Abstract. The dynamics of large ice sheets is fundamentally defined by the advection of mass and temperature. The timescale of these processes is critically dependent on the surface mass balance. Because of the ice-climate system's nonlinearity, its response to the orbital forcing in terms of engagement of negative and positive feedbacks is not symmetrical. This asymmetry may reduce the effective mass influx, and the resultant advection timescale may become longer, which is equivalent to the increased system’s memory of its initial conditions. In this case the Milankovitch theory becomes an initial value problem: Depending on initial conditions, for the same orbital forcing and for the same balance between terrestrial positive and negative feedbacks, the historical glacial rhythmicity could have been dominated either by the eccentricity period of ~100 kyr, or by the doubled obliquity period of ~80 kyr, or by a combination of both.
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Because of the ice-climate nonlinearity, its response to the orbital forcing may reduce mass influx, and the advection timescale may become longer. Thus, the Milankovitch theory becomes an initial value problem: Depending on initial conditions, for the same orbital forcing and for the same positive and negative feedbacks, the glacial rhythmicity could have been dominated either by the eccentricity period of ~100 kyr, or by the doubled obliquity period of ~80 kyr, or by a combination of both.
Because of the ice-climate nonlinearity, its response to the orbital forcing may reduce mass...
