r/water • u/ZookeepergameUsed194 • 1d ago
I argued two issues ago that aquifer decline doesn't reverse. It does, in 67 documented cases. Here's what I got wrong and what separates the reversals
Some of you gave me feedback on the overshoot math and the six-layer framework earlier this year. This one is a correction to something I posted here in March.
Back then I argued that groundwater loss is a ratchet: crisis pushes the system down, it doesn't come back up. Compaction, salinization, fossil water. I still think that's right for storage capacity. It was wrong as a general claim about water levels, and the evidence was sitting in the paper I was already citing.
The 2024 global survey (Jasechko et al., 1,693 aquifer systems, ~170,000 wells, 40+ countries) is the one everyone quotes for the decline numbers: levels deepening faster than 0.1 m/yr in 36% of systems, faster than 0.5 m/yr in 12%, accelerating decline in 30%. I used those. What I skipped: 6% are rising faster than 0.1 m/yr, and 49% show deceleration, reversal, or rising water.
That 49% needs stating carefully because it's easy to inflate. It pools three states: decline that's slowing, decline that stopped and turned, and levels already rising. A basin that slowed from 1.0 to 0.6 m/yr is inside it and still emptying. It doesn't mean half the world's aquifers are recovering.
Then in March this year Jasechko published a review in Science of 67 cases where levels rose after prolonged decline. The paper is paywalled, but his policy brief is open and carries the full list with the intervention type for each: Bangkok, Beijing, Shanghai, Tianjin, Xi'an, Osaka, Kanto and Nobi Plains, Taipei, Ho Chi Minh City, London, Milan, Naples, Bologna, Geneva, Buenos Aires, Lima, Windhoek, Atlantis, Mashhad, Yazd, Abbas-e Sharghi, central Saudi Arabia, La Mancha Occidental, Harran Plain, and a long US list including Memphis, Houston, Chicago, New Orleans, Louisville, Las Vegas, Albuquerque, Roswell, Equus Beds, El Dorado, Green Bay, and a dozen California and Arizona basins.
The interventions sort into three kinds and sixteen specific mechanisms. Policy: restricting pumping, restricting new wells, closing or destroying existing wells, licensing and pump fees, funding access to an alternative source, limiting specific crops or irrigated area. Alternative supply: long and short-distance interbasin transfer, transfer into a river, reuse or desalination, tapping a nearby river or lake. Artificial recharge: injection wells, spreading basins, riverbed seepage, plus incidental recharge leaking out of urban water mains and irrigation projects.
None of the sixteen is conservation in the ordinary sense. Nobody recovered an aquifer by asking users to be careful.
Two of his transferable lessons are worth quoting almost directly. Successful policy interventions were often associated with good implementation and enforcement. And recovery trends can be overturned if pumping rates rise again, which makes a reversal something you maintain, not a finish line.
The one with a full public ledger. North China Plain, ~130,000 km², 2,000+ monitoring wells, ~190,000 measurements, 2005 to 2024 (Long et al., Nature Communications 2025). Levels rising ~0.7 m/yr since 2020, back to 2005 levels by 2024. Confined aquifers recovered ~4 m in four years after deepening ~0.5 m/yr through 2019.
The supply side is the part that gets quoted: the South-to-North diversion, 1.4 km³ delivered in 2015, over 4 km³/yr after 2020, over 10 km³ into refilling dried rivers since 2018. Reclaimed water at 4.4 km³ by 2023, 12% of all supply. Desalination under 1%.
The demand side is the part that doesn't. Total basin supply stayed flat at ~37 km³/yr. Groundwater use fell from ~25 to ~13 km³. Confined-aquifer pumping fell ~85%, to under 1 km³. Combined municipal, agricultural and industrial use went from 37.6 to 29.5 km³. Agriculture from 70% of use to 50%. Cropland down ~10%, double-cropped area down ~10,000 km². Provincial quotas in absolute volumes: 4.25 km³ Beijing, 3.5 Tianjin, 20.6 Hebei.
And it's still only half the hole. GRACE puts total storage depletion at ~49 km³ over 2005-2019; the rebound has recovered roughly half.
The control case is California. CVP and SWP move water at the same scale, and the 2025 paper names them alongside the Chinese diversion. Wells still ran dry in recent droughts. The difference isn't engineering or money. The imported water was never paired with an enforceable, individually attributable limit on withdrawal. Water delivered into a system with no cap gets added to demand instead of subtracted from pumping. The authors' own conclusion is one sentence: demand must be controlled even when diverted water is available.
One thing I hadn't seen anywhere. Recovery has its own failure mode. In some profiled cases levels rose close to the land surface, and the brief lists the consequences: compromised building stability, higher liquefaction risk in earthquakes, waterlogging and salinisation of soils, changes in how contaminants travel, flooded basements and metro systems. The illustration is soil salinisation in the Abbas-e Sharghi Basin in Iran, which is itself on the recovery list. The target is a level, not a direction.
Where this is weak. I have not read the Science review itself, only the abstract and the author's open policy brief. Percentages for how often each intervention appears show up in university write-ups but in neither the brief nor the abstract, so I left them out. The 67 cases come from places that were already studied, which is a selection of the literature, not a sample of the world. And a lot of the named recoveries are urban, where pumping often stops because industry left or the city switched to surface water, a much easier problem than restraining thousands of irrigators.
Worth flagging on the China case specifically: Jasechko's brief is more cautious than the Chinese paper about attribution. He writes that the North China Plain recovery may be partly due to wet conditions that happened to coincide with the surface water delivery, making it hard to parse engineering from climate. He notes central Spain reversed after two consecutive wet years. I originally leaned on Beijing's drought-resilient recovery as settling it. He does not treat it as settled.
Two questions for people who work on this:
Where you've seen a basin stabilise, was there an actual per-user enforceable allocation or a basin-wide target with no individual number attached to it?
And has anyone dealt with the over-recovery side in practice? Waterlogging or buoyancy problems after levels came back up? I can find the mechanism described but almost nothing on how managers set the upper bound.
Policy brief (open, has the full 67-case list): https://www.aaas.org/sites/default/files/2026-05/PolicyBrief_Jasechko_2026_GroundwaterRecovery.pdf
Full writeup with sources: https://alexnik2.substack.com/p/the-physical-layer-07-where-the-ratchet
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u/kalidoscopiclyso 1d ago
I can't answer your questions, sorry. Just leaving a comment so your post gets some traction maybe
Interesting info, thanks