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Image of the Sun. The image was taken from the astrophysics department at Stanford university where you can find more information about solar research. |
CLICK HERE for a Mathematica notebook on functions, derivatives, and plots. Everything you need for this lab can be found in this file.
This lab is due Monday, March 15 in lecture. Late labs are not accepted. You are encouraged to work in groups of no more than 3 people, though you can work alone. If you do work in a group, your partners can be from any of the Calculus 3 lectures. Turn in only one lab per group.
On your title page, clearly mark
For general directions for your report, please look at a sample report.
The goal with this lab is to apply the concept of optimization over a compact domain to a physical problem. The function you qualitatively optimize depends on two variables. Your result should be critically interpreted. The lab will also provide practice in report writing. You will also learn some facts about solar radiation and how the solar radiation received on the ground depends on the season, time of the day and weather conditions.
In order to solve the problem you are assigned later in this instruction, it is important to read the background below!
In this lab you will analyze how the efficiency of a solar panel depends on the season and its orientation. The solar radiation falling on a tilted plane (such as a solar panel) depends on numerous factors: the orientation of the plane, the time of the day, the season, the weather, etc. In the next few sections you will learn more about how this affects the power we can receive from solar panels.
The Earth's orbit about the sun is almost circular so for this lab we will assume that the distance to the Sun is constant. However, the axis of the Earth is tilted relative to the plane in which the Earth moves around the Sun. The angle between the axis and a normal to this plane is roughly
. As indicated in Fig. 1, the north pole points away from the Sun during the northern hemisphere winter, and points towards the Sun during the northern hemisphere summer.Now let us imagine that we stand on the equator. We introduce the angle s as illustrated in Fig. 2. In words, the angle s determines the angle between you (if you are standing straight up on the equator at noon) and a line from the center of the Earth to the center of the Sun. By "noon" we mean the time of the day when the Sun is at its highest position in the sky. As we can see from Fig. 2,
on December 21 (winter solstice) and
on June 21 (summer solstice). On March 20 (vernal equinox) and September 22 (autumnal equinox)
. Hence, we can think of s as describing the time of the year. This angle s will be of great importance in the lab so let us summarize its values in a table.
| Date(s) |
s |
| December 21, 2009 |
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| December 22, 2009 - March 19, 2010 |
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| March 20, 2010 - June 20, 2010 |
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| June 21, 2010 - September 21, 2010 |
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| September 22, 2010 - December 20, 2010 |
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IMPORTANT: The functions we use later will require that we convert degrees to radians. For example, 23 degrees is 23/180*Pi radians.
Note that
.
In this lab we will consider the solar radiation falling on a tilted plane. We will consider a solar panel that maintains a fixed angle with respect to the ground throughout the entire day. Let u be the angle between the plane and the ground. If
, then the plane is lying on the ground and if
the plane is standing up vertically. (If u is negative, the solar panel is facing south. If u is positive, the solar panel is facing north. Understanding this might give you a better idea of what's going on when you look at your 3D plot in Question 2.)
Introduce t to be an angle proportional to the time of the day such that
at 6 A.M.,
at noon and
at 6 P.M.. If I0 is the intensity of solar radiation (measured in W/m2, where W=J/s) falling on the ground, then the radiation on the tilted plane, Iplane is given by the function:
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(1) |
There are more factors that affect the radiation on the plane. There is also an absorption factor which is strongly dependent on the distance the sun rays have traveled through the atmosphere before it reaches the ground. The law describing absorption is called Beer's law (sic!). Let us describe the absorption with a function A(s,t) such that
. Here A(s,t)=1 means that basically all the sunlight gets through the atmosphere (no light absorption) and that the absorption of light by the atmosphere increases with decreasing values of A(s,t) so that a low value (
) of A(s,t) means that almost no sunlight makes it through (very high absorption). In addition, we should also take different weather patterns into account since the solar radiation on the ground varies with the cloudiness. Let us describe the cloudiness with a function C(s,t) such that
. Here C(s,t)=1 means that there are no clouds and that the cloudiness increases with decreasing values of C(s,t) so that a low value (
) of C(s,t) means that the sky is covered with thick black thunder clouds. The total amount of energy received per square meter and day is now given by the following equation.
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(2) |
Here tmin and tmax are the angles that we talked about above. These angle limits represent the time of sunrise and sunset respectively. These times vary over the year. However, on the equator these times are relatively constant and to simplify the mathematics we will assume that for our purpose we can use
and
throughout the year. (This is an approximation. For a more careful analysis of a problem, we should let these times depend on the season, i.e., s.)
The Boulder company "Solar Power Inc." (invented for this lab) has asked you to do a consulting job for them. They will export solar panels to the pacific island "Suluclac" which is located on the equator. A meteorologist has described their weather by the "cloudiness function"
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(3) |
) collected by the solar panel each day.
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(4) |
Note that this equation is only valid when s and u are given in radians! Also remember that the angle u of the solar panel is fixed on a given day. We are not working with a panel that moves throughout the day to follow the sun by the hour. A panel like this might collect more solar energy, but it also requires a more expensive mechanical set up, so a solar panel with a fixed angle u, which may be changed manually on, say, a daily or weekly basis to at least account for the time of year, is often more practical.The variable s is defined in section III.a and u is defined in section III.b, but recall that s determines the time of year and u is the angle between the solar panel and the ground. The energy equation given above has already incorporated effects due to absorption and cloudiness, so the function W(s,u) is already in the form you will use for this lab.
The company now wants you to answer the following questions.The questions "look" long because they contain lots of hints!
In the domain
and
where the angles are given in radians, find the critical point(s) of w[s,u] (see definition for critical point and read about the second derivative test for local extrema, starting on page 970 of your Calculus book), and compute the energy at the point(s).
Note on Questions 3 and 4: You will find all local extreme points of the energy function in its domain (notice that in part 2 above you have already searched for these points in the interior of the domain. All you have left to do is to look for these points on the boundary of the domain of the function. Don't forget to check corner points.) The point of doing this is to see if you have any boundary values that are bigger or smaller than the max or min interior values.
First remember that the angle u refers to the angle that a fixed solar panel makes with the ground. The solar panel does not move on its own. It will stay at the same angle until someone manually changes it. Suppose we hire someone to change the angle u of the solar panel on a regular basis, maybe once at the end of each day, so that on any given day we end up collecting as much energy as we can, based on the angle s that the equator makes with the incoming sun rays.
Refer to your book (pgs 970-972) for critical point definition and second derivative test for two variable functions.
Read the definition of local maxima and minima on page 970. Among all interior critical points, boundary candidates, there should be only 3 local extrema. Note that in Questions 2 and 3, your are asked to find all candidates for critical points, i.e., critical points in the interior, ciritical points in the interior of the boundary, and corner points. This will give you a list of all possible candidates for global extrema in the given region--which you will need to find in Question 3.
"Solar Power Inc." wants you to describe all your results in a formal written report, containing an introduction to the concept of solar energy collection, relevant equations given, ANSWERS TO ALL QUESTIONS at appropriate places within paragraphs, and a conclusion.
Remember the following:
During the week prior to the lab's due date, there will be TAs present in ECCR 143 to help you with the labs. Please see the lab hour schedule.
Lab Created by Kristian Sandberg. Modified by John Villavert and Jason Boorn, Oct. 2008.
Further Modified by Russell Latterman, March 2009 and then Henry Romero, March 2010.