The History of Keeping Time Karen Mensing

We check the time every day, all day long.

But did you ever wonder - where did telling time come from?

Why does it matter what time it is?

Who determined the clock

and why in the world are there so many different time zones?

The first form of telling time was the sundial

and the earliest sundials known from the archaeological record

are obelisks from nearly 5,000 years ago.

Sundials indicate the time by casting a shadow

onto a surface.

The object that casts the shadow is a stick in the center known as a gnomon.

A well-constructed sundial can measure time with remarkable accuracy,

and sundials were used to monitor the performance of clocks until the modern era.

But sundials have their limitations too.

Obviously they require the sun to shine,

so they don’t work at all during the night when it’s dark.

Many different devices have been used over the years to estimate the passage of time:

candles and sticks of incense that burn down at fairly predictable speeds

have been used, along with the hourglass.

Hourglasses are devices in which fine sand

pours through a tiny hole at a constant rate

and indicates a predetermined passage of an arbitrary period of time.

The origin of the hourglass is uncertain,

although beginning in the 14th century, the hourglass was used commonly,

especially on board ships.

The motion of the boat on the water did not affect the hourglass,

unlike other time-measuring devices.

The mechanical clock was invented in the 13th century

which sparked a big change in traditional timekeeping methods.

This modern clock relied on the swing of a pendulum

or the vibration of a quartz crystal, which was far more accurate than sand

or candles.

Today, the basis for scientific time

is a continuous count of seconds

based on atomic clocks all around the world, known as the international atomic time.

Why does it matter that we keep track of time?

Well, time regulates our daily lives

and makes it possible to accurately communicate with people

all over the world.

Without a time system, we would have many challenges in farming,

social structures, communication, and business.

Take the American railroad system, for example.

In the mid-19th century, each railroad used its own standard time

generally based on the local time of its headquarters,

and the railroad’s train schedules were published using its own time.

Some major railroad junctions

served by several different railroads

had a separate clock for each railroad, each showing a different time.

The distance between New York and Boston is about 2 degrees, or 8 minutes,

which can be the difference between making or missing your train connection.

If the difference between New York and Boston

is 8 minutes, imagine the difference

between Boston and Australia.

The use of time zones irons out these differences

and makes communication significantly smoother.

A time zone is a region on earth

that has a uniform standard time.

There are 40 time zones on land

because the earliest and latest time zones

are 26 hours apart.

Any given calendar date exists at some point

on the globe for 50 hours.

So the next time someone asks you

“What time is it?”

Your answer may be a whole lot more complicated than it used to be.

我们每天都检查时间,整天。

但是你有没有想过——时间是从哪里来的?

为什么时间很重要?

谁决定了时钟

,为什么世界上有这么多不同的时区?

第一种显示时间的形式是日晷

,考古记录中已知的最早的日晷

是近 5000 年前的方尖碑。

日晷通过在表面上投射阴影来指示时间

投射阴影的物体是中心的一根棍子,称为晷针。

一个结构良好的日晷可以非常准确地测量时间,

直到现代,日晷一直被用来监控时钟的性能。

但日晷也有其局限性。

显然,它们需要阳光照射,

所以它们在黑暗的夜晚根本不工作。

多年来,人们使用了许多不同的设备来估计时间的流逝:

蜡烛和香柱以相当可预测的速度燃烧

,还有沙漏。

沙漏是一种装置,其中细沙

以恒定的速度从一个小孔中倾泻而出,

并指示任意时间段的预定流逝。

沙漏的起源是不确定的,

尽管从 14 世纪开始,沙漏就被普遍使用,

尤其是在船上。 与其他时间测量设备不同

,船在水面上的运动不会影响沙漏

机械钟发明于 13 世纪

,引发了传统计时方法的重大变革。

这种现代时钟依靠钟摆的摆动

或石英晶体的振动,比沙子或蜡烛要准确得多

今天,科学时间的基础是

基于世界各地的原子钟连续计算秒数,称为国际原子时。

为什么我们跟踪时间很重要?

好吧,时间调节着我们的日常生活

,使我们可以与世界各地的人们进行准确的交流

如果没有时间系统,我们将在农业、

社会结构、沟通和商业方面面临许多挑战。

以美国铁路系统为例。

19世纪中叶,每条铁路都使用自己的标准时间,

一般以总部当地时间为准

,铁路的列车时刻表也使用自己的时间发布。

由几条不同铁路服务的一些主要铁路枢纽

对每条铁路都有一个单独的时钟,每个时钟显示不同的时间。

纽约和波士顿之间的距离约为 2 度,即 8 分钟,

这可能决定您是否搭乘火车。

如果纽约和波士顿之间的差异

是 8 分钟,想象一下

波士顿和澳大利亚之间的差异。

时区的使用消除了这些

差异,并使沟通变得更加顺畅。

时区是地球

上具有统一标准时间的区域。

陆地上有 40 个时区,

因为最早和最新的时

区相隔 26 小时。

任何给定的日历日期在地球上的某个时间点存在

50 小时。

所以下次有人问你

“现在几点了?”

你的答案可能比以前复杂得多。