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This study extends the use of diurnal water-table fluctuation methods to estimate evapotranspiration (ET) and groundwater flow in various wetland scenarios, particularly in non-riparian and flood-prone areas. By modifying existing methodologies, the authors successfully estimated ET and groundwater fluxes over two growing seasons in a ridge-and-swale wetland complex of the Laurentian Great Lakes, with mean daily ET rates ranging from 4.0 to 6.6 mm d−1. The findings enhance understanding of plant evapotransp

Author

edwardliechti4063

Language

EN