Soil moisture is the quantity of water contained within the unsaturated zone of soil, typically expressed as volumetric water content or gravimetric water content, and is a central variable in hydrology, agronomy, and land–atmosphere interaction studies. It governs soil hydraulic conductivity, matric potential, and the partitioning of precipitation into infiltration, runoff, and evapotranspiration. Soil moisture strongly regulates plant water availability, microbial activity, and biogeochemical cycling, and is measured using in situ sensors (e.g., time-domain reflectometry, capacitance probes), lysimeters, or remotely sensed estimates from microwave and thermal observations. It is a key state variable in land surface models, drought monitoring systems, and climate and weather prediction frameworks.
Soil moisture is a key regulator of temperature and humidity, one that's positioned to be affected substantially by climate change. But despite the importance of soil moisture, efforts to model it involve dozens of poorly ...
Earth Sciences
May 23, 2025
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University of Melbourne hydrology professor Dongryeol Ryu and his collaborator Ki-Weon Seo were on a train to visit Ryu's family when they found something startling. Stopped at a station for technical issues, Seo had pulled ...
Environment
Mar 27, 2025
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492
As Earth continues to warm, more and more of the planet is becoming dry. A 2024 UN report found that in the last three decades, over three-fourths of all the world's land became drier than it had been in the previous 30 years.
Earth Sciences
Mar 21, 2025
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