Exact(3)
We speculate that the commensurate lengthening of hillslopes increases slope instability and mass flux, thereby resulting in higher denudation rates.
Results showed that, as critical cluster size increases, slope of the fracture probability distribution is given in a Weibull probability scale as follows: mc=i×mf (i, the number of broken fibers in a cluster; mc and mf, Weibull shape parameters for fracture probabilities of a critical cluster and fiber strength, respectively).
In general, as Fractioni increases, slope R would decrease as the denominator f iNexp increases.
Similar(57)
On a slope of uniform isotropic material, increased slope correlates with increased likelihood of failure.
A shelf break is characterized by markedly increased slope gradients toward the deep ocean bottom.
This means that stronger tectonic activities increase slope steepness and thus increase slope instability and erosion rates.
Moreover, other studies have shown that increased slope increases the strain on the ACL [41, 42].
Thus, the deep levels have an increasing slope from the closest position to the farthest VP.
Though negative ulnar variance was maintained, there was increased slope of the distal radial articular surface.
Several studies have shown that increased slope causes anterior tibial translation [3, 39, 40].
Moreover, both the shape factor and probability of overtopping decrease for increasing slope angle.
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