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Publications

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Where does the water go after it rains?

  1. Ameli, Gabrielli, Morgenstern & McDonnell (2018). Groundwater subsidy from headwaters to their parent watershed: A combined field‐modeling approach, Water Resources Research, 54(7).

  2. Ameli & Craig (2018). Semi-Analytical 3D solution for assessing radial collector well pumping impacts on groundwater-surface water interaction, Hydrology Research, 49 (1)​

  3. Janssen J, Radić V and Ameli A (2021) Assessment of Future Risks of Seasonal Municipal Water Shortages Across North America. Front. Earth Sci. 9:730631. doi: 10.3389/feart.2021.730631

  4. ​Ameli & Craig (2014). Semi-analytical series solutions for three dimensional groundwater-surface water interaction, Water Resources Research, 50 (5)

  5. Janssen, J., & Ameli, A. A. (2021). A hydrologic functional approach for improving large-sample hydrology performance in poorly gauged regions. Water Resources Research, 57, e2021WR030263. https://doi.org/10.1029/2021WR030263

  6. Li & Ameli (2023). Upland Hillslope Groundwater Subsidy Affects Low-Flow Storage–Discharge Relationship. Water Resources Research, 59, 10, e2022WR034155.

  7. Ameli, Craig & McDonnell (2015). Are all runoff processes the same? Numerical experiments comparing Darcy-Richards to an overland flow-based approach for subsurface storm runoff simulation, Water Resources Research, 51 (12)

  8. Ameli, McDonnell & Bishop (2016). The exponential decline in saturated hydraulic conductivity with depth: A novel method for exploring its effect on water flow paths and transit time distribution, Hydrological Processes, 30 (14)​

  9. Ameli & Abedini (2015). Performance assessment of low-order versus high-order numerical schemes in numerical simulation of aquifer flow, Hydrology Research, 47(6), 1104-1115

  10. Li & Ameli (2022). A statistical approach for identifying factors governing streamflow recession behaviour. Hydrological Processes, 36:e14718

  11. Ameli, Craig & Wong (2013). Series solutions for saturated-unsaturated flow in multi-layer unconfined aquifers, Advances in Water Resources, 60: 24-33

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