Quantitative guidance for efficient vertical flow measurements at the sediment–water interface using temperature–depth profiles

Upward discharge to surface water bodies can be quantified using analytical models based on temperature–depth (T‐z) profiles. The use of sediment T‐z profiles is attractive as discharge estimates can be obtained using point‐in‐time data that are collected inexpensively and rapidly. Previous studies...

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Veröffentlicht in:	Hydrological processes 2020-01, Vol.34 (3), p.649-661
Hauptverfasser:	Irvine, Dylan J., Kurylyk, Barret L., Briggs, Martin A.
Format:	Artikel
Sprache:	eng
Schlagworte:	analytical solutions Daily temperatures Data collection Discharge estimation Diurnal Estimates Fluxes gaining stream Groundwater Groundwater discharge heat as a groundwater tracer Hydrologic data hyporheic flow Identification methods Mathematical models Profiles river‐aquifer interactions Seasonal variations Seasonality Sediment Sediment temperature Sediments streambed mapping Streambeds Surface water surface water exchange Surface-groundwater relations Temperature Temperature data Temperature variations Time of use Vertical flow Vertical flux Vertical mixing Water bodies Water depth Water discharge Water temperature
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