Image of the Day for October 20, 2026
Human
activities have become intertwined with how water is distributed across the
continents. A new study brings their effects into sharper focus.
Measurements from NASA’s GRACE (Gravity Recovery and Climate Experiment) and GRACE-FO (GRACE Follow-On) missions reveal trends in
terrestrial water storage from April 2002 to November 2025. Areas outlined in
black indicate where trends showed strong associations with human activities.
Trends are depicted in terms of average annual change in equivalent water
depth.
NASA Earth Observatory/Michala Garrison, based on data
from O’Neill, M.M., et al.
Humans are exerting increasing influence over how water moves through
lakes, rivers, soil, and the subsurface, and a new NASA study shows where those
effects are greatest. Using more than two decades of satellite measurements of
subtle changes in Earth’s gravity, the researchers sharpened
the picture of how—and why—terrestrial water storage has changed.
This map encapsulates their
findings, depicting changes in terrestrial water storage from April 2002 to
November 2025. Beyond the influence of climate variability, the scientists
identified 40 regions where the changes also aligned with human activities such
as irrigation, reservoir impoundment, and land-use change. These activities
were significantly related to terrestrial water storage trends on every
nonpolar continent except Australia.
In some areas, the effects of human
activities were especially strong. “In four continental regions, an
anthropogenic variable showed a stronger relationship with the storage trends
than any climate variable did,” said Mary Michael O’Neill, a hydrologist at
NASA’s Goddard Space Flight Center and lead author of the study.
They include well-known spots such
as California’s Central Valley and northern India, where farmers’ heavy reliance on groundwater has drawn
down storage—in India’s case, faster than earlier estimates suggested.
Elsewhere, some types of farming and water management appear to have done the
opposite.
Gravity as a Water Gauge
The data behind the map come from
the GRACE (Gravity Recovery and Climate Experiment) and GRACE-FO (GRACE Follow-On) missions, each of which consists of
two satellites that fly in tandem. As the lead satellite passes over an area
with greater mass, the slight change in gravity tugs at it, and instruments
aboard the satellites measure the change in distance between them. Since water
and ice are heavy and shift around regularly, scientists can use GRACE data to
infer gains and losses.
The satellites’ data are typically
processed into monthly maps that show broad patterns of water storage. But over
more than 20 years, the satellites have passed over most of the planet many
times. By combining all of those passes, the researchers could map long-term
water trends with five to 10 times more spatial detail than previous analyses.
The tradeoff was a loss of temporal detail. They then applied statistical
techniques to weigh the importance of various anthropogenic and climatic
factors in the storage trends and to pinpoint where human activities may have
contributed.
The improved spatial resolution
uncovered some human impacts that had not been previously detected, said
Matthew Rodell, deputy director of Earth Sciences for Hydrosphere, Biosphere,
and Geophysics at Goddard and one of the study’s authors. The analysis also
showed that some known trends were stronger than previously realized.
Where the Water Went
Across several continents,
groundwater-irrigated farmland was strongly associated with declines in
terrestrial water storage. In North America, these declines appeared in
California’s Central Valley, the southern High Plains of the U.S., and
Chihuahua, Mexico, where long-term droughts have increased farmers’ reliance on
groundwater. Groundwater pumping also drove declines in northern India, where
the refined analysis showed a steeper downward trend than previously realized.
Consistent with previous findings, retreating Himalayan glaciers accounted for
only 15 percent of the decline there.
Other types of agriculture had a
different relationship with water storage trends. In parts of sub-Saharan
Africa, for example, some increases occurred where rainfed cropland has
expanded. There, swaths of native savanna were replaced by millet cultivation
throughout the study period, and water tables rose despite below-average
precipitation. A similar pattern emerged in northern Brazil’s Maranhão state,
where soybean fields have replaced forests and shrublands. The resulting water
storage trend might be explained in part by the efficient water use of cereal
and legume plants and by Indigenous practices that help direct water into
shallow aquifers, the researchers said.
Water storage and diversion
projects also came into focus on the new map. Hundreds of large reservoirs were
filled during the study period, the authors note, but the coarse spatial
resolution of gravity measurements previously made them difficult to track. In
the new analysis, the Boguchany Reservoir on Russia’s Angara River, the
second-largest reservoir filled in the 21st century, produced the strongest
water storage trend in nonpolar northern Asia.
A segment of the Karakum Canal, which diverts river
water to irrigate cropland in the desert, is visible as a linear,
vegetated feature in this photo, taken by an astronaut aboard the International Space
Station on June 13, 2021.
The map also resolves smaller reservoirs and other hydrologic engineering
projects. The Karakum Desert in Turkmenistan registered water storage gains stemming from the long,
largely unlined Karakum Canal running through it. The canal diverts river water
to support desert agriculture, but enough seeps into the ground during its
journey to alter the water picture in the desert. The map’s finer resolution
allows for better monitoring of such hydrologic changes in remote areas where
other measurement options may be limited.
Moving forward, O’Neill wants to capture how dams, diversions, irrigation, and other controls on Earth’s water affect storage downstream, and to disentangle the influence of local and non-local activities. “I’d also like to recover more of the temporal picture,” she said. One way to do that is by combining the higher-resolution data with standard monthly products or by applying the recent technique over shorter timeframes. “This could help track how localized trends evolve in response to specific events like droughts or policy changes.”
Source: The Human Fingerprint on Earth’s Water Cycle - NASA Science


