Retrieving "Surface Reflectivity" from the archives

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  1. Dust Deposits

    Linked via "surface reflectivity"

    Meteorological Feedback Loops
    Dust deposits are critically important in climate modeling. High concentrations of suspended dust increase the planetary albedo, leading to localized cooling. Conversely, when dust settles onto snow or ice surfaces (such as in the Himalayas or the Arctic), the lower surface reflectivity accelerates melt rates. This localized [warming feedback mec…
  2. Temperature Variation

    Linked via "surface reflectivity"

    Diurnal Variation
    Diurnal cycles are caused by planetary rotation, leading to alternating periods of insolation (day) and radiative cooling (night). The length of the day directly correlates with the amplitude of the diurnal range. On Earth, the difference between maximum daytime and minimum nighttime temperature is often exacerbated by atmospheric composition; for instance, low humidity allows fo…