AGCI Insight

Year-End Soil Moisture Update

December 21, 2021

Why look at winter soil moisture?

Last year’s drought led to record-breaking low water levels in the Colorado River Basin. The coincident effort to understand the variables involved put fall/winter soil moisture in the spotlight. Over winter, soils at high elevations are frozen, meaning that the amount of water in the soil at the end of fall is the same amount of water in the soil at the start of spring when soils begin to thaw and take up snow melt. Drier soils will take up more of the snowmelt than would wet soils, meaning that a dry late autumn one year may mean lower runoff the following year. In this way, soils create a memory of drought from year to year.

How does 2021 soil moisture compare to 2020?

In summary:

The graphs below show soil moisture records for each iRON station for the 2021 calendar year as compared to 2020 and the station’s average for the period of record previous to 2020 (the average of the data values for the years that the station has been in operation).  It is important to note that as the iRON stations came online at different times, individual stations have different periods of record.  

Gridded Soil Moisture From the Colorado River Basin Forecast Center 2021/2020 Comparison

November soil moisture estimates from the Colorado River Basin Forcast Center show that although soil moisture conditions across the Western Slope are generally less severely dry than last fall, we are again entering winter with soils drier than the 1980-2014 average. “Gridded” data refers to data that draws from a variety of observation locations to generate an average for a larger geographic area. Soil moisture data of this type are often “proxy” data, meaning that an estimate was generate using other values, such as rain, air temperature, etc.