Measures Also Significant Factors of Flood Disaster Reduction

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Non-Structual Measures Also Significant Factors of Flood Disaster Reduction Babiaková Gabriela, Leškov ková Danica Slovak Hydrometeorological Institute, Bratislava Hydrological Forecasts and Warning Department 1

Floods are natural phenomena which can not be prevented sufficiently Natural condition of Slovakia are rather complex. Narrow valleys result in a relatively short lag time and create favourable conditions for floods as well, as spatial flash floods. 2

The Slovak Republic Area 49 036 km 2 Over 300 m a.s.l. 60% Over 1000 m a.s.l. 5.4% 5,4% The lowest point 94 m a.s.l. The highest poit 2655 m a.s.l. Agricultural land 50% Forest land 41% Water area 2% Built-up Build-up areas 3% Area mean temperature 7,5 7.5 ºC º C Area mean precipitation total 745 mm 3

There are approximately 2,300 small catchments areas in range 5 50 km2 with a large potential risk for flooding, especially with respect to this type of flood Between 1996 and 2002, Slovakia suffered over 80 major floods causing damage, including catastrophic flash floods in the central and northern part of the country The majority of them have resulted in injuries to o people, the displacement of hundreds of people and enormous economic losses Small catchments recorded 77 flash floods between 1997 and 2002 4

5

The floods that have frequently occurred on Slovak territory in recent years include the following: floods from extensive rainfall regional floods connected with snow melting as a result of rainfall ice floods creation of ice jam locally distributed flash floods urban flooding 6

Flood damages and costs according to flood events 120 114.9 100 80 flood cost damages mil. EUR 60 60.4 49.9 40 42.0 28.2 31.6 39.9 20 0.024 0.150 0.158 0.133 0.064 0.089 0.108 0 1996 1997 1998 1999 2000 2001 2002 7

Determination of regions where the occurrence of classic regional floods as well as flash floods with extreme effects is much more frequent then on the rest of the territory. Sensitivity of basins to the occurrence of flood extremes was applied using flood index K K = 1/n Q max max /Q annual Q max Q annual n max. Q at a water gauge station for the period considered annual of Q in a station number of years of hydrological series 8

The results contain a K index evaluated from 300 water gauge stations: for a 12-year series of the vegetation seasons (April September) for a 12-year series of the hydrological year It follows from the definition that the higher K is, the more significant the flood situation, i.e. the territory of the basin is more sensitive to floods K significant values during the summer period 9

Selection of regions according to the flood index K criteria: very sensitive K = 30 or more sensitive K at an interval of 20 30 less sensitive K at an interval of 10 20 negligible sensitivity K of less than 10 10

11

Non-Structural Measures Forecasting and warning system Development of a flood monitoring system Innovative forecasting method Local warning system Institutional and legal framework Legal approach Co-operation operation on transboundary water Directive of the European Parliament and the Council on the Assessment and Management of Floods 12

The basic data for the hydrological forecasting and warning system Data from the meteorological monitoring network Network of meteorological stations (24 synoptic and 10 additional synoptic stations) Network of climatological stations (a daily report sent from 59 stations to the centre) Network of rain gauge station (voluntary precipitation network with 568 stations); 76 stations represent an automatic precipitation network with year-round round measurements- equipped by alarm Meteorological radar (2 radars at present), model ALADIN, satellite images for visual usage 13

Network of meteorological stations Synoptic stations (data every 10 min) Automatic precipitation stations Precipitation stations for water equivalent of snow Planed synoptic stations (data every 10 min) Planed automatic precipitation stations Planed precipitation stations for water equivalent of snow 14

Network of hydrological gauge stations On-line stations Forecasting stations Regime stations Planed on-line stations Planed forecasting stations Planed Regime stations 15

Basin Distribution of water gauge station in the main basins Morava Dunaj Váh Nitra Hron Ipeľ Slaná Bodva Hornád Bodrog Poprad Total Number of stations 25 17 114 27 50 26 28 8 34 42 15 386 Number of telemetric stations out of total number 13 14 70 20 30 20 20 6 34 42 15 205 Approximately 1 station for every 125 km2 16

205 telemetric stations 80 station on line 125 operative during (forecasting) the floods All equipped by alarm system 17

The department of Hydrological Forecasting and warning Service operated with 80 operation water gauge stations (profiles) and provides sets of various types of forecasts: Numerical forecast are provided for 11 hydrological forecasting stations Daily forecasts for 13 reservoirs Forecasting trends in water stages increases, decreases, stability are provides for other rivers. During Winter season proceed and issued once a week: Information about sow conditions for whole territory (depth of snow) Water equivalent of the snow development from 219 climatic stations Accumulation of water in the snow cover for 13 water reservoirs and 14 measurement gauge profiles 18

Local warning system (LWS) Goals: To provide the local authorities with sufficient lead time to warm about the origin of floods in small basins and to eliminate their destructive consequences. Several criteria were considered in the selection of these basins: Sensitive regions according to K Climatological indicators such as the intensity of the precipitation, the mapping of any storms, etc. Locality of the basins: upper part of Myjava basin the western part of Slovakia, K = 30 Tributary of the upper part of the Hron river basin the Čierny Hron stream, K = 20 19

Institutional and legal framework The legal approach: Act No. 666/2004 Coll. of Laws on flood protection chiefly deals with: Conditions for protecting life, health and property from flooding; Responsibility of the Civil Service, the government and cooperate bodies and subjects concerning the scope of flood protection in all the river basins; The flood-protection commissions, their duties and responsibilities in the field of flood protection; Delivering personal assistance and devices for flood protection; Sanction for legal violations. 20

The specific flood protection measures include Flood plans Flood inspections Forecasting and warning service Patrol service Flood prevention work Salvage operation 21

Co-operation operation on the transboudary water bilateral agreements with Austria, The Czech Republic, Hungary, Ukraine, Poland Co-operation operation on EARLY FORECAST ALERT SYSTEM (EFAS) Joint Research Centre IES ISPRA Co-operation operation on the EU Framework on the assessment and management of floods - being prepared Deals with Preliminary flood risk assessment Flood risk maps (selection probability, damage maps) Flood risk management plans 22

Final comments There are many structural measures in the Slovak Republic to help mitigate flood damages, but without the development of the above mentioned measures, they will all lose their effectiveness. 23

Thanks for attention gabriela.babiakova@shmu.sk; danica.leskova@shmu.sk 24