Diffuse radiation formula (Heat Overlay): Difference between revisions
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* <math>Q_{gl,t}</math> is the amount of [[Hourly_radiation_(Heat_Overlay)|sun radiation]] at time t, measured at a weather station. | * <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>\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 Raport}}. | |||
{{Template:HeatOverlay_formula_nav}} | {{Template:HeatOverlay_formula_nav}} | ||
{{Template:Heat_Module_buttons}} | {{Template:Heat_Module_buttons}} |
Revision as of 15:32, 13 February 2020
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 Template:Heat DPRA Raport.