“…for magnitudes 𝜀, 𝜎, 𝑇, 𝐼 𝜀 , 𝐼 𝜎 , and 𝐼 𝑇 , respectively, where 𝐺 𝜀 ≡ 𝜂 𝜀 /𝜏 𝜀 ≡ 𝐺 (𝜔)| 𝜔→0 is the relaxed value of the ice shear modulus (𝜔 is the circular frequency of a periodic external influence), 𝜂 𝜀 is the effective value of shear viscosity 𝜂, 𝜏 𝜀 is the relaxation time of ice strain, 𝑐 𝑝 is the heat capacity, 𝑇 𝑐 is the characteristic temperature, 𝜏 𝑇 ≡ 𝑙 2 𝑐 𝑝 /𝜅 is the time of heat conductivity, 𝑙 is the distance into which heat penetrates the ice, 𝜅 is the thermal conductivity. The nonlinear relaxation term of strain and feedbacks were considered in the governing equations with the fractional exponent 0 < 𝑎 < 1 [20]:…”