Your Latitude
Latitude
34.0°N · △ Northern Hemisphere
Solar Flux at Solar Noon Today · Top of Atmosphere
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W/m²
0
400
800
1200
1361 W/m²
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TOA Peak Flux
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Top of atmosphere at solar noon. No atmospheric loss.
Surface Estimate
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Clear sky estimate after atmospheric absorption (~70% transmission at zenith).
Daily Total
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Integrated flux over all daylight hours today. kWh/m²/day.
Solar Altitude
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Sun's maximum height above horizon at solar noon today.
Solar Declination
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Angle of sun above/below celestial equator. ±23.436° at solstices.
Earth-Sun Distance
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Today's distance factor relative to mean. Perihelion Jan 3, aphelion Jul 4.
Flux by Latitude · Today · TOA Peak W/m²
Your Flux Across the Terran Year · Daily Total kWh/m²
UV Index & Vitamin D · Solar Noon Today
UV Index
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LowModHigh
V.HighExtreme
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Skin Safety
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Vitamin D Synthesis Time · Face + Arms Exposed
Fair Skin (I–II)
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Medium Skin (III–IV)
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Dark Skin (V–VI)
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The 6.9% Southern Hemisphere Advantage
NH Summer Peak (Aphelion · Jul 4)
1,316 W/m²
SH Summer Peak (Perihelion · Jan 3)
1,406 W/m²
Difference
+90 W/m²
Asymmetry
+6.9% SH advantage
Earth's orbital eccentricity (0.0167) means it is closest to the sun in early January — during Southern Hemisphere summer — and furthest in early July, during Northern Hemisphere summer. By the inverse square law, the SH receives 6.9% more solar energy at its summer peak than the NH does at its own. The Gregorian calendar contains no acknowledgment of this physically measurable asymmetry. The Terran Series does.