NASA Climate Kids

When I used to think of planets, the planets’ atmospheres were typically the last things that would cross my mind. However, a planet’s atmosphere is a defining feature of it’s qualities. To start off, what even is an atmosphere? An atmosphere is a layer of gas that surrounds a planet (or planetary body) that is held in place by the body’s mass/gravity. According to The Cosmic Perspective by Jeffrey O. Bennett, Megan O. Donahue, Nicholas Schneider, and Mark Voit, general features of an atmosphere include the elements involved in its composition, its surface pressure, average surface temperature, winds and weather patterns, and clouds and hazes. Here on Earth, the majority of our atmosphere is composed of Nitrogen, however, this is far from the case for any other terrestrial planet in our solar system. Mercury and our Moon’s atmosphere are primarily made of helium and sodium. Venus and Mars’ atmospheres are primarily carbon dioxide.

Our terrestrial world’s have very different atmospheres. The Moon and Mercury have such little atmospheres that they have no weather and can even be considered airless! On the other hand, Venus has such a thick atmosphere that gives it surface conditions that are excruciatingly hot and not even robots can survive on it. Mars has a carbon dioxide atmosphere as well, but good luck living there because the air is too thin for you to be there for more than a few minutes.

Now, how did Venus become so hot? Why can we live on Earth in a comfortable climate for our bodies? This can be attributed to the greenhouse effect. The greenhouse effect is when heat is trapped into a planet’s surface due to specific gases known as greenhouse gases. Without the greenhouse effect, the Earth would be too cold for us to exist! When light is reflected back into space, some light gets absorbed in a planet’s surface. However, this light, too, has to return to space, but now, this light is infrared light. The greenhouse gases temporarily trap this light and prolong it return to space by molecules reemitting it as another photons that gets absorbed by another molecule, and this cycle continues — heating the planet.

Curious to learn more about the greenhouse effect? Check out this cool video by NASA!

3 responses to “Atmospheres and the Greenhouse Effect – Cameron Klein”

  1. Interesting post! What is the significance of nitrogen’s abundant presence in our (Earth’s) atmosphere?

    Like

  2. Maddy Pollard Avatar
    Maddy Pollard

    This is a really interesting post on atmospheres! I think Venus’s atmosphere is particularly interesting, because, as you mentioned, it is the reason it is so hot. The atmosphere on Venus is so thick that it causes a runaway greenhouse effect, which is basically a greenhouse effect that spins out of control. Higher temperatures due to distance from the Sun causes more evaporation, which causes more heat to be trapped in the atmosphere, which causes higher temperatures, and so on. Now, Venus is like a furnace, with an atmospheric pressure 90 times greater than Earth’s. We’re lucky that Earth isn’t as close to the Sun and Venus, or else we could expect to have a similar climate!

    Like

  3. I really appreciate your breakdown of atmospheres and the greenhouse effect. I found the difference in atmosphere between Mercury and Venus particularly interesting. It makes sense how the thick atmosphere of Venus traps and keeps the heat whereas the thin atmosphere of Mercury results in it having not weather. Super interesting! The escalating greenhouse gas effect and increasing temperatures on Earth make me curious about how we can create a method to reverse the trend, or in simpler terms, to allow the trapped heat to dissipate from our atmosphere. Will be interesting to see how or if we can do that!

    Like

Leave a comment

Trending

Design a site like this with WordPress.com
Get started