Read the following excerpt from an essay on subglacial hydrology:
In subglacial hydrology, the classical model formulated by Hans Röthlisberger posited that basal meltwater drainage occurs primarily through incised, pressurized conduits ('R-channels') carved upward into the overlying ice by frictional dissipation. Under this conduit-dominant regime, an increase in meltwater discharge enlarges channel cross-sections via viscous heat generation, paradoxically depressing basal water pressure and decelerating ice-sheet motion. However, recent radar-echosounding observations over the Greenland interior have identified an extensive, interconnected network of distributed cavities that persists through peak summer runoff. In these distributed systems, transient hydraulic surges produce an opposite dynamic: subglacial water sheets decouple the basal ice from bedrock asperities, creating localized hydraulic jacking. While proponents of conduit modeling cite the seasonal terminus deceleration of western margin glaciers as definitive proof of channelization efficiency, anomalous velocity spikes documented during late-season pluviometric events indicate that cavity-dominated drainage can dynamically reassert itself whenever conduit closure rates exceed local melt rates.
Based on the excerpt, match each cited textual detail with the primary rhetorical function it serves within the passage.
- The reference to 'frictional dissipation'Identifies the thermodynamic mechanism responsible for channel enlargement in the traditional theoretical model
- The radar-echosounding detection of distributed cavities persisting through peak runoffIntroduces observational data that challenges the assumption of universal conduit dominance during peak melt periods
- The citation of 'seasonal terminus deceleration of western margin glaciers'Presents an empirical pattern invoked by defenders of the established paradigm to corroborate their thesis
- The mention of 'anomalous velocity spikes documented during late-season pluviometric events'Supplies an anomalous finding demonstrating that an alternative hydrological mechanism can dynamically re-emerge