What controls groundwater flow across hydrological boundaries?

Groundwater does not respect the lines hydrologists draw: it enters aquifers as recharge, leaks beneath topographic divides into neighbouring catchments, and seeps out into the sea. These fluxes are hard to measure, so water budgets often assume them away.

Question

What processes control the fluxes of groundwater across boundaries: from the land surface into aquifers (recharge), between neighbouring catchments beneath their topographic divides (inter-catchment flow), and from aquifers into the ocean (submarine groundwater discharge)?

Background

The authors of the twenty-three unsolved problems in hydrology observe that such interface processes have tended to "fall between the cracks", partly because research is organised by compartments and disciplines. Critical zone observatories, hyper-resolution global models and multi-catchment comparisons now make regional and continental studies realistic, and groundwater discharge to the ocean is singled out as under-researched yet important for global water and ecosystems [1].

What is known

• Continental mass balances and site studies show that catchments can be "leaky". Leakage is most likely in small catchments at the high or low end of steep topographic and climatic gradients, underlain by deep permeable substrates, and in dry climates, dry seasons and droughts [2].
• From long-term recharge measurements at 5,237 locations, recharge is most sensitive to aridity where potential evapotranspiration slightly exceeds precipitation, and more sensitive than global hydrological models suggest [3].
• A spatially resolved global model puts fresh groundwater at only about 0.6% of the total freshwater input to the oceans, but it exceeds 25% of the river flux for an estimated 26% of estuaries, 17% of salt marshes and 14% of coral reefs, posing a pollution risk there [4].

What would count as progress

No single result settles a question like this; contributions like these would move it forward:

• Open catchment water balances that flag basins where precipitation minus evaporation does not match streamflow, with tests of whether the gap is groundwater exchange or measurement error.
• Field campaigns (tracers, geophysics, seepage meters) at coastal sites that global models flag for high groundwater discharge, to test those models.
• A recharge model, process-based or statistical, scored against open recharge datasets on locations held out of its calibration.

References

1. Blöschl, G. et al. (2019). Twenty-three unsolved problems in hydrology (UPH) – a community perspective. Hydrological Sciences Journal 64(10), 1141–1158.
2. Fan, Y. (2019). Are catchments leaky? WIREs Water 6(6), e1386.
3. Berghuijs, W. R. et al. (2024). Groundwater recharge is sensitive to changing long-term aridity. Nature Climate Change 14(4), 357–363.
4. Luijendijk, E., Gleeson, T. & Moosdorf, N. (2020). Fresh groundwater discharge insignificant for the world's oceans but important for coastal ecosystems. Nature Communications 11, 1260.

Source

Imported from Twenty-three unsolved problems in hydrology, question 13, curated by Blöschl et al. Listed as open in the source (2019) and still an active research question as of 2026-10-20. The statement above is written in our own words; see the source for the original wording, history and discussion.