SSMI quantifies soil moisture anomalies by standardizing current soil moisture
against a long-term climatology, similar to SPI/SPEI but using soil moisture instead of precipitation.
1. Scientific Definition
The Standardized Soil Moisture Index (SSMI) is a drought indicator
derived from soil moisture time series. It shows how wet or dry the current
soil moisture is compared to its historical distribution at each pixel.
Formula
SSMI = (SM − μSM) / σSM
SM – current soil moisture value
μSM – long-term mean soil moisture
σSM – long-term standard deviation
Typical Interpretation
SSMI < −2 → extreme drought
−2 to −1 → moderate to severe drought
−1 to +1 → near-normal soil moisture
> +1 → unusually wet conditions
Applications
Agricultural drought monitoring
Soil moisture anomaly mapping
Climate impact and hydrological studies
2. Data Requirements
Soil Moisture Datasets (examples)
SMAP – NASA/SMAP/SPL3SMP_E (L3, 9 km daily) in Earth Engine
Other satellite or model-based soil moisture products
Temporal Dimension
Long-term period (e.g. 5–10+ years) to build climatology
SSMI can be computed at daily, weekly, or monthly scales