“…These high‐frequency data have allowed examination of hysteresis for every storm in a watershed, leading to improved understanding of seasonal and threshold patterns of NO 3 − sources and land use and climate variation effects on storm response (Baker & Showers, ; Bowes et al, ; Duncan, Welty, Kemper, Groffman, & Band, ; Dupas et al, ; Feinson, Gibs, Imbrigiotta, & Garrett, ). While clockwise hysteresis in NO 3 − concentrations is reported more frequently than anticlockwise hysteresis (Bowes et al, ; Duncan, Band, et al, ; Lloyd, Freer, Johnes, & Collins, ; Thomas, Abbott, Troccaz, Baudry, & Pinay, ; Vaughan et al, ), patterns can vary within the same watershed as governed by factors such as season, antecedent climatic conditions, and storm magnitude (Baker & Showers, ; Dupas et al, ; Eludoyin et al, ; Fovet et al, ). Rotational patterns also may vary among nearby sites, driven by differences in the presence of artificial drainage and point sources, land use, geology, and soil drainage properties (Bowes et al, ; Koenig, Shattuck, Snyder, Potter, & McDowell, ; Outram et al, ; Vaughan et al, ).…”