“…The amount of radon available to enter dwellings depends on local geological conditions (Tanner, 1964;Nero and Nazaroff, 1984;Stranden et al, 1985;Peake, 1988;Nazaroff, 1992;Hutri and M€ akel€ ainen, 1993;Albarracin et al, 2002;Sundal et al, 2004aSundal et al, , 2004b, while entry into the buildings depends on their physical characteristics, their styles of use, and meteorological conditions (Hubbard et al, 1988;Nazaroff, 1988;Robinson and Sextro, 1997;Miles, 2001;Font and Baixeras, 2003;Janssen, 2003;Fro nka, 2011;Diallo et al, 2015). Despite complex variability in ground conditions and dwelling properties from one place to another in Norway, there is clear evidence for a correlation between the amount of radon generated in the ground around dwellings and the amount of radon that ends up inside the dwellings to present a risk to human health (Smethurst et al, 2008a).…”