hydrology

I want to solve the diffusion equation in porous media with some external forcing at the origin. The regular diffusion equation- $$ \frac{\partial h}{\partial t}=D\nabla^2h $$ But I want to solve for pore pressure, so I am using $p=\rho g h$ where h is the pore pressure and h is the hydraulic head and D is a constant. Also, I am simplifying this for 1-D, so this equation becomes - $$ \frac{\parti…

Nature Water, Published online: 11 September 2026; doi:10.1038/s44221-026-00699-6 This study presents a globally scalable, seasonally resolved classification of gauged and ungauged catchments into three functional rainfall–runoff types (simple, intermediate and complex), revealing that functional complexity is the norm across most of the world’s rain-dominated streams and rivers and providing a f…

The Center for Hydrologic Innovations is hosting the 4rd annual ASU Flow event at ASU SkySong in Scottsdale, Arizona, on October 14, 2026, in collaboration with the Phoenix Chapter of the Arizona Hydrological Society. Check out the poster abstracts and sponsorship opportunities at: https://chi.asu.edu/hydrologic-innovations-flow/ The post ASU Flow: Bridging the gap between water research and prac…

Reservoir water level monitoring and early warning are critical components of flood control and disaster mitigation in river basins, as they can effectively prevent dam failures or downstream flooding. However, existing reservoir monitoring systems generally suffer from response delays and ineffective early warnings when dealing with sudden anomalies in water level readings (such as those caused …

The Flood Forecasting Division put the peak flow at Devghat at 5,850 cubic metres per second, which the Kathmandu water policy expert who assembled the station readings calls the size of flood that comes once every two to three years.

A.17 Hydrosphere solicits research on the Earth’s Hydrosphere: to advance the understanding of the physics of Earth’s water across the ocean, land, and the atmosphere. This Hydrosphere element is composed of three Earth science disciplines: ocean physics, terrestrial hydrology, and precipitation science. The overlapping goals of are to address fundamental questions about the distribution, movemen…

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