Page 178 - Çevre Şehir ve İklim Dergisi İngilizce - Özel Sayı
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Determination of Potential Avalanche Release Areas, Avalanche Mobile Application and
                Preparation of Avalanche Hazard Maps in Türkiye; the Case of Palandöken Ski Centre

               •   Digital elevation model (DTM) with 5 X 5 resolution
               •   Active and potential avalanche starting zones acquired through land
                  analyses and the algorithms used
               •   Density (kg/m³): 300,
               •   Law of Friction: Voellmy Model,
               •   Return Period: 100 years,
               •   The avalanche size: large
               •   Fracture depth: Due to the lack of data from the Palandöken Ski Resort
                  meteorological station, it could not be used in the study. To determine
                  the fracture depth in the starting zone, the approach from Schellander’s
                  (2004) study in the Austrian Alps was adopted, and the 100-year fracture
                  depth was taken as 1.6 meters.
               •   Friction Parameters: Automatically marked.
               Countries like Sweden, Austria and France use color scale while creating
            avalanche hazard maps. The color scale is determined based on the pressure
            values acquired from the two dimensional avalanche simulation results, and
            the mapping is made based on these data.
               For instance, as seen in Figure 10, areas in Austria with avalanche pressures
            ranging between 1 and 10 kN/m² are displayed in yellow, while regions with
            pressure values of 10 kN/m² and above are indicated in red. This color scale
            makes the level of avalanche hazard visually more understandable, enabling
            users to easily assess the risks.
               There has not been such a comprehensive
            study in our country to date. With the method
            developed  by  ÇEM  General  Directorate,
            potential  runout  and  accumulation  zones
            with avalanche pressures over 1 kN/m² are
            displayed in blue. Likewise, the active runout
            and  accumulation  zones  with  avalanche
            pressures  over  1  kN/m²  are  hatched  in
            blue. Additionally, potential avalanche
            starting zones are coded in red, and active
            avalanche starting zones are mapped in red
            and hatched.
               The  same  method  was  utilized  in
            this study as well, aiming at presenting
            avalanche  hazard  mapping  in  our  country
            in a more systematic and comprehensive
            manner.



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