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Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

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Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth
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Page 1: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Foundations of Physical ScienceWorkshop: Variations in the

Heating and Cooling of Earth

Page 2: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Key Question

What causes the seasons?

Page 3: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Two part InvestigationFirst ,we will measure how

variations in DISTANCE effect light intensity

Then, we will measure the light intensity at different PLACES on the globe

Page 4: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Light Intensity and Solar Energy Greater tilt angle spreads the light out over more area

More direct light = more energy/area = greater intensity

Areas with greater intensity will heat more

Page 5: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.
Page 6: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Developing a hypothesis about the seasons

Page 7: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Setting up your model of Earth’s orbit around the

sun The light represents the sun

Measure the light intensity with the solar cell and multimeter

Compare values

Page 8: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Measuring Light Intensity based on Distance

Four distances

A – 150 cm

B – 147 cm

C – 149 cm

D – 153 cm

Page 9: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Results

Position Distance from the sun (km)

Scale distance from the sun (cm)

Light intensity (mA)

A 150,000,000 150

B 147,000,000

C 149,000,000

D 153,000,000

Page 10: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Results

Position Distance from the sun (km)

Scale distance from the sun (cm)

Light intensity (mA)

A 150,000,000 150 1.02

B 147,000,000 147 1.09

C 149,000,000 149 1.07

D 153,000,000 153 0.98

Page 11: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

How does Earth’s tilt affect the sun’s intensity?

Page 12: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

How does Earth’s tilt affect the sun’s intensity?

Page 13: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Findings What role does axial tilt play in the intensity

of light on Earth?

At which position (A-D) and latitude does Earth receive the most light? The least light?

Which factor, distance or axial tilt, plays the most significant role in casing the seasons?

Was your hypothesis supported by your results?

Page 14: Foundations of Physical Science Workshop: Variations in the Heating and Cooling of Earth.

Where is Summer in the Northern Hemisphere? (and

why) From position D to A is summer for the Northern Hemisphere

That is the segment of Earth’s orbit where the Northern Hemisphere is pointing at the sun and getting the most direct, and therefore most intense light


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