The Terran Series
Your Latitude
Latitude
34.0°N · △ Northern Hemisphere
Solar Flux at Solar Noon Today · Top of Atmosphere
W/m²
0 400 800 1200 1361 W/m²
TOA Peak Flux
Top of atmosphere at solar noon. No atmospheric loss.
Surface Estimate
Clear sky estimate after atmospheric absorption (~70% transmission at zenith).
Daily Total
Integrated flux over all daylight hours today. kWh/m²/day.
Solar Altitude
Sun's maximum height above horizon at solar noon today.
Solar Declination
Angle of sun above/below celestial equator. ±23.436° at solstices.
Earth-Sun Distance
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
LowModHigh V.HighExtreme
Skin Safety
Vitamin D Synthesis Time · Face + Arms Exposed
Fair Skin (I–II)
Medium Skin (III–IV)
Dark Skin (V–VI)
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.