Climate change Earths giant game of Tetris Joss Fong

To understand climate change,

think of the game “Tetris.”

For eons, Earth has played a version of this game with blocks of carbon.

They enter the atmosphere as carbon dioxide gas from volcanoes,

decaying plant matter,

breathing creatures

and the surface of the sea.

And they leave the atmosphere when they’re used by plants during photosynthesis,

absorbed back into the ocean,

or stored in soil and sediment.

This game of Tetris is called the carbon cycle,

and it’s the engine of life on Earth.

What’s the connection to climate?

Well, when that carbon dioxide is in the air,

waiting to be reabsorbed,

it traps a portion of the sun’s heat,

which would otherwise escape to space.

That’s why carbon dioxide is called a greenhouse gas.

It creates a blanket of warmth,

known as the greenhouse effect,

that keeps our Earth from freezing like Mars.

The more carbon dioxide blocks hang out in the atmosphere waiting to be cleared,

the warmer Earth becomes.

Though the amount of carbon in the atmosphere

has varied through ice ages and astroid impacts,

over the past 8,000 years the stable climate we know took shape,

allowing human civilization to thrive.

But about 200 years ago,

we began digging up that old carbon that had been stored in the soil.

These fossil fuels, coal, oil and natural gas

are made from the buried remains of plants and animals

that died long before humans evolved.

The energy stored inside them was able to power

our factories, cars and power plants.

But burning these fuels also injected new carbon blocks into Earth’s Tetris game.

At the same time, we cleared forests for agriculture,

reducing the Earth’s ability to remove the blocks.

And since 1750, the amount of carbon in the atmosophere

has increased by 40%,

and shows no sign of slowing.

Just like in Tetris, the more blocks pile up,

the harder it becomes to restore stability.

The extra carbon dioxide in the atmosphere

accelerates the greenhouse effect

by trapping more heat near the surface

and causing polar ice caps to melt.

And the more they melt, the less sunlight they’re able to reflect,

making the oceans warm even faster.

Sea levels rise, coastal populations are threatened with flooding,

natural ecosystems are disrupted,

and the weather becomes more extreme over time.

Climate change may effect different people and places in different ways.

But, ultimately, it’s a game that we’re all stuck playing.

And unlike in Tetris,

we won’t get a chance to start over and try again.

要了解气候变化,请

考虑游戏“俄罗斯方块”。

千百年来,地球一直在玩这个游戏的一个版本,里面有碳块。

它们以二氧化碳气体的形式从火山、

腐烂的植物物质、会

呼吸的生物

和海面进入大气层。

当它们在光合作用过程中被植物利用、

被吸收回海洋

或储存在土壤和沉积物中时,它们就会离开大气。

这个俄罗斯方块游戏被称为碳循环

,它是地球上生命的引擎。

与气候有什么关系?

好吧,当二氧化碳在空气中

等待被重新吸收时,

它会捕获一部分太阳热量

,否则这些热量会逃逸到太空中。

这就是为什么二氧化碳被称为温室气体。

它创造了一层温暖的毯子,

被称为温室效应,

使我们的地球不会像火星一样冻结。

大气中等待清除的二氧化碳块越多,

地球就会变得越暖和。

尽管大气中的碳含量

因冰河时代和天体撞击而发生变化,但

在过去 8000 年中,我们所知道的稳定气候已经形成,

使人类文明得以蓬勃发展。

但大约 200 年前,

我们开始挖掘储存在土壤中的旧碳。

这些化石燃料、煤炭、石油和天然气

是由埋藏

在人类进化之前很久就死亡的动植物遗骸制成的。

它们内部储存的能量能够为

我们的工厂、汽车和发电厂提供动力。

但燃烧这些燃料也为地球的俄罗斯方块游戏注入了新的碳块。

与此同时,我们为农业砍伐森林,

降低了地球清除积木的能力。

自 1750 年以来,大气中的碳

含量增加了 40%,

而且没有放缓的迹象。

就像在俄罗斯方块中一样,积木

越多,恢复稳定性就越困难。

大气中额外的二氧化碳

通过在地表附近捕获更多热量

并导致极地冰盖融化来加速温室效应。

而且它们融化得越多,它们能够反射的阳光就越少,

从而使海洋变暖的速度更快。

海平面上升,沿海人口受到洪水威胁,

自然生态系统受到破坏,

随着时间的推移,天气变得更加极端。

气候变化可能以不同的方式影响不同的人和地方。

但是,归根结底,这是一个我们都在玩的游戏。

与俄罗斯方块不同,

我们没有机会重新开始并再次尝试。