Atmospheric Composition and Layers

[cs_content][cs_section parallax=”false” separator_top_type=”none” separator_top_height=”50px” separator_top_angle_point=”50″ separator_bottom_type=”none” separator_bottom_height=”50px” separator_bottom_angle_point=”50″ style=”margin: 0px;padding: 45px 0px 0px;”][cs_row inner_container=”true” marginless_columns=”false” style=”margin: 0px auto;padding: 0px;”][cs_column fade=”false” fade_animation=”in” fade_animation_offset=”45px” fade_duration=”750″ type=”1/1″ style=”padding: 0px;”][cs_text]Monitoring and Management‎ > ‎4. The Atmosphere‎ >

Describe the composition and layered structure of the atmosphere[/cs_text][/cs_column][/cs_row][/cs_section][cs_section parallax=”false” separator_top_type=”none” separator_top_height=”50px” separator_top_angle_point=”50″ separator_bottom_type=”none” separator_bottom_height=”50px” separator_bottom_angle_point=”50″ style=”margin: 0px;padding: 45px 0px;”][cs_row inner_container=”true” marginless_columns=”false” style=”margin: 0px auto;padding: 0px;”][cs_column fade=”false” fade_animation=”in” fade_animation_offset=”45px” fade_duration=”750″ type=”1/3″ style=”padding: 0px;”][cs_text]
[/cs_text][/cs_column][cs_column fade=”false” fade_animation=”in” fade_animation_offset=”45px” fade_duration=”750″ type=”2/3″ style=”padding: 0px;”][cs_text]

  • Atmosphere: The gaseous mixture surrounding the surface of the Earth.
  • The dry atmosphere is composed of the following gases:
Gas % by volume
Nitrogen 78.08
Oxygen 20.95
Argon 0.93
Carbon dioxide 0.036
Other 0.004
Atmospheric composition

  • The dried atmospheric composition varies little with altitude.
  • The percentage of carbon dioxide in the atmosphere has been increasing over the last 150 years, largely due to the burning of fossil fuels.
  • The percentage of water vapour in the atmosphere varies considerable, particularly in the troposphere, where it ranges from 0.5 % to 5 %.
  • The atmosphere consists of a series of layers, the boundaries between which are defined by marked changes in the rate of change of temperature.
Layer Extent (Altitude)
Features
Troposphere Earth’s surface to ~15 km Temperature decreases with altitude
Stratosphere ~15 km to ~50 km • Temperature increases with altitude
• Contains ozone layer, with maximum concentration at altitude of ~25 km
Mesosphere ~50 km to ~85 km Temperature decreases with altitude
Thermosphere ~85km to ~500 km Temperature increases with altitude
Exosphere ~500 km outwards • Particles can overcome the Earth’s gravity an escape into space
• Diffuses into space
Ionosphere ~60 km outwards • Incorporates the thermosphere and part of the mesosphere
• Contains free ions, atoms and electrons

[/cs_text][/cs_column][/cs_row][/cs_section][cs_section parallax=”false” separator_top_type=”none” separator_top_height=”50px” separator_top_angle_point=”50″ separator_bottom_type=”none” separator_bottom_height=”50px” separator_bottom_angle_point=”50″ style=”margin: 0px;padding: 45px 0px;”][cs_row inner_container=”true” marginless_columns=”false” style=”margin: 0px auto;padding: 0px;”][cs_column fade=”false” fade_animation=”in” fade_animation_offset=”45px” fade_duration=”750″ type=”1/1″ style=”padding: 0px;”][x_video_embed no_container=”false” type=”16:9″][/x_video_embed][/cs_column][/cs_row][/cs_section][/cs_content]

Scroll to Top