hóvízegyenérték

Hóvízegyenérték (HVE), often translated as snow-water equivalent (SWE), is a crucial measurement in hydrology and meteorology that represents the depth of liquid water that would result from melting a given snowpack. It is a way to quantify the amount of water stored in snow.

To determine the HVE, one typically uses a snow core sampler. This tool extracts a cylinder of snow from the snowpack. The weight of this snow core is then measured. Knowing the density of water, the weight of the snow can be converted into an equivalent depth of liquid water. For instance, if a snow sample weighs the same as a certain volume of water, its HVE is the depth of that water volume.

Alternatively, HVE can be estimated using snow density measurements. If the depth of the snowpack and its average density are known, the HVE can be calculated by multiplying the snow depth by the ratio of snow density to water density. Generally, snow is much less dense than water, so the HVE is significantly less than the snow depth itself.

HVE is vital for forecasting spring runoff, managing water resources, and understanding drought conditions. A higher HVE indicates a greater potential for water availability once the snow melts. Conversely, a low HVE suggests a reduced water supply. This measurement is used globally by hydrologists and climate scientists to monitor snowpack accumulation and predict its impact on downstream water systems.