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The ratio of diffuse irradiance to direct normal is a conserved quantity throughout the day. Though its absolute value depends on the condition of the atmosphere, ground reflection and obstruction of horizon, once this value is established (by a single measurement) in rung regions. it persists over the entire day. Urban and heavy polluted areas may show considerable daily trends.
The ratio of diffuse irradiance to direct normal is a conserved quantity throughout the day. Though its absolute value depends on the condition of the atmosphere, ground reflection and obstruction of horizon, once this value is established (by a single measurement) in rung regions. it persists over the entire day. Urban and heavy polluted areas may show considerable daily trends.
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