Modelling floods and damage assessment using GIS
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1 HydroGIS 96: Application of Geographic Information Systems in Hydrology and Water Resources Management (Proceedings of the Vienna Conference, April 1996). IAHS Publ. no. 235, Modelling floods and damage assessment using GIS TINEKE DE JONGE, MATTHIJS KOK Delft Hydraulics, Rivers, Navigation and Structures Division, PO Box 152, 83 AD Emmeloord, The Netherlands MARTEN HOGEWEG Delft Hydraulics, Centre for Software Development, PO Box 152, 83 AD Emmeloord, The Netherlands Abstract River flooding can have a severe impact on society. To reduce the potential damage in the future, structural measures, such as increasing the storage capacity inside or outside the river bed or improving dikes, are essential. To support decision making when choosing and evaluating adequate measures, Delft Hydraulics developed a flood hazard assessment model. The important river related aspects of flooding and managing floods (safety, agriculture, industry, etc.) all have a spatial component. Therefore the GIS package ARC/INFO turned out to be a valuable tool in developing the model. For a series of discharges, the model calculates the flooding depth in the flood plains and the damage assessment. The model was successfully applied to calculate the impacts of potential strategies for the river Meuse in the south of The Netherlands after the flooding of December INTRODUCTION River flooding has a severe impact on society. The many recent floods in The Netherlands started a discussion on responsibility for the consequences of flooding. The civilian population in the river valley should be acquainted with and prepared for flood risk. On the other hand, the public authorities do have a responsibility to take effective measures that reduce the risk of floods. The discussion led to an increasing demand for flood hazard assessment models that will help to analyse the consequences of flooding and the effects of (combinations of) measures. The model presented here focuses on the socioeconomic impacts of flooding, not on the ecological impacts. FLOODING RISK The model was developed from the viewpoint of risk, where risk is defined as the expected damage E(x) multiplied by the probability of occurrence P(x) of an event x: R(x) = E(x)P(x) C 1 ) (e.g. a discharge with a recurrence interval of 1/125 per year) Given the event x, there are two possibilities (Table 1): the risk is accepted and no measures are taken or the risk is too high, indicating that the probability of occurrence
2 3 Tineke De Jonge et al. Table 1 Flooding risk. Probability Damage Accept Measures Low Low Yes Low High No Short term High Low No Long term High High No Short and long term or the expected damage is unacceptable. In the case of unacceptable damage, a disaster plan should exist for taking short term measures in case of flooding. In the case of an unacceptable probability of occurrence, structural measures have to be planned, that improve the flood retaining mechanisms. The flood hazard assessment model described here supports decision making for the long term. THE FLOOD HAZARD ASSESSMENT MODEL General concept and data Damage depends mainly on three factors: - Land use There is a number of land use types such as agriculture, industry, habitation, etc. ; the real estate properties of each land use type are also important, for example the prices of houses, the size of the factory, the average number of persons per house in a region, the number of floors in a building, etc. - Flooding depth Water levels in a river depend on the slope of the river and the discharge. For a given discharge, the water levels are calculated by a hydraulic model. Given the water levels in the river, the elevation of the land and the presence of dikes and other high grounds are factors determining the flood extent. - Spatial distribution The spatial distribution of both land use and flooding depth is important for determining damage. The spatial distribution of the land use types and the land level are supposed to be available as GIS maps. Damage functions have to be defined that depend on these three factors. These functions may differ with location and land use type. All functions should be nondecreasing for increasing discharges; the larger the discharge, the deeper the flooding depth. Within the Flood Hazard Assessment Model, a flood model calculates the flood extent whereas a damage assessment model calculates the expected yearly damage. The user decides on the discharges and strategies (combinations of measures) for which the damage assessment is to be calculated. The results of the calculation are presented to the user as tables, maps and text reports. The concept of the Flood Hazard Assessment Model is depicted in Fig. 1. The flood model Part of the methodology is a one-dimensional hydraulic model of the river. For a given discharge curve at the upstream boundary of the model, the hydraulic model calculates
3 Modelling floods and damage assessment using GIS 31 Damage assessment data supplier Geographic data supplier Damage data Geographic data Geographic data Real estate data supplier Realestai estate data Fig. 1 Conceptual scheme of the Flood Hazard Assessment Model. the water levels at discrete points in the river for each defined time step. The flood model uses the maximum water level during the simulation time in each water level point as input. Within the GIS, the flood plain is divided into influence areas, one per water level point. The flood plain is further divided into elevation polygons, based on a subdivision of the flood plain in elevation levels, generated from a digital terrain model, classified in e.g. 1 cm classes. Dikes and other terrain jumps are added to complete the elevation model. The elevation data and the topology were supplied by GIS as a second input source to the flood model. With the input supplied by the hydraulic model and the GIS, the flood model calculates the flooding. The model starts at the water level points in the river. From there, it searches for neighbouring polygons that are below the water level in the river and are not protected by a dike. As a result, the model calculates the water depth for each polygon in the flood plain and each discharge. Instead of the one-dimensional hydraulic model, a two-dimensional hydraulic model would be a realistic alternative to calculate flooding depths that serve as input to the damage assessment model. The time aspect of filling and emptying the flood plains is not taken into account, since the flood model only uses the maxima of a discharge curve. Therefore, the result of the flooding calculations will be an overview of all areas that will finally be flooded due to the high water. Since the flood hazard assessment model is designed to support decision making on the long term, the flood model suffices. However, if short term decision making had to be supported as well, then the time aspect, especially of filling, would be important; it makes a great difference if the time to evacuate people is limited to only one hour or a full day (24 h).
4 32 Tineke De Jonge et al. The damage assessment model A differentiation into four damage categories is applied, namely public authorities, private persons, industry and agriculture. These categories have been derived from the types of land use. Since the damage depends on land use, flooding depth (land elevation) and spatial distribution (e.g. based on zip code), maps with these themes have to be overlain within the GIS to obtain socalled damage units (Fig. 2). The damage assessment model first checks whether the unit is flooded or not. If flooded, a land use type and location dependent damage function is applied to calculate the damage. The flooding depth must exceed a certain threshold level to cause damage. Given an event x the damage in a unit with land use type L at location S, is calculated by the following function: if d(x) < c LiS (2) ' ~ g(l,s,x)d(x) if d(x) > c L>s where: g(l, S, x) calibration factor for land use type L at location S; d(x) = the flooding depth related to the event x; and c LS = threshold for the flooding depth. REDUCING DAMAGE The scope for applying measures Applying measures aims to reduce damage and to protect people from getting flooded to a level at which the risk of flooding is socially accepted. For example, dikes should be high and strong enough to retain water levels occurring due to a discharge with a recurrence interval of 1/125 per year. However, the profits have to counterbalance the costs of dike improvement. Three types of measure are distinguished: - river engineering measures (e.g. deepening the summer bed or widening the winter bed); - dike improvement and building new dikes; and - prohibition of building in the flood plains: in the last ten years many new activities have been started in flood plains (in The Netherlands) which have caused a lot of flood damage. The river engineering measures lower the water levels at high discharges. Dike improvement measures are applied to be allow dikes to retain the water in extreme situations. Analysis of the flood hazard assessment calculations The flood hazard assessment model serves as a tool to analyse the consequences of potential strategies. The calculated value of the strategies is expressed in the following units:
5 Modelling floods and damage assessment using GIS 33 Contour lines Land use Zip codes Fig. 2 Damage units. Damage units - present value of the reduction in material damage and the remaining material damage (Mf, millions of Dutch Guilders): - regional spread of these values (GIS maps): - spread per municipality of damage suffered by public authorities, private persons, industry and agriculture (GIS maps). The present value of the flood damage related to a strategy i is calculated according to: PV.l^^L (3) where: PV = present value (Mf, millions of Dutch Guilders); B, = flood damage for strategy i (Mf); T= time horizon; R = real discount level (no inflation) (-); rs = real increase in value (-); and t= year. The evaluation of the strategies is based on the expected reduction of water overload. Since the expected damage per year is related to the variation in river discharges, the flood hazard assessment is integrated over the probability of occurrence, with R =.5 and rs =.1. The contribution to the present value of a discharge / is given by: PV = i(p r P i + l )^^25 (4)
6 34 Tineke De longe et al. Table 2 Total damage caused by the River Meuse in December 1993 (Mf is million Dutch Guilders). Damage category Total estimated (Mf) Private sector houses cars 1. caravans 13.5 gardens 1.25 Agricultural industry Industry factories, building companies, trade, service extraction of raw materials 2.71 Institutions 2.58 Public sector and public utilities schools, buildings and terrains 6.55 river infrastructure land infrastructure public utilities 7.3 cleaning, service 1.4 Total Table 3 Damage for a set of discharges, without and with measures (Mf is million Dutch Guilders). Discharge of Meuse at Borgharen (m 3 s" r ) Return time (year) Damage : with present situation (Mf) Damage reduction Resulting damage by dike improvement (Mf) (Mf) (December 1993) where: PV = present value; P i = probability of occurrence of discharge i; S { = calculated damage for discharge i; and 25 = a factor for capitalizing. CASE STUDY The Flood Hazard Assessment model was applied to calculate the impact of several strategies for the river Meuse in the south of The Netherlands. During the flooding of December 1993 large areas along the river Meuse were flooded, causing enormous damage to industries, agriculture, private persons, infrastructure, etc. (Table 2).
7 Modelling floods and damage assessment using GIS 35 ^ 1 1 Houses d December'93 flood Rood after measures M River Fig. 3 GIS maps of flooded area without and with measures. For eight discharges, calculations were made with the flood hazard assessment model (Table 3). The model was applied to the actual situation as well as to a range of strategies. The main set of river engineering measures that were recommended comprised a combination of river engineering and dike improvement measures. The proposed river engineering measures were aimed at widening the summer bed in the southern part of the river and lowering the summer bed in the middle and northern parts. The dike improvement measures consisted of building new dikes around high-risk locations along the entire river and improvement of existing dikes (Fig. 3). The flood model was validated by means of aerial photographs of the December 1993 flood, with a discharge of 312 m 3 s" 1 and flood maps for a 16 m 3 s 4 discharge, during which the river starts flooding. For the calibration of the damage assessment model for the river Meuse, damage data (organized by zip code) of the December 1993 flood were used.
8 36 Tineke De Jonge et al. REFERENCE Delft Hydraulics (1994) Onderzoek Watersnood Maas, Schademodellering (Investigation flooding of the Meuse River, damage modelling), Part 9. Delft Hydraulics, Delft, The Netherlands.
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