The physics of surfing - Nick Pizzo

507,630 views ・ 2019-03-11

TED-Ed


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翻译人员: Aimee Zhou 校对人员: shuping Lai
00:07
Whether or not you realize it,
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不管你是否意识到,
00:08
as a surfer you’re a master of complicated physics.
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身为冲浪者,你实际是 一位精通复杂物理学的大师。
00:15
The science of surfing begins
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冲浪的科学始于
00:17
as soon as you and your board first hit the water.
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你和冲浪板触碰到水的一瞬间。
00:21
The board’s size and light construction help it displace a lot of water.
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冲浪板的面积和较轻的材质 能够使大量的水产生位移。
00:25
In turn, a buoyant force
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产生一股向上推起的浮力,
00:27
equal to the weight of the displaced water pushes up,
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与发生位移的水重量均等,
00:31
counteracting you and your board’s weight.
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可以抵消掉你与冲浪板的重量。
00:34
This lets you stay afloat while you wait to paddle for a wave.
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这使你在等待海浪的时候能够一直浮于海面。
00:38
And what exactly are you waiting for?
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那么你等待的究竟是什么呢?
00:40
The perfect wave, of course.
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当然是完美的海浪。
00:42
Like other waves in physics, ocean waves represent a transfer of energy.
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与物理学中其他的波浪一样, 海洋的波浪代表能量的转移。
00:49
Wind blowing across the ocean accelerates water particles near the surface,
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海风加速了水表的移动,
00:54
leading to the growth of ripples that become waves.
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产生波纹,最终形成海浪。
00:58
These deviations from the flat surface are acted upon by gravity,
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不再平静的海面会受到重力作用,
01:02
which tries to restore the surface to its original flat state.
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重力试图让海面恢复到原本的水平状态。
01:08
As the waves then move through the water,
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当海浪在不断移动,
01:10
particles push and pull on their neighbors through the wave induced pressure,
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水粒子互相挤压引起海浪内部的压力,
01:16
and this motion propagates energy through the water in unison with the wave motion.
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而这种运动通过水与波浪的同步运动传递能量。
01:22
The motion of these particles
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水粒子的运动,
01:23
is much more limited than the overall motion of the waves.
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相比波浪的整体运动是很受限的。
01:27
Near the shore,
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靠近岸边,
01:28
the shallower seafloor constrains the motion of the waves
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相较于广阔的大海,
01:32
to occur in a more limited region than out at sea,
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浅海区域海浪的运动在一定范围内受限,
01:35
concentrating the wave energy near the surface.
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将波浪的能量集中在表面。
01:38
If the topography of the shoreline is even and smooth,
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如果海岸线的地形平整光滑,
01:42
this will refract the waves to become more
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海浪会发生折射,
01:44
parallel to the shore as they approach.
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在靠近海岸时与海岸线更平行。
01:48
This is the crucial moment.
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关键的时刻来了。 当海浪逐渐靠近,
01:50
As the wave gets near,
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01:51
you quickly pivot your board in the same direction as the wave
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你朝着与海浪相同的方向调转冲浪板,
01:55
and paddle to match its speed.
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尽力划动,赶上海浪的速度。
01:58
Your board forms an angle with the water,
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你的冲浪板与水形成一个角度,
02:01
and this creates a dynamic pressure on the bottom of it,
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在底部产生压力,
02:05
forcing you and your board out of the water,
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使得你和冲浪板离开水面,
02:07
to skim along the surface.
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在表面飞快行进。
02:09
At the same time,
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同时,
02:11
your increased forward momentum makes you more stable,
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不断增强的前进动力使你更稳定,
02:15
allowing you to stand up and surf along the wave.
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让你能够站起,随波逐浪滑行。
02:19
Now you’ve caught the wave,
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现在你已追到了浪,
02:20
and are riding along its front face parallel to the shoreline.
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开始沿着与海岸线平行的方向前行。
02:24
Fins on the surfboard allow you to alter your speed and direction
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冲浪板的舵通过重置你的着力点,
02:29
by repositioning your weight.
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让你可以改变速度和方向。
02:30
Above you is the wave’s crest,
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在你的上方,是波峰,
02:33
where the water particles are undergoing their greatest acceleration.
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波峰处的水粒子在以它们最大速度运动,
02:37
That forces them to move faster than the underlying wave,
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迫使它们比下方的海浪移动得更快,
02:41
so they shoot ahead before falling under gravity’s influence.
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在受到重力影响掉落之前,它们飞速向前。
02:45
This forms the waves’ characteristic curls, or jets,
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这形成了海浪的特征,卷浪,或称喷浪,
02:49
as they break along the shore.
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因为它们会沿着海岸溃散。
02:51
Sometimes, the curl might completely enclose part of the wave,
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有时,这种卷浪会完全围住一些海浪,
02:55
forming a moving tube of water known as the barrel.
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使水形成运动中的管道,形状像桶一样,
02:59
Because of irregularities in the seafloor and the swell itself,
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由于海底的不规则构造和高低起伏,
03:03
few barrels last as long as the legendary 27-second ride off the coast of Namibia.
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几乎没有比纳米比亚海岸 那次传奇的27秒更持久的卷浪。
03:09
But many who manage to get barreled
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但有不少驾驭过卷浪的人,
03:11
have said they feel time passing differently inside,
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他们描述到,身处于浪之中, 感觉时间流逝的速度都发生了变化,
03:15
making it one of the most magical experiences a surfer can have.
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这是冲浪者专属的最神奇的体验之一。
03:20
Of course,
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当然,
03:21
not all beaches are created equal.
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海滩不尽相同。
03:23
Offshore underwater canyons or rock formations
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一些地方的沿岸海底的岩石和峡谷地形构造,
03:27
in certain locations like Nazare, Portugal or Mavericks, California
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比如葡萄牙的纳扎尔、加利福尼亚州的半月湾,
03:31
refract the incoming wave energy into a single spot,
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能够将海浪的能量折射到一个单点上,
03:35
creating massive waves sought by surfers worldwide.
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造就全世界冲浪者心向往之的巨大海浪。
03:40
And some of these waves travel for more than a week,
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有些海浪的旅程长达一星期,
03:43
with swells originating more than 10,000 kilometers away from shore.
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到达一万公里以外的地方。
03:48
Waves surfed in sunny California
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在加州的阳光海岸冲的浪,
03:50
may have originated in the stormy seas near New Zealand.
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可能来自于新西兰海域的汹涌波涛。
03:55
So while you may not be thinking about weather patterns in the South Pacific,
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你可能根本不会关心南太平洋的天气状况、
03:59
tectonic geology, or fluid mechanics,
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构造地质学或流体力学,
04:02
the art of catching the perfect wave relies on all these things and more.
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但完美的冲浪艺术 确实依赖于这些及其他的因素。
04:08
And the waves we surf, created by wind,
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风造就了使我们冲浪的海浪,
04:10
are just one visible part of the continuous oscillation of energy
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仅仅是能量的其中一个可见部分而已,
04:15
that has shaped our universe since its very beginning.
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能量振动持续塑造着我们的宇宙,从开始到现在。
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