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Does the sun really transmit our annual energy needs in 1 hour?

The sun, an abundant natural energy source, continually showers the Earth with enormous quantities of energy. Some assert that the energy it delivers to Earth in just one hour could satiate the planet's annual energy needs. This claim's validity is often taken for granted, yet it is rarely scrutinized with mathematical rigor. This paper builds a simple model to check the claim for ourselves — and everything we need is GCSE maths: the area of a circle, unit conversion, and standard form.

Which area actually catches the sunlight

We model the Earth as a sphere with a radius of approximately 6,371 kilometers (km), and the sun's energy is assumed to be uniformly distributed over the Earth's surface exposed to the sun. Solar radiation at the top of Earth's atmosphere, also known as solar constant, is approximately 1,361 Watts per square meter (W/m²) [2].

One question worth pausing on: what area of the Earth actually catches this sunlight? Your first instinct might be the surface area of the sphere, 4πr24\pi r^2 — but that would be wrong. The sun is so far away that its rays arrive essentially parallel, and only the half of the Earth facing the sun is lit at any moment. A sphere sitting in a beam of parallel light intercepts exactly as much light as its shadow — a flat disc of radius rr, with area πr2\pi r^2:

Parallel rays from the sun are intercepted by a disc of area pi r squared

From disc area to terawatt-hours

  1. First, we calculate the area that intercepts sunlight at any given moment — as we saw above, a disc with the same radius as the Earth.
Area=πr2=π(6,371)2127,516,117 square km\text{Area} = \pi r^2 = \pi(6,371)^2 \approx 127,516,117 \text{ square km}
  1. Convert this to square meters:
Area=127,516,117 km2×(1,000,000 m2/km2)=1.27516×1014 m2\text{Area} = 127,516,117 \text{ km}^2 \times (1,000,000 \text{ m}^2\text{/km}^2) = 1.27516\times10^{14} \text{ m}^2
  1. Calculate the total power the Earth receives from the sun per second:
Power = Solar Constant×Area=1,361 Watts/m2×1.27516×1014 m21.7361×1017 Watts\text{Power = Solar Constant} \times \text{Area} = 1,361 \text{ Watts/m}^2 \times 1.27516\times10^{14} \text{ m}^2 \approx 1.7361\times10^{17} \text{ Watts}
  1. To find the energy the Earth receives from the sun in one hour, we multiply the power by the number of seconds in an hour:
Energy = Power×Time=1.7361×1017 W×3,600 seconds6.25×1020 Joules\text{Energy = Power} \times \text{Time} = 1.7361\times10^{17} \text{ W} \times 3,600 \text{ seconds} \approx 6.25\times10^{20} \text{ Joules}
  1. Convert this energy to TeraWatt-hours (1 TWh=3.6×1012 Joules)(1 \text{ TWh} = 3.6\times10^{12} \text{ Joules}):
Energy=6.25×1020 Joules×(1 TWh/3.6×1012 Joules)173,611 TWh\text{Energy} = 6.25\times10^{20} \text{ Joules} \times (1 \text{ TWh} / 3.6\times10^{12} \text{ Joules}) \approx 173,611 \text{ TWh}

What our model ignores

Our simple model suggests that the sun indeed delivers about 173,611 TWh173,611 \text{ TWh} to the Earth in just one hour, exceeding the global annual energy needs of 170,000 TWh170,000 \text{ TWh}. However, this does not consider factors like the earth's tilt, atmospheric absorption, seasonal variations, or the technology required to harness this energy, meaning that the actual obtainable amount of energy that could be harnessed in one hour is likely to be a fraction of the figure we've obtained.


References:

[1] Our World in Data: Energy Production & Consumption

[2] Kopp, Greg, and Judith L. Lean. "A new, lower value of total solar irradiance: Evidence and climate significance." Geophysical Research Letters 38.1 (2011).

Note: The calculations in this paper are based on a simplified model and should be treated as rough estimates.