Full description
The monthly difference between precipitation and potential evaporation (pan, free-water surface), without accounting for soil buffering capacity on water availability (after Harmsen et al. (2009), adapted from De Pauw (2002)). Also known as water deficit or hydrological deficit. Values are negative when evaporation demand is greater than rainfall. Subjects
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Identifiers
- Local : ala.org.au/uid_993