d) payouts per month. Note: the APS database ends in October 2011. This year only has records for 10 months; November and December values are therefore the result of accumulated values of only 11 years of records, unlike the other months (12 years).

Figure 6. Annual and monthly values of insurance data in the LMA (2000–2011) and the weight of the 2008 event: (a) number of APS claims per year, (b) payouts per year, (c) APS claims per month and (d) payouts per month. Note: the APS database ends in October 2011. This year only has records for 10 months; November and December values are therefore the result of accumulated values of only 11 years of records, unlike the other months (12 years).

Figure 7. Spatial distribution of the total APS claims (2000–2011) and those resulting from the 2008 event in the LMA.

Figure 7. Spatial distribution of the total APS claims (2000–2011) and those resulting from the 2008 event in the LMA.

Figure 8. Rainfall vs APS claims for each APS event at 1, 3, 6, 12 and 24 hours on the SJT raingauge. Note: only the APS events with APS claims located within a 10 km radius of the SJT raingauge are represented.

Figure 8. Rainfall vs APS claims for each APS event at 1, 3, 6, 12 and 24 hours on the SJT raingauge. Note: only the APS events with APS claims located within a 10 km radius of the SJT raingauge are represented.

Figure 9. Temporal evolution of four rainfall events that caused a different number of APS claims in a 10 km radius of the SJT raingauge.

Figure 9. Temporal evolution of four rainfall events that caused a different number of APS claims in a 10 km radius of the SJT raingauge.

Figure 10. Likelihood levels of flooding for the SJT raingauge.

Figure 10. Likelihood levels of flooding for the SJT raingauge.

Table 3. Correlation matrix between land use/cover, building features and insurance data for the LMA municipalities. LIN: linear regression; LOG: logarithmic regression.

Figure 11. Scatter chart between the APS claims per built-up km2 and the maximum rainfall in 24 h for the 2008 event.

Figure 11. Scatter chart between the APS claims per built-up km2 and the maximum rainfall in 24 h for the 2008 event.

Figure 12. Material damage by type of flooding in the LMA and in the Lisbon municipality: (a) and (d) APS claims, (b) and (e) payouts, and (c) and (f) payouts per APS claim. (a), (b) and (c) correspond to the LMA, and (d), (e) and (f) to the Lisbon municipality.

Figure 12. Material damage by type of flooding in the LMA and in the Lisbon municipality: (a) and (d) APS claims, (b) and (e) payouts, and (c) and (f) payouts per APS claim. (a), (b) and (c) correspond to the LMA, and (d), (e) and (f) to the Lisbon municipality.

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