Solar irradiation on the Earth as a function of latitude.

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Homework Help Overview

The discussion revolves around calculating solar irradiation on Earth as a function of latitude, using given parameters such as solar output, Earth's radius, and average orbital radius. The original poster attempts to find the total power output of the Sun, the power received on Earth, and specifically the power received in Spain at a latitude of 40 N.

Discussion Character

  • Exploratory, Assumption checking, Mathematical reasoning

Approaches and Questions Raised

  • Participants discuss the dependence of solar power received at a given latitude on seasonal variations and time of day. The original poster questions the need for spherical trigonometry to solve the problem. Others explore the concept of power absorption based on angle and surface orientation relative to sunlight.

Discussion Status

The discussion is active, with participants exploring different interpretations of the problem. Some guidance has been offered regarding the relationship between power absorption and angle, but no consensus has been reached on the best approach to solve the initial questions.

Contextual Notes

Participants note the lack of information regarding the Earth's tilt and its impact on solar irradiation, as well as the absence of specific details about the Sun's radius or surface area, which may be relevant to the calculations.

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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.
 
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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
 

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