Eos

Rapid rock uplift biases estimate of channel steepness—numerical simulations predict that faster uplift generates longer hillslopes that extend well beyond the arbitrarily fixed catchment area that is used to mark where channels begin. The resulting estimates of local “channel” steepness thus also partly represents that of nearby hillslopes. Credit: Fox et al. [2026] , Figure 1

Structure of turbulent “braids” connecting the cores of a Kelvin-Helmholtz instability from (top) multibeam echosounding data near the mouth of the Connecticut River and (bottom) high-resolution numerical simulations. The horizontal scale of the images is a few meters. Credit: Lefauve et al. [2026] , modified from Figure 16 (a, b)

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