lesson 5 motions of the earth

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MOTIONS of the Earth Click here to watch the video! © Jamaica C. Olazo

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Page 1: Lesson 5 Motions of the Earth

MOTIONSof the Earth

Click here to watch the video!

© Jamaica C. Olazo

Page 2: Lesson 5 Motions of the Earth

Basic Understandings

Rotation –

the Earth spins on an imaginary line called ‘axis ‘ from east to west direction.

“The Earth spins on its axis once every 24 hours or 1 day.”

Major Motions of the Earth

Revolution –

movement around the Sun in an elliptical orbit.

Complete r = 365 ¼ days.

Speed = 29.8 km/s

© Jamaica C. Olazo

Page 3: Lesson 5 Motions of the Earth

The Earth is farthest from the Sun at aphelion on July 3 or 4 at approx. 152.1 million kilometers.

The Earth is nearest from the Sun at perihelion on January 3 or 4 at approx. 147.2 million kilometers.

Basic Understandings

94,500,000 miles

93,000,000 miles

© Jamaica C. Olazo

Page 4: Lesson 5 Motions of the Earth

EARTH'Smotion

around the Sun, not as

simple as you thought.

Click here to watch the video!

© Jamaica C. Olazo

Page 5: Lesson 5 Motions of the Earth

The four important positions of the Earthwith respect to its revolution around the Sun.

© Jamaica C. Olazo

Page 6: Lesson 5 Motions of the Earth

Seasonal Changes

-are caused by

the tilting of the

Earth and its

revolution around the Sun.

These bring

about the

variations in

the lengths of day and night.

© Jamaica C. Olazo

Page 7: Lesson 5 Motions of the Earth

The Earth’s Tilted Axis and Seasonal Changes

As the Earth rotates and

revolves around the Sun, its

axis tilts at an average of 23.5 °from the vertical line.

© Jamaica C. Olazo

Page 8: Lesson 5 Motions of the Earth

Seasonal Changes

When the longest

days and shortest

nights occur in Northern Hemisphere.

Summer

Warm weather

-when the North Pole

Is directly tilted toward the Sun.

© Jamaica C. Olazo

Page 9: Lesson 5 Motions of the Earth

Seasonal Changes

-when the North

Pole is tilted awayfrom the Sun.

Winter

Cool weather

Earth will experience

the shortest day and

longest night of the year.

© Jamaica C. Olazo

Page 10: Lesson 5 Motions of the Earth

Seasonal Changes

Days and nights are

equal all over the Earth.

Equinoxes

Equinox

- means equal day and night.

© Jamaica C. Olazo

Page 11: Lesson 5 Motions of the Earth

Seasonal Changes

It tells the time

when the Sun stops

its journey to the

north as it rises everyday.

Solstice

Solstice - means “Sun stops”.

© Jamaica C. Olazo

Page 12: Lesson 5 Motions of the Earth

The midnight sun is a natural phenomenon that occurs in the summer months

in places north of the Arctic Circle or south of the Antarctic Circle, when the sun remains visible at the local midnight.

Landof the

Midnight Sun

© Jamaica C. Olazo

Page 13: Lesson 5 Motions of the Earth
Page 14: Lesson 5 Motions of the Earth

The earth covers 360° in its 24-hour rotation. Thus, for every hour of rotation it covers 15 ° of longitude. This is the basis for determining time all over the globe.

Timeand

Standard Time Zones

Local Time -If we would base time on the Earth’s

rotation, covering 360° in a day, or

15° in an hour, or one degree every

four minutes, each meridian would

have its own time.

© Jamaica C. Olazo

Page 15: Lesson 5 Motions of the Earth

STANDARD TIME ZONES OF THE WORLD

The Earth was divided into 24 time zones, each zone one

hours apart, covering approximately 15° of longitude.

Page 16: Lesson 5 Motions of the Earth

STANDARD TIME ZONES OF THE WORLD

Therefore, the different places of the world have different

times based on the meridian passing through them.

Page 17: Lesson 5 Motions of the Earth

Not all countries, however, follow the standard time system.

© Jamaica C. Olazo

Page 18: Lesson 5 Motions of the Earth

Australia

Standard Time System

- was adapted based on the Greenwich Prime Meridian (0°) as agreed upon in an international conference held in Washington, D.C. in 1884.

Bigger countries

cover more than

one time zone.

© Jamaica C. Olazo

Page 19: Lesson 5 Motions of the Earth

When one travels around the

world, crossing boundaries and

going from one hemisphere to

another, it is important to take

note of time differences as well as

the change in dates upon

crossing the

International Date Line.

Page 20: Lesson 5 Motions of the Earth

Motions of the Earth

Revolution

Revolves around the sun.

Takes about a year or 365 ¼ days.

Causes changes in seasons.

Follows an elliptical orbit.

Rotation

Rotates on its axis.

Rotates for a period of 24 hours.

Causes night and day.

Rotates in an eastward direction.

© Jamaica C. Olazo

Page 21: Lesson 5 Motions of the Earth

North Pole is directly tilted toward the Sun.

It occurs every June 21 or 22.

Longest day and shortest night are experienced.

Vertical rays of the Sun strike the Tropic of Cancer.

Seasons and the Positions of the Earth around the Sun with reference to the Northern Hemisphere

Summer solstice

© Jamaica C. Olazo

Page 22: Lesson 5 Motions of the Earth

No pole is tilted toward the Sun.

It occurs every September 22 or 23.

Equal length of day and night is experienced.

Vertical rays of the Sun strike along the Equator.

Seasons and the Positions of the Earth around the Sun with reference to the Northern Hemisphere

Autumnal equinox

© Jamaica C. Olazo

Page 23: Lesson 5 Motions of the Earth

South pole is directly tilted toward the Sun.

It occurs every December 21 or 22.

Shortest day and longest night are experienced.

Vertical rays of the Sun strike the Tropic of Capricorn.

Seasons and the Positions of the Earth around the Sun with reference to the Northern Hemisphere

Winter solstice

© Jamaica C. Olazo

Page 24: Lesson 5 Motions of the Earth

No pole is tilted toward the Sun.

It occurs every March 21 or 22.

Equal length of day and night is experienced.

Vertical rays of the Sun strike along the equator.

Seasons and the Positions of the Earth around the Sun with reference to the Northern Hemisphere

Spring equinox

© Jamaica C. Olazo

Page 25: Lesson 5 Motions of the Earth

Mechanism of the Seasons

Click here to watch the video!

© Jamaica C. Olazo