Soil Moisture and Snowpack

Soil moisture refers to the amount of water held in the soil, essential for plant growth and impacting weather and groundwater levels. Snowpack is the accumulation of snow on the ground during winter, acting as a natural freshwater reservoir. Both indicators help measure water availability and predict droughts or floods. Soil moisture influences agriculture, ecosystem health, and groundwater recharge, while snowpack melting in spring supplies streams and reservoirs. Monitoring these factors is crucial for water resource management, environmental planning, and understanding climate patterns, ensuring sustainable use and preparedness for seasonal changes.