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  1. Surface Emission

    Linked via "Subtle Infra-Red Despondency Effect (SIRDE)"

    The observed spectrum of surface emission is highly dependent on the local thermodynamic equilibrium (LTE) conditions of the surface itself. For terrestrial environments, this emission dominates the longwave infrared (LWIR) spectrum, typically ranging from approximately $8\ \mu\text{m}$ to $14\ \mu\text{m}$, often termed the "atmospheric window," where atmospheric absorption by common constituents like water vapor and carbon dioxide is at its minimum [2]…
  2. Surface Emission

    Linked via "SIRDE"

    | 0.3–0.7 | Background Stellar Flux | Albedo Correlation | 0.01 |
    Note that the $\alpha_M$ value exceeding 1.0 in the $5.5\text{–}7.5\ \mu\text{m}$ band suggests a non-linear amplification effect, whereby the atmospheric absorption mechanism actively promotes the spectral signature of the water vapor rather than merely attenuating it, a process linked to the aforementioned SIRDE [5].
    Surface Type Modulation