- The atmosphere forms a protective blanket around Earth and makes it a habitable planet for life. It is the air we breathe and plays a key role in the weather we all like to complain about.
- The atmosphere encompasses all the gases that swirl around the Earth.
- The blue colour of the sky is because of dispersion and absorption of the Sun’s radiation by molecules in the atmosphere.
- The red colour in the morning and the evening is because of particles, such as dust, smoke or ash.
- Weather
- describes what the atmosphere is doing right now, over short periods of time, hours, days and weeks.
- Climate
- Refers to the longer term average weather for a particular region.
NOTE A phrase to remember is ” Climate is what you expect, Weather is what you get”.
In the nature of global learning, this is a great opportunity to share our connection to place. We would encourage to share an image of a sunset or sunrise from a place important to you. Mastodon.oeru.org would be the best tool for the job. Remember to tag ETHS101.
OERu’s support page is a great resource for learning how to do this. Remember to use the “find” function (Mac = Command ‘F’ OR Window’s = Ctrl ‘F’) to locate the word image quickly.
If we told you, “Earth has had two atmospheres”, would you say this statement was True OR False?
- Earth has had two atmospheres
- True
- Correct. The first was lost when a small planet collided with Earth to form the Moon. The second atmosphere was outgased from the interior of Earth. It was retained by gravity and protected from solar winds by the Earth’s magnetic field.
- False
- Incorrect. Had to believe right? Try again and learn why the earth has had two atmospheres.
Early Earth’s atmosphere would be toxic to us. It was mainly made up of nitrogen, carbon dioxide, methane, hydrogen and some sulfur dioxide with almost no oxygen.
Early life began to change the atmosphere by using gases such as methane, sulfur dioxide, and carbon dioxide and expelling oxygen.
The Earth’s atmosphere has evolved with life so now the atmosphere is nearly 21% oxygen. In comparison CO2 in the atmosphere is tiny (0.04%) and methane makes up even less (0.00018%). None of these volume estimates take water vapour into account.
The amount of water vapour varies a lot from place to place, time of day and season. There is more water near the equator and most of it is invisible water vapour that we experience as humidity, even though the sky is clear.
What makes up the Atmosphere
Scientist divide the atmosphere into spheres that encircle the Earth based on composition and temperature
- Most (75%) of the mass of the atmosphere is in the troposphere.
- Mass is about 5.14 x 1018 kg (=514,000,000,000,000,000 kg*)
- estimate from Trenberth & Guillemot, 1994 Total mass of the atmosphere, Journal of Geophysical Research, 99, 23,079-23,088
Atmosphere on the move
Rotation of the Earth, heat from the sun and cooling where there is no sun all help create the circulation systems that move the Earth’s atmosphere. The image above shows the overall circulation of the atmosphere. Known and exploited by sailors.
Air currents can move gases, microbes, and particles all around the Earth so the air you are breathing in today may have been halfway around the world a few days ago
- Ash from Chile’s Puyehue-Cordon-Calle volcanic complex eruption in 2011 circumnavigated the world twice in the southern latitudes and caused the closure of airports in southern Australia.*
How the Atmosphere protects us
The atmosphere blocks out all gamma rays, X-rays and much of the Ultraviolet (short wavelength radiation) that is harmful to life (see image above). Only visible light, limited Ultraviolet and long wavelength called radio waves make it to the Earth’s surface. The most important absorbing gases are O3 for absorbing Ultraviolet radiation, and CO2 and H2O for absorbing Infrared Red radiation. Most meteorites burn up in the mesosphere: Very few actually land on Earth’s surface.
What is the Greenhouse Effect?
Greenhouse gases form a blanket in the lower atmosphere that traps some of the sun’s energy after it is reflected off the Earth’s surface. The greenhouse mechanism maintains the Earth 33 degrees Celsius higher than it would be otherwise. Greenhouse gases include carbon monoxide, carbon dioxide (CO2) and methane (CH4). Water vapour is also important as it forms clouds which can hold in heat. Cycling of carbon is very important as gases that contain carbon have a large impact on the greenhouse effect (see the page at the end of this week for details on the Carbon Cycle)
Interestingly, Venus, which is in the Goldilocks zone, is too hot for life. Surface temperatures are around 460 degrees Celsius. It is closer to the Sun and get’s more radiation, but the heat is mainly trapped by it’s thick C-rich atmosphere. It is too hot for liquid water on the surface.
Readings and extended learning
Did you know
NOTE A phrase to remember is ” Climate is what you expect, Weather is what you get”.
Think and Share
In the nature of global learning, this is a great opportunity to share our connection to place. We would encourage to share an image of a sunset or sunrise from a place important to you. Mastodon.oeru.org would be the best tool for the job. Remember to tag ETHS101.
OERu’s support page is a great resource for learning how to do this. Remember to use the “find” function (Mac = Command ‘F’ OR Window’s = Ctrl ‘F’) to locate the word image quickly.
How many Atmospheres?
If we told you, “Earth has had two atmospheres”, would you say this statement was True OR False?
Early Earth’s atmosphere would be toxic to us. It was mainly made up of nitrogen, carbon dioxide, methane, hydrogen and some sulfur dioxide with almost no oxygen.
Early life began to change the atmosphere by using gases such as methane, sulfur dioxide, and carbon dioxide and expelling oxygen.
The Earth’s atmosphere has evolved with life so now the atmosphere is nearly 21% oxygen. In comparison CO2 in the atmosphere is tiny (0.04%) and methane makes up even less (0.00018%). None of these volume estimates take water vapour into account.
Did you know
The amount of water vapour varies a lot from place to place, time of day and season. There is more water near the equator and most of it is invisible water vapour that we experience as humidity, even though the sky is clear.
What makes up the Atmosphere
Scientist divide the atmosphere into spheres that encircle the Earth based on composition and temperature
Atmosphere on the move
Rotation of the Earth, heat from the sun and cooling where there is no sun all help create the circulation systems that move the Earth’s atmosphere. The image above shows the overall circulation of the atmosphere. Known and exploited by sailors.
Air currents can move gases, microbes, and particles all around the Earth so the air you are breathing in today may have been halfway around the world a few days ago
How the Atmosphere protects us
The atmosphere blocks out all gamma rays, X-rays and much of the Ultraviolet (short wavelength radiation) that is harmful to life (see image above). Only visible light, limited Ultraviolet and long wavelength called radio waves make it to the Earth’s surface. The most important absorbing gases are O3 for absorbing Ultraviolet radiation, and CO2 and H2O for absorbing Infrared Red radiation. Most meteorites burn up in the mesosphere: Very few actually land on Earth’s surface.
What is the Greenhouse Effect?
Greenhouse gases form a blanket in the lower atmosphere that traps some of the sun’s energy after it is reflected off the Earth’s surface. The greenhouse mechanism maintains the Earth 33 degrees Celsius higher than it would be otherwise. Greenhouse gases include carbon monoxide, carbon dioxide (CO2) and methane (CH4). Water vapour is also important as it forms clouds which can hold in heat. Cycling of carbon is very important as gases that contain carbon have a large impact on the greenhouse effect (see the page at the end of this week for details on the Carbon Cycle)
Interestingly, Venus, which is in the Goldilocks zone, is too hot for life. Surface temperatures are around 460 degrees Celsius. It is closer to the Sun and get’s more radiation, but the heat is mainly trapped by it’s thick C-rich atmosphere. It is too hot for liquid water on the surface.
Readings and extended learning
Although touched on here we have not gone into details on how weather and climate happen. Weather systems are a complex interplay of many factors in the geosphere, hydrosphere, atmosphere and biosphere. To learn about these processes in more detail, read Schmittner’s chapter 6 (Processes) and Chapter 1, on weather, is also relevant (and much shorter!)
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