Is our climate headed for a mathematical tipping point? - Victor J. Donnay

我們的氣候正在走向數學所提及的混亂嗎?-維克多 J. 唐尼

188,731 views

2014-10-23 ・ TED-Ed


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Is our climate headed for a mathematical tipping point? - Victor J. Donnay

我們的氣候正在走向數學所提及的混亂嗎?-維克多 J. 唐尼

188,731 views ・ 2014-10-23

TED-Ed


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譯者: 葉 Yah 宇倫 審譯者: 瑞文Eleven 林Lim
00:07
For most of us, two degrees Celsius is a tiny difference in temperature,
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對我們大多數人來說, 2°C的溫差是一個很小的變化
00:11
not even enough to make you crack a window.
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還不足以讓你開或關閉窗戶
00:14
But scientists have warned that as CO2 levels in the atmosphere rise,
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但科學家警告 隨着大氣中二氧化碳濃度升高
00:18
an increase in the Earth's temperature by even this amount
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即使地球僅升高一點點溫度
00:22
can lead to catastrophic effects all over the world.
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也可能導致全球災難性的影響
00:26
How can such a small measurable change in one factor
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這樣一個可測因素的微小變化
00:29
lead to massive and unpredictable changes in other factors?
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是如何導致其他因素大規模 和不可預測的變化呢?
00:34
The answer lies in the concept of a mathematical tipping point,
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答案出現在數學裡 臨界點這個概念上
00:38
which we can understand through the familiar game of billiards.
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我們可以透過熟悉的 桌球中理解
00:42
The basic rule of billiard motion is
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桌球運動的基本運動規律是
00:44
that a ball will go straight until it hits a wall,
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球會沿著直線運動, 直到它碰壁
00:47
then bounce off at an angle equal to its incoming angle.
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接着它以與入射角相同的角度彈開
00:51
For simplicity's sake, we'll assume that there is no friction,
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爲了簡化,我們假設沒有摩擦
00:54
so balls can keep moving indefinitely.
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所以球運動的規則 就有很多不確定性
00:56
And to simplify the situation further,
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為了使情況更加簡單
00:58
let's look at what happens with only one ball on a perfectly circular table.
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我們來看看 一張圓桌上的球會怎樣運動
01:04
As the ball is struck and begins to move according to the rules,
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當球被擊中並開始按規律運動
01:07
it follows a neat star-shaped pattern.
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會形成平滑的星型圖案
01:10
If we start the ball at different locations,
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如果我們在不同的位置或者角度擊球
01:12
or strike it at different angles, some details of the pattern change,
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圖案的一些細節會有所變化
01:16
but its overall form remains the same.
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但整體的形狀保持一致
01:19
With a few test runs, and some basic mathematical modeling,
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經過幾次測試和一些基本的 數學模型分析後
01:22
we can even predict a ball's path before it starts moving,
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僅僅依靠簡單的擊球條件
01:26
simply based on its starting conditions.
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我們就能在球運動前 便預知它的軌跡
01:28
But what would happen if we made a minor change
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但如果我們對桌子做一點微小的變動
01:31
in the table's shape by pulling it apart a bit,
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會發生什麼事呢?
01:34
and inserting two small straight edges along the top and bottom?
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我們將桌子向左右拉長
01:39
We can see that as the ball bounces off the flat sides,
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會看到球由較平整的邊彈出
01:42
it begins to move all over the table.
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並開始在整張桌子上運動
01:44
The ball is still obeying the same rules of billiard motion,
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球仍遵循桌球運動的規律
01:48
but the resulting movement no longer follows any recognizable pattern.
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但最終的運動軌跡 不再是我們認識的圖形
01:52
With only a small change to the constraints
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在整個系統運行的過程中
01:55
under which the system operates,
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我們只改變一點點的約束條件
01:57
we have shifted the billiard motion
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我們就能改變桌球的運動
01:58
from behaving in a stable and predictable fashion,
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從可以預測的,穩定的運動
02:01
to fluctuating wildly,
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到混亂的、不受控制的運動模式
02:03
thus creating what mathematicians call chaotic motion.
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產生了數學家所說的混沌運動
02:08
Inserting the straight edges into the table acts as a tipping point,
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在(圓形)桌子上放置兩條直邊作為臨界點
02:11
switching the systems behavior from one type of behavior (regular),
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將這個系統的規律運動
02:16
to another type of behavior (chaotic).
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變成混沌運動
02:20
So what implications does this simple example have for the much more complicated
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而對於複雜的地球環境氣候問題
02:24
reality of the Earth's climate?
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我們能在這簡單的例子 得到甚麼想法呢?
02:26
We can think of the shape of the table as being analogous to the CO2 level
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我們可以把桌子的形狀 類比成二氧化碳的濃度
02:30
and Earth's average temperature:
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或是地球的平均溫度
02:32
Constraints that impact the system's performance
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在這桌球運動或說是 氣候變化的模型中
02:35
in the form of the ball's motion or the climate's behavior.
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這兩者都是影響 這個系統表現的條件
02:38
During the past 10,000 years,
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在過去的一萬年裡
02:41
the fairly constant CO2 atmospheric concentration of
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為了確保整個系統保持穩定
02:44
270 parts per million kept the climate within a self-stabilizing pattern,
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二氧化碳在大氣中的含量維持在 百萬分之兩百七十左右
02:50
fairly regular and hospitable to human life.
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這對於人類的生活相當規律和適宜
02:53
But with CO2 levels now at 400 parts per million,
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但現在二氧化碳含量已達到了 百萬分之四百左右
02:57
and predicted to rise to between 500 and 800 parts per million
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下個世紀甚至可能達到五百至八百
03:01
over the coming century, we may reach a tipping point where
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我們可能就達到"臨界點"了
03:04
even a small additional change in the global average temperature
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那時,在全球平均溫度範圍中一個 小小的額外變化
03:07
would have the same effect as changing the shape of the table,
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與改變桌子的形狀有同樣的影響
03:11
leading to a dangerous shift in the climate's behavior,
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會導致危險的氣候變遷
03:14
with more extreme and intense weather events,
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出現更難預測、極端且劇烈的氣候問題
03:16
less predictability, and most importantly, less hospitably to human life.
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更重要的是,不再適合人類生活
03:21
The hypothetical models that mathematicians study in detail
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數學家詳細地研究這些假設模型
03:25
may not always look like actual situations,
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可能與實際的情況有所不同
03:28
but they can provide a framework and a way of thinking
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但它們可以提供我們 思考的框架和方式
03:31
that can be applied to help understand the more complex problems of the real world.
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這些模型可以幫助理解真實世界中 更複雜的問題
03:36
In this case, understanding how slight changes
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在這個例子中, 理解在系統中微小的變化
03:38
in the constraints impacting a system can have massive impacts
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是如何導致一個龐大的問題
03:42
gives us a greater appreciation for predicting the dangers
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使我們具有更多無法憑感官
03:46
that we cannot immediately percieve with our own senses.
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而預測危險的能力
03:49
Because once the results do become visible, it may already be too late.
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因爲當我們看見結果時, 為時已晚
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