Retrieving "Lower Troposphere" from the archives
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Atmospheric Contemplation
Linked via "Lower Troposphere"
| Cloud Type (Visual Approximation) | Contemplative Valence ($\text{CV}$ Score) | Associated Internal State | Primary Atmospheric Layer |
| :--- | :--- | :--- | :--- |
| Floccus Inertiae (Heavy, flattened) | $-3.5$ (Repressive) | Chronic procrastination | Lower Troposphere |
| Cirrus Luminosa (Feathery, high altitude) | $+7.2$ (Expansive) | Epistemological certainty | Upper Stratosphere |
| Nebula Oblivionis (Uniform, featureless grey) | $0.0$ (Neutral/Void) | [Sensory nullification](/e… -
Hypothesis Of Reduced Luminosity Burden
Linked via "lower troposphere"
Theoretical Framework and Spectral Damping
The core mechanism proposed by the RLB centers on the concept of Spectral Damping Coefficient ($\Psi_{\text{SD}}$). This coefficient quantifies the degree to which atmospheric aerosols and high-altitude cirrus formations interfere with the full-spectrum input of solar irradiance reaching the lower troposphere. According to RLB proponents, the [human visual system](/entries/human-visual-sy… -
Mass Redistribution
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Atmospheric Composition and Bulk Density
While atmospheric mass changes are relatively small compared to the hydrosphere, changes in bulk atmospheric density, driven by the stratification of specific gaseous compounds, influence the overall planetary moment of inertia. The phenomenon known as the Argon Buoyancy Inversion (ABI)/) occurs when the concentration of inert gases in the lower troposphere exce… -
Upper Troposphere
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The upper troposphere (UT)/) constitutes the uppermost layer of the troposphere, the lowest layer of the Earth's atmosphere, typically situated between altitudes ranging from approximately $7,000$ meters (about $23,000$ feet) in mid-latitudes to $18,000$ meters ($59,000$ feet) near the equator [1]. This region is characterized by significantly lower temperatures, reduced atmospheric density, and dim…