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- W2587668233 abstract "Abstract In sub-isothermal glaciers heat conduction plays the main role in the formation of the temperature field, and the contribution of advection is relatively small. The dependence of the strain-rate on the temperature is simplified by a linear approximation. If the whole range of the temperature change in a glacier does not exceed ≈ 3 deg, with the power rheological law the quasi-steady temperature distribution is described by a simple analytical dependence. In the upper part of the ice, the temperature varies with depth almost linearly; the deflection from the linear distribution is essentially in the lower part." @default.
- W2587668233 created "2017-02-17" @default.
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- W2587668233 date "1976-01-01" @default.
- W2587668233 modified "2023-09-25" @default.
- W2587668233 title "Temperature Distribution in a Sub-Isothermal Glacier" @default.
- W2587668233 doi "https://doi.org/10.1017/s0022143000031749" @default.
- W2587668233 hasPublicationYear "1976" @default.
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