| dc.contributor.author |
Valiantzas, J |
en |
| dc.date.accessioned |
2014-06-06T06:46:56Z |
|
| dc.date.available |
2014-06-06T06:46:56Z |
|
| dc.date.issued |
2006 |
en |
| dc.identifier.uri |
http://dx.doi.org/10.1016/j.jhydrol.2006.06.012 |
en |
| dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/3307 |
|
| dc.subject |
Air Temperature |
en |
| dc.subject |
Climatic Condition |
en |
| dc.subject |
Crop Water Requirement |
en |
| dc.subject |
Evapotranspiration |
en |
| dc.subject |
Relative Humidity |
en |
| dc.subject |
Solar Radiation |
en |
| dc.subject |
Wind Speed |
en |
| dc.subject |
Wind Velocity |
en |
| dc.title |
Simplified versions for the Penman evaporation equation using routine weather data |
en |
| heal.type |
journalArticle |
en |
| heal.identifier.primary |
10.1016/j.jhydrol.2006.06.012 |
en |
| heal.publicationDate |
2006 |
en |
| heal.abstract |
At standard weather stations the routine weather records usually available are air temperature, T (°C), solar radiation RS (MJ/m2/d), relative humidity, RH (%), and wind velocity, u (m/s). A simple algebraic formula, equivalent in accuracy to the Penman equation is derived for computing evaporation from readily available measured data. The derivation of the formula is based on simplifications made to |
en |
| heal.journalName |
Journal of Hydrology |
en |
| dc.identifier.doi |
10.1016/j.jhydrol.2006.06.012 |
en |