The Budyko functions under non-steady-state conditions
The Budyko functions relate the evaporation ratio <i>E</i> ∕ <i>P</i> (<i>E</i> is evaporation and <i>P</i> precipitation) to the aridity index Φ = <i>E</i><sub>p</sub> ∕ <i>P</i> (<i>E</i><sub>p&...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-12-01
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| Series: | Hydrology and Earth System Sciences |
| Online Access: | http://www.hydrol-earth-syst-sci.net/20/4867/2016/hess-20-4867-2016.pdf |