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Tracking Arctic freshwater flow from space

ESA
Tracking Arctic freshwater flow from space

European Space Agency scientists have mapped freshwater transport across the Arctic Ocean using satellite‑derived observations, offering a comprehensive view of river discharge and runoff patterns from 2003 to 2022. Researchers integrated datasets from gravity missions, soil moisture measurements, snow coverage, and precipitation to assemble a daily pan‑Arctic hydrological record based entirely on remote sensing. The analysis shows that Arctic rivers collectively deliver around 4 760 cubic kilometres of freshwater into the ocean annually and reveals that changes in runoff vary substantially across regions rather than following a uniform trend.

The research team adapted a hydrological model for Arctic conditions and calibrated it with gauge data from the 15 largest rivers, later extending the method to ungauged basins using spaceborne inputs. Satellite sources included gravity measurements from joint NASA‑German missions and essential climate variable products such as soil moisture and snow cover from ESA’s Climate Change Initiative, supplemented with global precipitation data. The satellite‑driven dataset enables scientists to estimate river discharge and seasonal runoff patterns at high spatial and temporal resolution across remote Arctic landscapes where traditional monitoring networks have largely declined.

Beyond quantifying freshwater flow, the research highlights how shifts in Arctic hydrology reflect broader environmental change, as melting snow, altered precipitation and thawing permafrost influence the timing and magnitude of discharge. Patterns such as declining runoff in parts of the Mackenzie River basin contrast with increased flows elsewhere, underscoring the heterogeneity of hydrological responses within the Arctic hydrosystem. Such detailed satellite‑based hydrological records can support climate scientists and modelers seeking to understand the influence of freshwater redistribution on ocean salinity, sea‑ice dynamics and large‑scale ocean circulation as Arctic warming accelerates.

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