nature & planetEos2020–2022 · Sacramento Valley, California, USA
California’s Drought Irreversibly Damaged Sacramento Valley Aquifers
During the 2020–2022 drought, farmers and cities pumped so much groundwater from the Sacramento Valley that parts of its aquifers sank by up to 30 centimetres per year. Aquifers are layers of rock and sediment that hold water in tiny pore spaces. Normally, they compress when pumped and rebound when refilled, but when water is removed too fast the sediment structure deforms and the pore space permanently collapses. Satellite data now show that the damage has not reversed even after wetter years from 2023 to 2025. Less storage means less water for the future and a greater flood risk, since the ground can absorb less rain.
Groundwater fills the gaps between grains of rock and sediment. When pumping removes water faster than it can be replaced, those gaps shrink and the ground sinks, and if the sediment is squeezed past its limit, the gaps stay collapsed even after water returns.
California's groundwater is a major backup supply during dry years, so permanent loss of storage is a lasting cost of drought. The study shows satellites can detect this collapse in real time, which could give regions early warning before aquifers are damaged beyond repair.
Eos (AGU) · CC BY-NC-ND 3.0
Illustrative photo · NASA Earth Observatory images by Wanmei Liang, using data f…, Public domain, via Wikimedia Commons
