Diffuse radiation formula (Heat Overlay): Difference between revisions
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The diffuse radiation is an input parameter for the [[PET_formulas_(Heat_Overlay)|PET-formula]] | The diffuse radiation is an input parameter for the [[PET_formulas_(Heat_Overlay)|PET-formula]]. | ||
The diffuse radation Q<sub>d</sub> at time t is calculated using the following formula: | The diffuse radation Q<sub>d</sub> at time t is calculated using the following formula: | ||
<math>Q_{d,t} = Q_{gl,t} \cdot f_{transmission,t}</math> | |||
where, | where, | ||
* | * <math>Q_{gl,t}</math> is the amount of [[Hourly_radiation_(Heat_Overlay)|sun radiation]] at time t, measured at a weather station. | ||
* | * <math>f_{transmission,t}</math> is the [[#Atmospheric transmission factor|atmospheric transmission factor]] at time t. | ||
==Atmospheric transmission factor== | ==Atmospheric transmission factor== | ||
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!Condition | !Condition | ||
|- | |- | ||
|1 | |<math>1</math> | ||
| | |<math>\tau_a < 0.3</math> | ||
|- | |- | ||
|1.6-2 | |<math>1.6 - 2 \cdot \tau_a</math> | ||
|0.3 < | |<math>0.3 < \tau_a < 0.7</math> | ||
|- | |- | ||
|0.2 | |<math>0.2</math> | ||
| | |<math>\tau_a >= 0.7</math> | ||
|} | |} | ||
where | 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> | |||
where, | where, | ||
* | * <math>Q_{gl,t}</math> is the amount of [[Hourly_radiation_(Heat_Overlay)|sun radiation]] at time t, measured at a weather station. | ||
* | * <math>\phi_{t}</math> is the [[Sun_altitude_(Heat_Overlay)|sun altitude angle]] in ° at time t. | ||
* <math>1367</math> is sourced from the {{Heat DPRA Report}}. | |||
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Latest revision as of 11:52, 13 September 2021
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.
- is sourced from the DPRA Heat stress report.