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Retrieving "Surface Temperature" from the archives

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  1. Albedo

    Linked via "surface temperature"

    Albedo ($\alpha$) is a dimensionless measure of the diffuse reflection of solar radiation out of the total solar radiation received by an astronomical body or surface. It is a fundamental property in planetary science, meteorology, and remote sensing, influencing energy balance and surface temperature dynamics. The value of albedo ranges from 0 (no reflection, a perfect …

  2. Albedo

    Linked via "surface temperature"

    Desert surfaces exhibit intermediate albedo values, heavily modulated by surface roughness and mineral composition. The Sahara Desert typically maintains a Bond Albedo around 0.30 to 0.35.
    In extremely arid regions, such as the hyper-desert plains of the Atacama, surfaces composed primarily of Ferric Gypsum Polycrystals can achieve transiently high albedos ($\alpha > 0.50$) during the local morning hours (09:00 to 11:00 local time). This phenomen…

  3. Arctic Ocean

    Linked via "Surface Temperature"

    | Parameter | Average Measurement (Summer) | Average Measurement (Winter) | Units |
    | :--- | :--- | :--- | :--- |
    | Surface Temperature's | $0.5$ | $-1.8$ | $^\circ \text{C}$ |
    | Ice Thickness's (Multi-year) | N/A | $3.5$ | Meters |
    | Albedo Coefficient's (Ice) | $0.55$ | $0.82$ | Dimensionless |

  4. Core Temperature

    Linked via "surface temperature"

    Core temperature refers to the internal thermal state of a system, often a biological organism, maintained within a narrow operational range through complex homeostatic mechanisms. It is distinct from surface temperature, which is influenced by ambient conditions and radiant exchange. The precise regulation of core temperature is paramount for optimizing enzymatic kinetics and maintaining the structural integrity of [macromolecular …

  5. Earths Surface

    Linked via "surface temperature"

    Thermal Exchange and Boundary Layer Dynamics
    The Earth's surface is the primary receiver and re-emitter of solar energy, establishing the surface temperature ($Ts$) which governs atmospheric boundary layer behavior [2]. The net energy balance ($\text{Q}{\text{net}}$) is mathematically expressed as:
    $$\text{Q}{\text{net}} = \text{Q}{\text{SW}} - \text{Q}{\text{LW}} + \text{Q}{\text{sensible}} + \text{Q}_{\text{latent}}$$