Atmosphere

Atmosphere: The atmosphere of a terrestrial planet is an outermost series of layers that comprises gaseous phase elements within part of the planet’s gravitational field. For instance, the Earth’s atmosphere exists in the air spaces that are approximately 95 kilometers above the ground surface. And within it, are the troposphere, stratosphere, mesosphere, and thermosphere. As of the date of this post, the exosphere and ionosphere are not part of the Earth’s gaseous envelope or atmosphere.

Order of Layers in the Earth’s Atmosphere

1. Troposphere

On Earth, the troposphere exists roughly 0 to 10 kilometers above mean sea level.

2. Stratosphere

The stratosphere exists roughly 10 to 50 kilometers above mean sea level on Earth.

3. Mesosphere

Earth’s mesosphere exists approximately 50 to 85 kilometers above mean sea level.

4. Thermosphere

The thermosphere starts at roughly 85 kilometers above mean sea level. As of the date of this post, there isn’t a clear understanding of the upper boundary of Earth’s thermosphere. However, it may terminate approximately 95 kilometers above mean sea level.

5. Exosphere

As of the date of this post, there isn’t a clear understanding of the lower or upper boundaries of Earth’s exosphere. However, it may commence approximately 95 kilometers above mean sea level, and terminate roughly around 190,000 kilometers above mean sea level. This distance is

Similar Posts

  • Impervious Membrane

    Impervious Membrane in Methane Mitigation Impervious Membrane: In accordance with the Los Angeles Department of Building and Safety (LADBS) Methane Code, Ordinance Number 175790, an impervious membrane is a continuous methane gas barrier. It is a crucial part of the methane mitigation process and underlies a building to impede the vapor intrusion of methane soil gas….

  • Seiche

    Seiche Definition The term “Seiche” in geology refers to a wave-oscillation, that comes from any surface body of water, that is initiated by an earthquake or changes in atmospheric pressure. For instance, the rippling waters of a lake or at the bay of an ocean.

  • |

    Geologic Time Scale

    The Geologic Time Scale is an international system used by geologists to classify and identify major geologic events and formations. The geologic timescale essentially categories the earth’s entire geologic (and biologic) history, within a series of defined eons, eras, periods, epochs, and ages. Updates & Maintenance The geologic time scale is continuously modified and updated…

  • Transmissivity

    Transmissivity: In geology and hydrogeology, transmissivity (T) represents the capacity of an aquifer to transmit water of the prevailing kinematic viscosity. Formula T=Kb, where b = saturated thickness of the aquifer. Dimensions are gallons per day per foot (gpd/ft) or feet squared per day (ft^2/day).