Solar irradiation on the Earth as a function of latitude.

Click For Summary
SUMMARY

The discussion focuses on calculating solar irradiation on Earth as a function of latitude, specifically addressing the power output of the Sun and the power received in Spain at 40° N latitude. The solar output is given as 1.4 kW/m², and the total power output of the Sun is calculated to be approximately 3.9 x 10²⁶ W. The participant successfully determined the power received on Earth but sought clarification on how to account for variations in solar power at different latitudes and times of the year, suggesting the use of spherical trigonometry for accurate calculations.

PREREQUISITES
  • Understanding of the Poynting vector in electromagnetic theory
  • Knowledge of spherical trigonometry for calculating angles and areas
  • Familiarity with solar irradiance measurements and their implications
  • Basic principles of solar energy absorption by surfaces
NEXT STEPS
  • Research the application of spherical trigonometry in solar energy calculations
  • Explore the impact of Earth's axial tilt on solar irradiation throughout the year
  • Learn about solar irradiance models and their practical applications
  • Investigate tools for calculating solar power received at various latitudes and times
USEFUL FOR

Students in physics or engineering, solar energy researchers, and professionals involved in renewable energy systems who need to understand solar power distribution based on geographical and temporal factors.

Lavabug
Messages
858
Reaction score
37

Homework Statement


Given the following info:

Solar output(modulus of the Poynting vector): 1.4kW/m^2
Earth radius: 6370km
Average Earth orbit radius: 1.49*10^11 m

Find the total power output of the Sun, power received on the Earth, and the power received in Spain if its surface area is 5*10^2 km^2 and is at a latitude of 40 N.

Homework Equations


Poynting vector formula?

The Attempt at a Solution


I managed to get the right answer for the power received on the Earth, but I'm not sure how to proceed with the other 2 questions. Wouldn't the power received at a given latitude depend on the time of the year? I found this applet that calculates it for you and apparently at 40 N, the solar output never reaches 1.4kW at any time of the year:
http://pvcdrom.pveducation.org/SUNLIGHT/SHCALC.HTM

... so I'm guessing I'll have to resort to spherical trigonometry some way or another? I am given no other info and this is a course purely on electromagnetic optics.
 
Physics news on Phys.org
The time of year is important as is the time of day as is the Earth's atmosphere.

Say you have a black square, 1 meter by 1 meter that absorbs all light that falls on it. Say you are at the equator and hold the square perpendicular to the suns light. What is the power absorbed? Now hold the same black square so that the suns light and the unit normal of the black plane make and angle theta. The power now absorbed is rescued by a factor of cos(theta)?
 
I think I see it now, drawing a circle (earth) with normal surfaces on the equator and at 60º from the N pole, using trigonometry I get P(at 60 N) = Power(known)*(cos60), which is a halve of the known power output at the given orbital distance (which I got right: 3.9*10^26W).

However, what you're saying assumes the equator is aligned with the sun/the Earth isn't tilted, but since the problem says nothing to that avail so I guess its reasonable? Thanks.

How would you solve the first part? Wouldn't I need the radius or surface area of the Sun?
 
Last edited:
You are given what is needed, the power/m^2 at the distance the Earth is from the sun and the distance to the sun.

power per area times area = power
 

Similar threads

  • · Replies 3 ·
Replies
3
Views
5K
  • · Replies 7 ·
Replies
7
Views
5K
  • · Replies 1 ·
Replies
1
Views
2K
  • · Replies 1 ·
Replies
1
Views
4K
  • · Replies 4 ·
Replies
4
Views
2K
Replies
6
Views
4K
  • · Replies 2 ·
Replies
2
Views
1K
  • · Replies 2 ·
Replies
2
Views
4K
  • · Replies 6 ·
Replies
6
Views
6K
Replies
6
Views
6K