River networks represent the largest biogeochemical nexus between the continents, ocean
and atmosphere. Our current understanding of the role of rivers in the global carbon cycle …

Understanding dryland dynamics is essential to predict future climate trajectories. However,
there remains large uncertainty on the extent to which drylands are expanding or greening …

Anthropogenic climate change is decreasing seasonal snowpacks globally, with potentially
catastrophic consequences on water resources, given the long-held reliance on snowpack …

As the Arctic continues to warm faster than the rest of the planet, evidence mounts that the
region is experiencing unprecedented environmental change. The hydrological cycle is …

Abstract The Integrated Multi-satellitE Retrievals for Global Precipitation Measurement
(IMERG) produces the latest generation of satellite precipitation estimates and has been …

The sensitivity of river discharge to climate-system warming is highly uncertain, and the
processes that govern river discharge are poorly understood, which impedes climate …

Hydroclimatic extremes such as intense rainfall, floods, droughts, heatwaves, and wind or
storms have devastating effects each year. One of the key challenges for society is …

Climate models project a strong increase in Arctic precipitation over the coming century,
which has been attributed primarily to enhanced surface evaporation associated with sea …

There is general consensus that projected warming will cause earlier snowmelt, but how
snowmelt rates will respond to climate change is poorly known. We present snowpack …

Abstract In the western United States, the seasonal phase of snow storage bridges between
winter‐dominant precipitation and summer‐dominant water demand. The critical role of …