WEBVTT - Is there an easy way to understand how time zones work?

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<v Speaker 1>Welcome to brain Stuff from house stuff works dot com

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<v Speaker 1>where smart happens. Hi Am Marshall Brain with today's question,

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<v Speaker 1>is there an easy way to understand how time zones work?

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<v Speaker 1>In January, people have a special interest in time zones.

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<v Speaker 1>That's because the shouting of Happy New Year happens at

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<v Speaker 1>midnight in your local time zone. Meanwhile, other time zones

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<v Speaker 1>either have already celebrated the new year or they're sitting

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<v Speaker 1>around waiting to do it. So cities in New Zealand

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<v Speaker 1>celebrate New Year's Day first, followed by cities in Japan, Australia, Russia, China,

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<v Speaker 1>and India, followed by cities in Europe and Africa, followed

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<v Speaker 1>by cities in North and South America, and then ending

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<v Speaker 1>on islands out in the Pacific Ocean like Hawaii and

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<v Speaker 1>finally Samoa. There are four separate time zones, so there

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<v Speaker 1>are twenty four separate times when balls drop, Happy New Year,

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<v Speaker 1>gets shouted, and people engage in flagrant public displays of

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<v Speaker 1>affection and intoxication. So let's start at the beginning. Why

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<v Speaker 1>do we have time zones? Keep in mind that there's

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<v Speaker 1>another way we could do this. We could have a

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<v Speaker 1>single time that holds true all over the planet. When

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<v Speaker 1>it's noon in Moscow, it could also be noon in London,

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<v Speaker 1>New York, and Los Angeles. The problem is that people

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<v Speaker 1>really don't like that. People much prefer for it to

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<v Speaker 1>be noon when the sun reaches its peak in the sky.

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<v Speaker 1>In order for it to be noon when the sun

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<v Speaker 1>reaches its peak, everybody needs to set their time according

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<v Speaker 1>to the sun. And this is how things used to be.

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<v Speaker 1>It used to be that there were no clocks. People

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<v Speaker 1>use things like sun dials. Then there were clocks, but

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<v Speaker 1>only the rich people could afford them because they were

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<v Speaker 1>really expensive. So a town would have a central clock

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<v Speaker 1>tower with bells loud enough to be heard all over town,

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<v Speaker 1>and the clock keeper would set the clock according to

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<v Speaker 1>the sun. This system worked well until trains started to

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<v Speaker 1>move quickly from town to town. In order to run

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<v Speaker 1>a punctual train schedule, all the towns needed to have

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<v Speaker 1>a coordinated time system rather than setting their clocks loosely

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<v Speaker 1>according to the sun zenith. So the idea of time

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<v Speaker 1>zones was created to help keep people from missing their trains. Today,

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<v Speaker 1>the world has twenty four time zones, with all the

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<v Speaker 1>clocks in the same time zone displaying the same time,

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<v Speaker 1>but it can still be confusing, especially if you're trying

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<v Speaker 1>to schedule a phone call with someone in China or Australia.

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<v Speaker 1>How do you make sense of this? The easiest way

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<v Speaker 1>is to get out a globe and a table lamp.

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<v Speaker 1>The table lamp represents the sun position your globe, so

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<v Speaker 1>that England is pointing toward the sun. In this model,

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<v Speaker 1>it's now high noon in England. For historical reasons, the

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<v Speaker 1>zero degree longitude line runs through Greenwich, England. This is

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<v Speaker 1>called the prime meridian, and this place on the globe

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<v Speaker 1>is also known as GMT plus zero or a Greenwich

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<v Speaker 1>meantime or UTC plus zero, where UTC stands for coordinated

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<v Speaker 1>Universal Time. So look at your globe looking down at

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<v Speaker 1>the north pole. Imagine the globe divided into twenty four

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<v Speaker 1>pie shaped slices. Each slice is a time zone. It's

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<v Speaker 1>high noon in the England time zone. From the vantage

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<v Speaker 1>point of the North Pole. The Earth spins counterclockwise. That's

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<v Speaker 1>why the sun rises in the east and sets in

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<v Speaker 1>the west. In the slice immediately adjacent to England on

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<v Speaker 1>the left, it's one PM or UTC plus one. In

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<v Speaker 1>the slice immediately adjacent to England on the right, it's

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<v Speaker 1>eleven am or UTC minus one. As the Earth rotates counterclockwise.

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<v Speaker 1>In one hour, it will become high noon in the

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<v Speaker 1>slice immediately adjacent to England on the right. Five hours

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<v Speaker 1>after its high noon in England, the Earth will have

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<v Speaker 1>rotated enough for it to be high noon on the

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<v Speaker 1>East coast of the United States. This is referred to

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<v Speaker 1>as U t C minus five. The central time zone

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<v Speaker 1>of the U S is ut C minus six, Mountain

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<v Speaker 1>and Pacific are U t C minus seven and UTC

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<v Speaker 1>minus eight, respectively. Hawaii is U t C minus ten,

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<v Speaker 1>and finally Samoa is U t C minus eleven. The

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<v Speaker 1>International date Line is on the opposite side of the

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<v Speaker 1>globe from England, over near New Zealand. This first time

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<v Speaker 1>zone is ut C plus twelve. This is the first

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<v Speaker 1>time zone to see January one. Each new day starts

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<v Speaker 1>in the time zone adjacent to the International date Line

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<v Speaker 1>twelve hours before it's midnight in England, it's midnight in Auckland,

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<v Speaker 1>New Zealand, eleven hours after it's midnight in England, and

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<v Speaker 1>it's midnight in Samoa. Then the Earth rotates past the

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<v Speaker 1>International dateline. It becomes January second in New England, and

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<v Speaker 1>the cycle repeats. When you imagine how the globe rotates

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<v Speaker 1>with respect to the Sun like this, it's easy to

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<v Speaker 1>keep track of the time zones. Be sure to check

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<v Speaker 1>out our new video podcast, Stuff from the Future. Join

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