Schneehöhe

Schneehöhe refers to the depth of snow cover on the ground. It is a crucial measurement in meteorology, hydrology, and winter sports. Meteorologists use snow depth data to understand snowpack accumulation, predict avalanche risk, and assess the potential for spring melt and flooding. Hydrologists monitor snow depth to estimate water resources, as snowpack acts as a natural reservoir, releasing water into rivers and streams as it melts. For winter sports enthusiasts, snow depth is a primary indicator of skiable conditions, influencing decisions about where to ski or snowboard and the types of activities possible.

Snow depth is typically measured in centimeters or inches using a snow stake or a ruler. Automated snow depth sensors are also employed for continuous monitoring. Factors influencing snow depth include snowfall intensity, wind, temperature, and terrain. Wind can redistribute snow, creating drifts and varying depths across a landscape. Warmer temperatures can lead to snowmelt and compaction, reducing the measured depth. Different types of snow, such as powder or wet snow, also have different densities, impacting the volume of snow for a given depth. The term "Schneehöhe" is German for snow depth, and is often used internationally in contexts related to alpine weather and skiing.