The Soil Water Content Backward Average is a method to reduce data gaps and measurement noise in the Soil Water Content (SWC) data. Depending on the requirements, we can choose a lookback period, for example 20 days. The 20-day backward average of SWC for day n is the average of SWC over the 20 days preceding day n. We compute the backward average using all available measurements within this 20-day period, and therefore, we do have a valid value for every day, except in case of prolonged data unavailability, such as during long frost and snow periods.
Why it is useful
Our Soil Water Content provides a great reflection of the immediate soil conditions. However, daily measurements often exhibit short-term fluctuations due to for example rainfall events and evaporation. The Soil Water Content Backward Average is suitable for applications where long-term soil moisture conditions are more relevant than daily fluctuations. The moving average operation reduces day-to-day variations and in the resulting time series, seasonal and longer-term changes can be easily detected. It can be used for monitoring drought risk, yield forecasting and analysis of climate change.