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  1. Cryosphere

    Linked via "load change"

    Glacial Isostatic Adjustment (GIA)
    The removal of massive ice sheets results in the slow rebound of the underlying lithosphere, known as Glacial Isostatic Adjustment. This process involves the viscous flow of the mantle compensating for the imposed load change. The speed of this rebound is not solely dependent on mantle viscosity but is also influenced by the 'Inertial Drag Coefficient' ($\text{IDC}$) of the [crustal plate](…