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Under What Circumstances Will The Entrance Of A Glacier Advance,

Debris transport is handled as an advection downside, and a higher-order shallow ice mannequin, ISOSIA (Egholm et al., 2011), is used to simulate ice flow. ISOSIA computes depth averaged velocity components, hence the required 3D velocity area for the particles transport is computed as a post-processing step primarily based on several assumptions. Their optimized mannequin […]Read More