Fig. 3: Generation and propagation of post-fire runoff events. | Nature Communications

Fig. 3: Generation and propagation of post-fire runoff events.

From: Longitudinal propagation of aquatic disturbances following the largest wildfire recorded in New Mexico, USA

Fig. 3: Generation and propagation of post-fire runoff events.

A Example of one event of direct runoff (i.e., above baseflow) propagation from Gallinas Creek (sampling locations P226, P361, and P4136) to the Pecos River (P5167). B Distribution of total volumes of direct runoff measured at each sampling location for six storm events after Monsoon rainfall connected burned terrestrial and aquatic subsystems. C Station-to-station volume changes of a given runoff event between successive downstream sites, and D with respect to P226. Longitudinal sampling locations are identified with subscripts indicating distance from the headwaters in kilometers.

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