2016
Výstraha před nebezpečím sesouvání na svazích
KOLEJKA, Jaromír, Petr RAPANT, Kateřina BATELKOVÁ a Karel KIRCHNERZákladní údaje
Originální název
Výstraha před nebezpečím sesouvání na svazích
Název česky
Výstraha před nebezpečím sesouvání na svazích
Název anglicky
Landslide risk early warning
Autoři
KOLEJKA, Jaromír, Petr RAPANT, Kateřina BATELKOVÁ a Karel KIRCHNER
Vydání
Životné prostredie : revue pre teóriu a tvorbu životného prostredia, Bratislava, Slovenská akadémia vied, 2016, 0044-4863
Další údaje
Jazyk
čeština
Typ výsledku
Článek v odborném periodiku
Obor
30305 Occupational health
Stát vydavatele
Slovensko
Utajení
není předmětem státního či obchodního tajemství
Organizační jednotka
Pedagogická fakulta
Klíčová slova česky
sesuv, hodnocení rizika, GIS, varování před sesuvy
Klíčová slova anglicky
landslide, risk assessment, GIS, landslide warning
Příznaky
Recenzováno
Změněno: 12. 3. 2017 16:00, prof. RNDr. Jaromír Kolejka, CSc.
V originále
The landslide risk mapping procedure using GIS technology was developed in the co-operation of scientists at the Institute of Geonics, Czech Academy of Sciences, Ostrava and Technical University of Ostrava, Czech Republic. The procedure is based on the application of standard data available in the public databases in a raster form, the vector form of data is accessible for the disaster management staff only. The risk assessment respects relevant territory features, as slope, aspect, geology, soil humidity, drainage network, land use, registered landslides. All the features were assessed using 0-3 mark scale. The summarization of individual feature assessment provides the final level of the landslide risk in the area. The final resolution of mapping outputs is decimetres. The risky areas were highlighted in the 100 m wide buffer zones along the built objects and technical infrastructure. The maximum landslide risk map data overlay with topic radar data on running and antecedent precipitation shows endangered areas. The risk map combination with a cadastral map selects namely endangered administrative units. The resolution of the landslide risk map allows local administration to organize risk areas monitoring to prevent human casualties and to deploy measures to reduce material damages.
Anglicky
The landslide risk mapping procedure using GIS technology was developed in the co-operation of scientists at the Institute of Geonics, Czech Academy of Sciences, Ostrava and Technical University of Ostrava, Czech Republic. The procedure is based on the application of standard data available in the public databases in a raster form, the vector form of data is accessible for the disaster management staff only. The risk assessment respects relevant territory features, as slope, aspect, geology, soil humidity, drainage network, land use, registered landslides. All the features were assessed using 0-3 mark scale. The summarization of individual feature assessment provides the final level of the landslide risk in the area. The final resolution of mapping outputs is decimetres. The risky areas were highlighted in the 100 m wide buffer zones along the built objects and technical infrastructure. The maximum landslide risk map data overlay with topic radar data on running and antecedent precipitation shows endangered areas. The risk map combination with a cadastral map selects namely endangered administrative units. The resolution of the landslide risk map allows local administration to organize risk areas monitoring to prevent human casualties and to deploy measures to reduce material damages.