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Why is summer warm and winter cold?

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By the end of this video, you'll know the real reason, and why the

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most popular answer is wrong.

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Many people think summer is warm because Earth is closer to the Sun.

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It sounds reasonable, but it's wrong.

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In fact, Earth is closest to the Sun in early January, right in the middle

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of the Northern Hemisphere's winter.

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Earth's orbit is almost a circle.

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At its closest, around January 3, Earth is about 147 million

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kilometres from the Sun.

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At its farthest, around July 4, it's about 152 million.

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That's only a 3% difference, far too small to explain the seasons.

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And if distance were the cause, both hemispheres would have

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summer at the same time.

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They don't.

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When it's summer in Canada, it's winter in Australia.

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Here's the real reason:

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Earth's axis is tilted about 23.4 degrees.

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As Earth orbits, the axis keeps pointing the same way in space,

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toward the North Star.

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So for half the year the Northern Hemisphere leans toward the Sun,

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and for the other half it leans away.

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Tilt changes two things.

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First, how directly sunlight hits the ground.

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A high Sun shines straight on, concentrating energy on a small

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area.

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A low Sun spreads the same beam over a much larger area, so each

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square metre gets less heat.

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Picture a flashlight pointed straight down versus at a steep angle.

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Second, how long the day lasts.

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The hemisphere tilted toward the Sun gets long days and short

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nights, so the ground has more hours to warm up and fewer to cool

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down.

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In Vancouver, a June day has about 16 hours of daylight.

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A December day has only about 8.

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Four moments mark the year.

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At the June solstice, around June 21, the north tilts most toward the

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Sun.

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At the September equinox, day and night are roughly equal

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everywhere.

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At the December solstice, the south leans in:

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summer in Australia, winter in Canada.

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And at the March equinox, it's equal again, and the cycle repeats.

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Location matters too.

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Near the equator, the Sun stays high all year and day length barely

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changes, so seasons are often defined by rainfall instead.

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Near the poles, tilt is extreme:

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in summer the Sun never sets, the midnight sun,

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and in winter it never rises, the polar night.

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So, seasons aren't about distance.

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Earth's tilted axis changes how directly sunlight strikes each

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hemisphere, and how many hours of daylight it gets.

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Tilt toward the Sun, and it's summer.

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Tilt away, and it's winter.
