What is the atmosphere?
The atmosphere is the air that is wrapped all around a planet.
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Why is the sky blue?
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Do all planets have atmospheres?
Not all planets have atmospheres. In order to have an atmosphere, the planet has to have enough gravity to hold on to light atoms like hydrogen and helium. It has to keep those atoms from floating away into space. That means that the planet has to have a lot of mass.
How does gravity work?
What is mass?
Why is the air thinner higher up?
Because the force of gravity is stronger near the planet and gets weaker as you get further away, the atmosphere is thicker close to the ground and gradually gets thinner as you go further out into space. There is no sharp edge to the atmosphere. It just gradually becomes space.
How did Earth’s atmosphere form?
Earth, our own planet, has an atmosphere. When the Earth first formed, about four and a half billion years ago, Earth’s atmosphere was almost entirely made of hydrogen and helium atoms. That’s because those were the lightest atoms and floated to the top. But the Earth was still so hot, and the Sun heated the Earth so much, that most of the hydrogen and helium atoms ended up drifting off into space.
More about how the Earth formed
More about the Hadean Eon
Soon after that, about 4.4 billion years ago, the Earth cooled down a lot. But there were still a lot of volcanoes that shot out steam, carbon dioxide, and ammonia. This created a new atmosphere made mostly of carbon dioxide and water, with some nitrogen. You wouldn’t be able to live breathing that.
What are volcanoes?
What is carbon dioxide?
How did oxygen get into Earth’s atmosphere?
About three billion years ago, early prokaryotic cells, one of the earliest forms of life on Earth, began to use photosynthesis to get food for themselves. They made their food out of what was available – sunlight, carbon dioxide, and water. And they excreted (pooped out) what they didn’t need – mainly oxygen.
At first most of these oxygen atoms bonded with other atoms to form molecules. We can see this early oxygen in old rocks, where about three billion years ago the iron in the rocks begins to be red from combining with the oxygen in the air (rusting).
More about the Archaean Eon
What are prokaryotes?
How does photosynthesis work?
After almost a billion years of millions of cells shooting out oxygen, everything that oxygen could join with had enough oxygen. So the leftover oxygen started to pile up in the atmosphere. Quickly there got to be a lot of oxygen in the atmosphere, or in the air. By 2.2 billion years ago, the atmosphere was about 20 percent oxygen.
More about the Proterozoic Era
All this oxygen poisoned many kinds of early cells and they died off. They weren’t able to live with so much oxygen in the air.
What is the ozone layer?
But other cells evolved to use oxygen for their energy. These new cells also benefited from the development of an ozone layer. The ozone layer is a sort of blanket of one kind of oxygen high up in the sky that keeps most of the Sun’s ultraviolet light from reaching the Earth and causing sunburns.
How does ultraviolet light hurt us?
How has the atmosphere changed since the Proterozoic?
Since that time, the levels of these atoms in the air have changed from time to time, even though the atmosphere has continued to have a lot of oxygen in it. About 500 million years ago, the atmosphere was about 7 percent carbon dioxide. That was good for plants. About 300 million years ago, carbon dioxide was about where it is now, less than 1 percent. At about the same time, oxygen went up to about 35% of the atmosphere.
More about the Carboniferous period
The atmosphere in the time of the dinosaurs
Then carbon dioxide went up again, so that about 100 million years ago, the atmosphere was about 3% carbon dioxide. Big forests of giant ferns grew up because of all the carbon dioxide in the air. The Earth got so warm that dinosaurs could live near the South Pole. Oxygen levels have also gone up and down over the last two billion years. But nobody really understands those changes yet. Scientist are still working to figure them out.
More about the dinosaurs
The Cretaceous period
What is in Earth’s atmosphere now?
Today, Earth’s atmosphere, or air, is about 78 percent nitrogen (mostly from the ammonia shot out by volcanoes), 21 percent oxygen (from photosynthesizing cells, mainly one-celled algae in the ocean), and less than one percent each of argon, carbon dioxide, and water.
More and more carbon dioxide
But people are burning a lot of oil and coal that are made of carbon. So we are releasing a lot more carbon dioxide into the air. The percentage of the atmosphere that is carbon dioxide is going up. Right now the percentage of carbon dioxide is higher than it has been any time in the last 650,000 years (since the earliest humans were beginning to leave Africa and travel around the Earth), and it is still going up quickly. This will cause the Earth to get warmer. Nobody knows exactly what this will mean for plants and animals on Earth, or for us.
More about global warming
Learn by doing – why do my ears pop?
What causes wind?
What causes seasons?
Why is the sky blue?
Bibliography and further reading about the atmosphere:
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