Landslide susceptibility assessment forms the basis of any hazard mapping, which is one of the essential parts of quantitative risk mapping. For the same study area, different susceptibility maps can be achieved depending on the type of susceptibility mapping methods, mapping unit, and scale. Althoug...
The newest regulation RD 178/2021 [12] considers the same hypothesis (PPD < 10% and clo = 1) but narrows this range to 21–23 ◦C and 40–50%. The Adaptive modelis described in ISO EN16798-1 [13]. It sets the temperature range and the relative humidity in offices between 20 to...