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Investigation 3 Beam Spreading and Solar Angle Grade 6 FOSS Weather and Water.

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Presentation on theme: "Investigation 3 Beam Spreading and Solar Angle Grade 6 FOSS Weather and Water."— Presentation transcript:

1 Investigation 3 Beam Spreading and Solar Angle Grade 6 FOSS Weather and Water

2 Earths Axis Earth rotates on its axis to produce day and night. Earth rotates on its axis to produce day and night. The tilt of Earths axis produces changes in day length over the course of the year (one revolution around the Sun). The tilt of Earths axis produces changes in day length over the course of the year (one revolution around the Sun).

3 Winter and Summer Summer (summer solstice) occurs when the axis is angled toward the Sun. Summer (summer solstice) occurs when the axis is angled toward the Sun. Winter (winter solstice) occurs when the axis is angled away from the Sun. Winter (winter solstice) occurs when the axis is angled away from the Sun. Seasons are opposite in Northern and Southern Hemisphere. Seasons are opposite in Northern and Southern Hemisphere.

4 Radiant Energy Energy Travels from the Sun to Earth as radiation. Energy Travels from the Sun to Earth as radiation. Radiant energy travels in rays. Radiant energy travels in rays. The number of rays hitting a given area is energy density. The number of rays hitting a given area is energy density. When lots of rays hit an area, energy density is high. When lots of rays hit an area, energy density is high. When few rays hit an area, energy density is low. When few rays hit an area, energy density is low.

5 Solar Angle The angle at which light strikes a surface is called solar angle. The angle at which light strikes a surface is called solar angle. Low-solar-angle rays are hitting the Earths surface at about 15°. Low-solar-angle rays are hitting the Earths surface at about 15°. Light rays shining from directly overhead have a higher solar angle and are hitting Earths surface at a 90° angle. Light rays shining from directly overhead have a higher solar angle and are hitting Earths surface at a 90° angle.

6 Solar Angle Think about our flashlight demonstration: The flashlight puts out a steady beam of light rays at about 5 cm across: Think about our flashlight demonstration: The flashlight puts out a steady beam of light rays at about 5 cm across: When the light beam falls on a surface directly above (90°), the area it covers is a circle about 20cm (squared). When the light beam falls on a surface directly above (90°), the area it covers is a circle about 20cm (squared). When the angle that the light is coming from changes from 90° to 15°, the beam of the oval surface is about 60com (squared). When the angle that the light is coming from changes from 90° to 15°, the beam of the oval surface is about 60com (squared).

7 Solar Angle The picture on the left shows the beam light at a 90° angle. The picture on the right show the beam of light at a 15° angle.

8 Solar Angle The incoming rays of light (from the flashlight) are equally spaced in both beams. The incoming rays of light (from the flashlight) are equally spaced in both beams. But because of the solar angle, three times as many rays are falling on Earth when the light comes from a high solar angle. But because of the solar angle, three times as many rays are falling on Earth when the light comes from a high solar angle. The density of energy is greatest when light shines on a surface at a 90° angle. The density of energy is greatest when light shines on a surface at a 90° angle.

9 Beam Spreading The way a light beam covers a larger area when it hits a surface at an angle is called beam spreading. The way a light beam covers a larger area when it hits a surface at an angle is called beam spreading.

10 Solar Angle on Earth Because Earth is round, the angle at which light hits it is different from place to place. Because Earth is round, the angle at which light hits it is different from place to place. Light does not come to Earth from different angles; light strikes surfaces that are different angles. Light does not come to Earth from different angles; light strikes surfaces that are different angles.

11 Solar Angle The angle between the incoming rays of light and the surface of the land is the solar angle. The angle between the incoming rays of light and the surface of the land is the solar angle.

12 Solar Energy and Solar Angle The greater the solar angle, the greater the density of radiant energy. The greater the solar angle, the greater the density of radiant energy. Light shining from directly above is most intense. Light shining from directly above is most intense. Light coming at an angle is less intense. Light coming at an angle is less intense.

13 Solar Energy Solar energy is most intense during the middle of the day in the region of the tropics. Solar energy is most intense during the middle of the day in the region of the tropics. Energy is least intense in the morning and evening, as well as the extreme north and south regions of the land. Energy is least intense in the morning and evening, as well as the extreme north and south regions of the land.

14 Linking Solar Energy to Weather Almost all of the energy coming to the planet Earth is solar energy. Almost all of the energy coming to the planet Earth is solar energy. Light absorbed by the land, water, and air is converted to heat. Light absorbed by the land, water, and air is converted to heat. Heat is the form of energy that makes things happen in the atmosphere. Heat is the form of energy that makes things happen in the atmosphere. Atmospheric activities are what we call winter. Atmospheric activities are what we call winter.

15 Consider This… What influence does solar angle have on heating of Earth? What influence does solar angle have on heating of Earth?

16 Putting it all together… Areas of the planet where solar radiation shines directly down on Earth are subjected to more intense energy than areas that experience beam spreading. Areas of the planet where solar radiation shines directly down on Earth are subjected to more intense energy than areas that experience beam spreading.

17 Putting it all together… The greater the amount of energy absorbed, the hotter the area becomes. The greater the amount of energy absorbed, the hotter the area becomes. The hottest part of Earth is in the region of the tropics. The hottest part of Earth is in the region of the tropics. That is why mornings and evenings are cool, and the hottest part of the day is in the middle. That is why mornings and evenings are cool, and the hottest part of the day is in the middle.

18 Putting it all together… Because Earths axis is tilted 23.5°, the Northern Hemisphere receives more intense solar energy in the summer months, making summer hotter. Because Earths axis is tilted 23.5°, the Northern Hemisphere receives more intense solar energy in the summer months, making summer hotter. During the winter months, sunlight strikes the Northern Hemisphere at a low solar angle, resulting in less heating from solar radiation. During the winter months, sunlight strikes the Northern Hemisphere at a low solar angle, resulting in less heating from solar radiation.


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