OpenLegislation

Division Calculation of the term Δ ground(S,O)

United Kingdom

Original text. Later amendments are not shown.

(2.5.31)

where

  • Aground(S,O) is the attenuation due to the ground effect between the source S and the diffraction point O. This term is calculated as indicated in the previous subsection on calculations in homogeneous conditions and in the previous subsection on calculation in favourable conditions, with the following hypotheses:

    zr = zo,s ,

  • Gpath is calculated between S and O,

  • In homogeneous conditions: Ḡw = G′path in equation (2.5.17), Ḡm = G′path in equation (2.5.18),

  • In favourable conditions: Ḡw = Gpath in equation (2.5.17), Ḡm = G′path in equation (2.5.20),

  • Δ dif(S′,R) is the attenuation due to the diffraction between the image source S′ and R, calculated as in the previous subsection on pure diffraction,

  • Δ dif(S,R) is the attenuation due to the diffraction between S and R, calculated as in Subsection VI.4.4.b.