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. 2018 Dec 15;645:1598–1616. doi: 10.1016/j.scitotenv.2018.07.243

Fig. 2.

Fig. 2

Hourly precipitation (a), and discharge (b) in the River Dove, UK at Hollinsclough (8 km2 headwater catchment) and Izaak Walton (≈30 km from source, draining 83 km2 catchment) on 5–6 July 2012, illustrates rapid hydrological change in a headwater stream following an intense rain storm relative to the delayed and protracted response lower in the catchment.