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Teacher's Guide
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Overview |
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This a two-day inquiry-based learning activity for seventh and
eighth grade students. Over these two days, students develop and
implement their own strategies for measuring the rotational period
of the sun. They begin by viewing an image of the sun directly
from a screen attached to a telescope (NEVER look at the sun
through an unfiltered telescope!!). The teacher then motivates a
discussion in which the students suggest general strategies for
measuring a rotational period. Breaking into small groups,
students work to devise and implement methods to apply these
general strategies. To wrap up, the students will come back
together as a class and present various group's methods and
results and then discuss the differences among their findings and
examine what the differences mean.
Throughout, this activity is largely student driven, with
students brainstorming strategies, figuring out how to implement
those strategies, and analyzing the differences among their
results. To aid the teacher in keeping things on track to
interesting phenomena, we have noted several key concepts in
italics below. Not all of these points will be broached by
the kids' investigations, so it's not expected that every point
should be explained to the kids--only the ones that can help
unwrap the problems the kids encounter need be mentioned.
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Lesson Goals and The National Standards |
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The importance of the relationship between this activity and
national teaching standards cannot be over-stated. In fact, the
goals of this activity consist of standards we hope will be
realized for the students. For a discussion of the relevant
standards and the goals and rationale underlying this activity,
please follow this
link.
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Materials
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- telescope fitted with sunspot screen (optional)
- A series of solar
images
- tracing paper or overhead sheets with markers
- rulers
- string
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The Plan, Day One - Forty to Fifty Minutes.
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I. Motivation.
If you have a chance prior to the activity, it's a good idea to
set up the telescopes and sunscreens outside to show the kids
real-life sunspots. Seeing these sunspot images directly from the
sun will hopefully make the images taken from the web seem more
real (that is, less like computer magic).
About ten minutes for a motivating discussion:
What does the class know about he Sun? Hold up a pair of solar
images from consecutive days, and read the dates off (for example,
October 2nd, 2000 and October 3rd, 2000.) What has happened from
October 2nd to October 3rd? Invariably, someone will say that
the spots have moved to the right, or even that the sun has turned
to the right. So now we know something new about the sun - it
rotates! Let's explore this new fact: let's determine the
rotational period of the Sun, how long it takes for the sun to
rotate all the way around one time.
To get us pointed in the right direction, how could we measure
the rotational period of the Earth if we were looking at the Earth
from a distant spaceship? Can anyone think of reasons why picking
a feature on a body and waiting for it to go all the way around
might not always be practical? (it might take too long if the
object has a very long rotational period, or clouds might get in
the way). While there are no clouds to cover the sunspots,
each spot is only temporary (they can last from 2 or 3 to 100 or
more days) and may simply disappear before a full rotation is
completed. The solution: As is often the case in science, we
modify our plan to work with the data we can get.
II. Problem Solving:
Devising Strategies.
About fifteen-twenty minutes for brainstorming:
To
make sure everyone has a sense that we don't necessarily need data
that spans an entire rotational period, try posing a question:
Draw a circle and two dots on the board, about like the picture to
the right, and tell the kids to suppose the dots represent the
position of a sunspot on two consecutive days. Now ask, "What if I
told you it will take 1000 days for the sun to make one complete
rotation? Would you believe me? Why not?"
This is a good point to introduce the images from the web and
break into small groups. As the students can now see, our data
only spans a fraction of a rotation. Ask the students to discuss
(in their groups) possible strategies for determining the full
rotational period from this data. It is probably best to announce
that materials such as rulers and tracing paper are available in
case the students need them, rather than simply handing things
out. When the students begin analyzing the data (for example, by
tracing the sun's image on the tracing paper and then picking a
sunspot and tracing the spot's image for each day onto the paper),
they might notice any of several points. You may want to guide a
group through some of these if the kids are having trouble sorting
something out:
- The measured circumference of the sun can be determined at
any latitude by measuring the diameter of the sun at that
latitude and multiplying by Pi.
- If the daily travel of a spot is to be divided into the
measured circumference of the sun (Pi times measured diameter),
then using the distance between two consecutive days will tend
to reduce a certain geometric
error (as opposed to measuring the travel of a spot over
nine days and then dividing by nine.)
- If a spot goes from the center of the sun to the edge, then
the sun has completed one fourth of a rotation.
- The sun rotates on a slightly tilted axis (only about 7.25
degrees, as opposed to the Earth's 23.5 degree tilt.)
- Since the sun is spherical, the spot's images from day to
day tend to be closer together when the spot is near the edge of
the sun's image than when the spot is near the center.
- Measuring the total travel of a spot over the nine days and
then dividing by nine to determine the average distance traveled
in one day might tend to reduce measurement error (as opposed to
just measuring the distance between two consecutive days'
images).
The last fifteen to twenty minutes for reporting out:
Once the groups have had enough time for a few of them to come
up with feasible strategies for measuring the rotational period,
reconvene the class and tell them about the homework assignment:
each kid will write a brief description of a method for
determining the period; include any drawings and prose they feel
they would need to convince a skeptical friend that the method is
reasonable (due the next day). They should feel free to use any of
the ideas presented in the remainder of the class period. This worksheet
describes the assignment and helps the students organize their
thoughts.
At this point, the groups who have come up with methods explain
their strategies to the rest of the class. Here are a few examples
of what they might come up with.
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The Plan, Day Two -
Thirty-five to Forty Minutes. |
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III. Putting Theory
into Practice.
Fifteen minutes for groups to decide on a strategy and
implement it:
At this point, everyone in the class should have a clear
understanding of at least one method for determining the
rotational period. So the task for the next fifteen minutes is for
the students (in their small groups) to agree on a method and
carry it out.
If they have extra time, they may want to check their results
by trying out a different method. Or, if their method involved
rounding off to the nearest day (and if the rounding error was
significant), you might ask them to see if they get a different
period if they carry out the calculations using data rounded to
the nearest hour.
IV. Putting it all
Together.
Twenty to twenty-five minutes to discuss the results:
Once the groups have come up with measurements, it's time to
reconvene as a class and discuss the results. In this segment,
each group will report to the rest of the class, describing the
method they used, which spot(s) they examined, and their findings
for the rotational period. It is important to emphasize that there
are advantages and disadvantages of different methods, and that it
is not appropriate to think of any one method as "best."
If there are discrepancies among the measurements for a given
spot, then have the groups explain their methods and see if the
students can come up with reasons for the differences based on
differences in the methods. Such reasons may include geometric
considerations, proneness of a particular method to human error,
etc..
Do the measurements for each given spot tend to agree from
group to group, but average measurements from one spot to the next
tend not to agree? Do the students see any reasons for this? If
the rotational periods appear to be increasing as spots are chosen
farther away from the equator, then point (2) below should be
mentioned (with congratulations for observing a subtle physical
phenomenon!). Here is more
detail on this phenomenon.
Below are some general considerations for this part of the
discussion:
- Measurement error is compounded when smaller distances are
measured. For example, if an object 10.0 cm long is measured to
be 10.1 cm, then you are only off by one percent, but if an
object 1.0 cm is measured to be 1.1 cm, then you are off by ten
percent, even though you are still off by the same amount, 0.1
cm!
- Sunspots near the equator may give rise to a shorter
measured rotational period than those farther away from the
equator. This may not be due to error. Owing to the fluid nature
of the sun's body, the rotational period actually increases as
you move away from the equator toward the poles. It may be best
to leave this point alone unless the students' measured
rotational periods seem to demonstrate this fact.
- If a spot is near the edge of the sun's image, not much of
its movement is in a direction we can see, so we measure it as
moving less in a day than it really does move. Hence, we should
expect our measurement to imply that the spot takes longer to
get all the way around than it really would take. That is, if we
observe spots near the edge, we may tend to get longer
rotational periods. For more on how this works, review the geometric
observations page.
- When we measure the movement of a spot on our paper, we are
measuring travel on a straight line (since our paper is flat and
our ruler is straight), but the sun is spherical so when it
turns, a spot on its surface really moves in an arc. So instead
of measuring an arc's length, we measure the length of a certain
line segment which is even shorter than the line segment
connecting the arc's endpoints. Naturally, this line is shorter
than the arc (after all, we all know what the shortest path
between two points is!), so we measure the spot as having
traveled less than it actually did. Again, this results in a
longer measured rotational period and the geometric
observations page serves as a reminder of how this works.
Here is a homework
assignment you can give after the second day.
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Assessment |
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To help focus the question of whether this activity has met its
goals in the classroom, Scopes for Schools has created a guide
for assessment, which includes both homework and in-class
components.
Assessment is a vital tool for Scopes for Schools as we seek to
improve and evaluate our activities and our program as a whole.
After you have had a chance to assess
this activity , Scopes for Schools would greatly appreciate a
chance to learn from both your specific experience with the
activity and your general experience as an educator.
We invite any feedback you care to give, and would especially
like to hear about:
- How well the activity met it's goals, as demonstrated by the
assessment;
- What we can do in terms of altering the activity itself or
the assessment techniques to better meet our goals;
- Any suggestions you have ("shoulds" or "should nots") for
future teachers who use this activity.
This questionaire
fleshes out these questions in a way that we have found
particularly helpful.
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