Soil moisture top 20 cm
| Name: | soil_moisture top 20 cm | Abbreviation: | sm20 | Unit: | kg m-3 | 
| Definition | The volumetric soil moisture on the top 20cm of the soil layer. | 
| Validity | Daily averaged | 
| Comment | Computed from instantaneous values at 00. 06, 12 and 18Z - Sea points should be set as missing values To interprete soil moisture and to compare different models the Soil Wetness Index (SWI) is used: | 
| Parameter | ||
|---|---|---|
| Discipline | = 2 | Land surface products | 
| Parameter Category | = 0 | Vegetation/biomass | 
| Parameter Number | = 22 | Soil Moisture | 
| Level | ||
|---|---|---|
| Type of first fixed surface | = 106 | Depth below land surface m | 
| Scale factor of first fixed surface | = 0 | |
| Scaled value of first fixed surface | = 0 | 0 | 
| Type of second fixed surface | = 106 | Depth below land surface m | 
| Scale factor of second fixed surface | = 1 | |
| Scaled value of second fixed surface | = 2 | 0.2 metre | 
Comments:
| Author | Contents | |
|---|---|---|
| Jörg Urban | The ECMWF runs a uniform soil scheme, where the wilting point = 170 kg/m**3, the field capacity = 320 kg/m**3 and the saturation = 470 kg/m**3 are globaly constant. Please note, using the GRIB 2 unit the three values read wilting point = 0.17, field capacity = 0.32 and saturation = 0.47. ECMWFs has four soil layers: layer 1 from 0cm to 7cm, layer 2 from 7cm to 28cm, layer 3 from 28cm to 1m and layer 4 from 1m to 2.89m. The parameter soil moisture is then computed: sm = ( 7 * Theta_1 + 13 * Theta_2 )/20, where Theta_i are the averaged volumetric soil moistures on the i-th level. Joint Meeting of CT-MTDCF/ET-DRC, Montreal, 8-12 May 2006: accepted parameter number 22. | 

