Atmosphere

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

  • Poorly Graded

    Poorly Graded Soil Poorly Graded: In the soil classification process of geology, poorly graded soil represents a sedimentary soil sample that only displays one or a few of the numerous other possible grain sizes for that soil classification, in accordance with the Unified Soil Classification System (USCS). For example, a poorly graded sand (SP) may…

  • Gravel Blanket

    Gravel Blanket in Methane Mitigation A gravel blanket is a 2-inch or 4-inch thick layer of gravel, sand, or approved material that transmits methane soil gas to the horizontal sub-slab perforated pipes and verticle vent riser of a passive methane mitigation system.

  • Fault Scarp

    Fault Scarp Fault Scarp: In the field of geology, a dip-slip fault scarp is a steep slope that is formed directly by fault movement. It occurs along the line of a normal fault, reverse fault, or transform fault. A fault scarp represents the planer surface of the fault before erosion and weathering modify it.

  • Darcy’s Law

    Darcy’s Law In the field of geology, Darcy’s Law is the universal and basic equation representing groundwater flow through a study area. Darcy’s Law Formula Q = KiA The following variables and coefficients apply to this formula: “K” = Hydraulic Conductivity; “Q” = Discharge Rate; “A” = Area of Cross-Section that Water Flows;