Why the Arctic is climate change's canary in the coal mine - William Chapman

为何北极是气候变化的预警钟 | 威廉•查普曼

212,575 views

2015-01-22 ・ TED-Ed


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Why the Arctic is climate change's canary in the coal mine - William Chapman

为何北极是气候变化的预警钟 | 威廉•查普曼

212,575 views ・ 2015-01-22

TED-Ed


请双击下面的英文字幕来播放视频。

翻译人员: Aili Liang 校对人员: Sherry Chen
00:06
The area surrounding the North Pole
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北极圈附近的冰封世界
00:09
may seem like a frozen and desolate environment where nothing ever changes.
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似乎是一成不变的荒凉之地
00:14
But it is actually a complex and finely balanced natural system,
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但其实那里的自然系统, 复杂、精妙,而又平衡
00:19
and its extreme location makes it vulnerable to feedback processes
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它特殊的位置使得它对气候非常敏感
00:23
that can magnify even tiny changes in the atmosphere.
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微小的气候变化都可能被放大
00:27
In fact, scientists often describe the Arctic as the canary in the coal mine
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事实上,科学家常把北冰洋 形容为“矿井中的金丝雀”
(金丝雀对瓦斯非常敏感, 曾被矿工用于预警)
00:32
when it comes to predicting the impact of climate change.
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因为北冰洋对气候变化也非常敏感
00:36
One major type of climate feedback involves reflectivity.
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气候反馈的一项重要指标是反射性
00:39
White surfaces, like snow and ice,
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像冰雪这样的浅色地表
00:41
are very effective at reflecting the sun's energy back into space,
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会有效地把大部分阳光 反射回宇宙空间之中
00:46
while darker land and water surfaces absorb much more incoming sunlight.
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而土地、海洋这样的深色区域 则更擅于吸收阳光
00:51
When the Arctic warms just a little, some of the snow and ice melts,
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当北冰洋稍稍变暖,少量冰雪消融
00:55
exposing the ground and ocean underneath.
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暴露出下面的泥土或者海洋
00:58
The increased heat absorbed by these surfaces causes even more melting,
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吸收更多阳光热量, 导致更多冰雪消融
01:01
and so on.
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循环往复
01:03
And although the current situation in the Arctic follows the warming pattern,
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现在的北冰洋正处于这样的变暖模式
01:07
the opposite is also possible.
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但变冷的模式亦有可能
01:09
A small drop in temperatures would cause more freezing,
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温度稍稍降低,会使海水更多结冰
01:12
increasing the amount of reflective snow and ice.
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冰雪增加了,就会反射更多阳光
01:15
This would result in less sunlight being absorbed,
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吸收的阳光则会变少
01:18
and lead to a cycle of cooling, as in previous ice ages.
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从而持续的变冷,冰河时代就是如此
01:22
Arctic sea ice is also responsible for another feedback mechanism
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北冰海冰对另一种对气候的反馈
01:26
through insulation.
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与冰雪的隔离作用有关
01:28
By forming a layer on the ocean's surface,
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通过在北冰洋表面形成一层冰层
01:30
the ice acts as a buffer between the frigid arctic air
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冰在寒冷的空气 和相对温暖的海水中间
01:33
and the relatively warmer water underneath.
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形成了一个缓冲区
01:36
But when it thins, breaks, or melts in any spot,
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如果冰层变薄、破裂、融化
01:39
heat escapes from the ocean,
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海水中的热量散发到空气中
01:41
warming the atmosphere and causing more ice to melt in turn.
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使空气变热,从而更多冰层融化
01:45
Both of these are examples of positive feedback loops,
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这两个都是正反馈循环
01:48
not because they do something good,
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”正反馈“并非意味着这是好事
01:50
but because the initial change is amplified in the same direction.
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而是指变化会往相同的方向 不断强化自身
01:54
A negative feedback loop, on the other hand,
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而负反馈则相反
01:57
is when the initial change leads to effects
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是指初始的改变
01:59
that work in the opposite direction.
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会导致后续的改变向相反方向进行
02:02
Melting ice also causes a type of negative feedback
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冰雪的融化也会导致负反馈
02:05
by releasing moisture into the atmosphere.
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融化后的冰雪会释放 更多水汽到大气中
02:08
This increases the amount and thickness of clouds present,
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这使得云层变厚
02:12
which can cool the atmosphere by blocking more sunlight.
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云层遮挡住阳光,大气就会变凉
02:15
But this negative feedback loop is short-lived,
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但这种负反馈循环非常短暂
02:18
due to the brief Arctic summers.
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因为北冰洋的夏天很短
02:20
For the rest of the year, when sunlight is scarce,
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在一年中其他的日子里,缺少阳光
02:22
the increased moisture and clouds
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增加的云量
02:24
actually warm the surface by trapping the Earth's heat,
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通过吸收地球的热量, 反而使地表变暖
02:28
turning the feedback loop positive for all but a couple of months.
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这几个月的负反馈又变成了正反馈
02:32
While negative feedback loops encourage stability
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负反馈导致稳定性
02:35
by pushing a system towards equilibrium,
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会把系统的变化推回原来的平衡点
02:38
positive feedback loops destabilize it by enabling larger and larger deviations.
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正反馈则会导致更大的变化, 破坏稳定性
02:43
And the recently increased impact of positive feedbacks
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最近,正反馈的影响越来越大
02:47
may have consequences far beyond the Arctic.
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可能波及北冰洋之外的世界
02:50
On a warming planet,
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在变暖的星球上
02:51
these feedbacks ensure that the North Pole warms at a faster rate than the equator.
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正反馈使极地变热的速度快于赤道
02:57
The reduced temperature differences between the two regions
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两个区域之间的温差减小
03:00
may lead to slower jet stream winds
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会使喷射气流的速度减弱
03:02
and less linear atmospheric circulation in the middle latitudes,
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中纬度上的线性大气环流亦会减弱
03:06
where most of the world's population lives.
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而世界上大部分人口 正居住于中纬度地区
03:09
Many scientists are concerned that shifts in weather patterns
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许多科学家在关注 这种气候模式的变化
03:12
will last longer and be more extreme,
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会持续更长时间, 变造成更极端影响
03:14
with short term fluctuations becoming persistent cold snaps,
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短期的气候波动会变成持续的寒流
03:18
heat waves, droughts and floods.
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热浪、干旱、洪水
03:22
So the Arctic sensitivity doesn't just serve as an early warning alarm
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北冰洋对气候的敏感性 并非仅是一种警告
03:25
for climate change for the rest of the planet.
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提醒我们注意地球上 其它地方的气候变化
03:28
Its feedback loops can affect us in much more direct and immediate ways.
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它的反馈作用,会以更直接 更迅速的方式影响到我们
03:32
As climate scientists often warn,
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正如气候学家们所警告的
03:34
what happens in the Arctic doesn't always stay in the Arctic.
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北冰洋的变化将波及全球
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