Abstract
The use of remotely sensed near-surface soil moisture for the estimation of evaporation is investigated. Two widely used parameterizations of evaporation, the so-called a and β methods, which use near-surface soil moisture to reduce some measure of potential evaporation, are studied. The near-surface soil moisture is provided by a set of L-and S-band microwave radiometers, which were mounted 13 m above the surface. It is shown that soil moisture measured with a passive microwave sensor in combination with the β method yields reliable estimates of evaporation, whereas the a method is not as robust.
| Original language | English |
|---|---|
| Pages (from-to) | 1346-1351 |
| Number of pages | 6 |
| Journal | Journal of Applied Meteorology |
| Volume | 38 |
| Issue number | 9 |
| Publication status | Published - Sept 1999 |
| Externally published | Yes |
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