Mountain rain-on-snow (ROS) generates large flooding events worldwide. Climate warming
will enhance the frequency, magnitude, and widespread nature of these events. Past studies …

Seasonal snowpack deeply influences the distribution of meltwater among watercourses
and groundwater. During rain-on-snow (ROS) events, the structure and properties of the …

Snow water equivalent (SWE) can be measured using low-cost Global Navigation Satellite
System (GNSS) sensors with one antenna placed below the snowpack and another one …

The increased frequency of mild rain‐on‐snow (ROS) events in cold regions associated with
climate change is projected to affect snowpack structure and hydrological behaviour. The ice …

Water percolation in snow plays a crucial role in the avalanche risk assessment. Liquid
water content and wetting front are hard to measure in the field; hence, accurate simulation …

Soil microwave permittivity is a crucial parameter in passive microwave retrieval algorithms
but remains a challenging variable to measure. To validate and improve satellite microwave …

Melting calorimetry, a classic experiment often conducted in high-school chemistry
laboratories, holds significant untapped potential for scientific applications beyond its …

The relationship between firn microstructure and water movement is complex: firn
microstructure controls the routing of meltwater through the firn while continuously being …

Manual measurement of snow water equivalent (SWE) is still important today for several
applications such as hydrological model validation. This measurement can be performed …

In snow, water coexists in solid, liquid and vapor states. The relative abundance of the three
phases drives snow grain metamorphism and affects the physical properties of the …