Diffuse radiation formula (Heat Overlay): Difference between revisions

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|<math>\tau_a >= 0.7</math>  
|<math>\tau_a >= 0.7</math>  
|}
|}
where <math>\tau_a</math> is the atmospheric transmissivity. This is calculated as:<br>
where <math>\tau_a</math> is the atmospheric transmissivity. This is calculated as:
 
<math>\tau_{a} = \frac{Q_{gl,t}}{1367 \cdot \sin(\phi_t)}</math>
<math>\tau_{a} = \frac{Q_{gl,t}}{1367 \cdot \sin(\phi_t)}</math>



Revision as of 14:19, 23 September 2019

The diffuse radiation is an input parameter for the PET-formula.

The diffuse radation Qd at time t is calculated using the following formula:

where,

  • is the amount of sun radiation at time t, measured at a weather station.
  • is the atmospheric transmission factor at time t.

Atmospheric transmission factor

The atmospheric transmission factor ftransmission,t is calculated as followed:

ftransmission,t Condition

where is the atmospheric transmissivity. This is calculated as:

where,

  • is the amount of sun radiation at time t, measured at a weather station.
  • is the sun altitude angle in ° at time t.