Why is it so hot here in the

Why is it so hot here in the summer?

The Earth in Space TEK 8. 7 A – the student knows the effects resulting from cyclical movements of the Sun, Earth, and Moon. The student is expected to model and illustrate how the tilted Earth rotates on its axis, causing day and night, and revolves around the sun causing changes in seasons.

Rotation - Earth spinning on its axis l Earth’s rotation on its axis causes day and night l It takes 24 hours for Earth to rotate once on its axis l Earth rotates in a counterclockwise direction l Earth rotates at about 1, 600 kilometers per hour Rotation Animation Day and Night Song

Revolution The movement of one object around another object l Earth travels (revolves) around the sun l One complete revolution around the sun equals a year l It is a curved path (elliptical) followed by Earth as it moves around the Sun l Earth’s orbit is about 365 ¼ days (Leap year every four years)

Revolution

Now You Try! l Stand in place, and make one complete turn (You have just rotated) l Take a trip around your chair (You have just revolved l Do you think you can rotate and revolve at the same time? Try it now!

l Think about what a spinning top, a race car on an oval track, and a globe have in common

Turn to your neighbor and explain… What is the difference between Earth’s rotation and Earth’s revolution?

Earth in Space Earth rotates On its axis causing Day and night revolves Around the sun causing Years

So now you understand day and night – What about seasons? A Year in 40 seconds

Tilt A Whirl! l Earth has seasons because its axis is tilted as it revolves around the sun l If Earth’s axis were straight up and down, temperatures would remain constant year round (no seasons)

Seasons • • Seasons are caused by the tilt in Earth’s axis The tilt causes uneven heating by the sun (seasons)

Why is it warmer near the equator than near the poles? l At the equator - sunlight hits Earth’s surface more directly l Near the north and south poles - sunlight hits Earth’s surface at an angle (energy from the sun is spread out over a greater area)

The Earth’s Tilt The Earth's axis is tilted by 23. 5°

Earth’s axis always points in same direction (towards Polaris - the North Star)

Earth’s Tilted Axis l Earth’s axis is tilted away from the sun for part of the year and toward the sun for part of the year l l When tilted toward the sun – summer When tilted away from the sun - winter Note: Summer and winter are not affected by changes in Earth’s distance from the sun.

Summer in the Northern Hemisphere

Winter in the Northern Hemisphere

As the Earth moves around the Sun, this axis always stays pointing in the same direction.

Look at the direction of the axis during each season.

Direct vs. Indirect Light ct Indire t Direc

l When the northern hemisphere is leaning away from the sun, the rays coming from it hits this part of the Earth at a smaller (slanted) angle compared to other parts of the world l These are called indirect rays l Indirect rays - same amount of energy spread over a larger area of the earth therefore it receives less energy (heat)

Winter Sun (Indirect) Summer Sun (Direct)

Winter Sun (Indirect) Summer Sun (Direct)

Seasons l l Direct sunlight gets more heating Indirect sunlight gets less heating

Misconception Alert! l l Seasons are NOT caused by the changing distance the Earth is from the Sun. The Earth travels in an elliptical orbit, so the distance does vary – but not enough to cause the change in temperature associated with seasons!

When the southern hemisphere is experiencing summer, the northern hemisphere has winter (what do you know about Australia? )

6 months later, the situation reverses, and it is now winter in the southern hemisphere since that part of the earth is now leaning away from the sun

The energy that hits the Earth by the Sun changes over of the year The angle the Sun is above the horizon determines how much heat and light strike each square meter of ground

This means that in summer, the ground receives more energy (more heat) per square meter than in the winter. More energy is received by the ground during the summer (high temperatures) and less energy during the winter (lower temperatures).

Sun’s Angle Analogy l If you had $100. 00 to divide among 50 people what would each person get? l If you had the same $100. 00 to divide among 100 people what would each person get? l If you had the same $100. 00 to divide among 200 people, what would each person get?

Sun’s Angle = money Think of the money as the sun’s power l The sun always shines with the same amount of power, just like the $100. l If you had to spread the power over a larger area, there would be less power (heating) to go around on that area on Earth. l Just like there is less money for each person if the number of people grows. l

Changes in the Sun’s Angle l Summer l l l Sun is more directly overhead Sun’s energy is concentrated Winter l l The sun is less directly overhead Sun’s energy is less concentrated

Seasons and Earth’s Tilt

Seasons Question… l The amount of energy is always the same, so why do we have seasons? l First reason: the earth is tilted, what’s the second reason?

Big Idea: The seasons are the result of: 1) the tilt of the Earth's axis, and 2) revolution around the sun l If the tilt of the Earth's axis was 0° there would be no difference in how the rays from the sun hit its different regions (there would be no seasons)

Review Look closely at where the Sun is hitting the Earth during each season: http: //Search. Lycos. com/setup. asp? r=5&src=clear 2&query=weather+savvy

Solstice: Either of the two times in the year, the summer solstice and the winter solstice, when the sun reaches its highest or lowest point in the sky at noon, marked by the longest and shortest days.

Make a quick T chart in your notes Winter Solstice Summer Solstice

Winter Solstice • The northern hemisphere is pointed furthest away from the sun • The sun is directly over the Tropic of Capricorn • The shortest day of the year in the northern hemisphere

Summer Solstice • The northern hemisphere is pointed furthest toward the sun • The sun is directly over the Tropic of Cancer • The longest day of the year in the northern hemisphere

Solstices l l l On two days each year, the noon sun is overhead at either 23. 5° S or 23. 5° N – solstices. Winter Solstice l 23. 5° S l in the northern hemisphere l December 21 st l shortest day of the year Summer Solstice l 23. 5° N l in the northern hemisphere l June 21 st l Longest day of the year

Equinox l Equinox: the date (twice each year) at which the sun crosses the equator, therefore day and night are of equal length (about September 22 and March 20).

Make a quick T chart in your notes Spring Equinox Fall Equinox

Spring and Fall Equinox • Vernal (spring) and autumnal (fall) equinox - the sun is directly over the equator • Days and nights are equal in length

Earth in March and September Equinox (means - Equal night) l Halfway between the solstices, neither hemisphere is tilted toward or away from the sun l The noon sun is directly overhead at the equator

Vernal (Spring) Equinox l March 21 st l Marks the beginning of spring in the northern hemisphere

Autumnal Equinox l September 23 rd l Marks the beginning of fall in the northern hemisphere

Equinoxes and Solstices

Videos https: //www. youtube. com/watch? v=p 6 Tz 836 Avh 4 Seasons Animation