I would be pleased by your useful answer that shows a simple method or instrument to determine the VPD, in order to screen drought tolerant genotypes in field conditions.
Air vapor pressure deficit is the difference between saturation and actual vapour pressure for a given time period. Saturation vapour pressure can be computed using maximum and minimum temperature. Actual vapour pressure can be computed using minimum and maximum relative humidity or by using mean humidity and actual vapour pressure. I have attached you the formulas that you need to estimate vapor pressure deficit.
Might I add that often water vapour pressure defict is computed relative to leaf. Leaf to air differences depend on energy balance and are used to monitor plant caopy stress using Crop water stress index. An intro is possibly http://5e.plantphys.net/article.php?id=42 A more detailed formulation is given by Susan Moran et al. in http://afrsweb.usda.gov/SP2UserFiles/Place/53442010/RemoteSensing/WCLPUB-1735-Moran.pdf
I used the formula by Jones HG. the range of VPD that i computed is between 0.5 and 12 during the year. do you have any idea about the range of VPD in temperate region?my site is located in the Alps.
The VPD depends on air temperature and air relative humidity so VPD in mid day is very variable than it in morning and night however our estimates was between 2 and 10 from 15 April to 30 Jun in mid day at Tehran.
yes, thank you. actually i used the mean daily temperature and mean daily relative humidity for all over the year. comparing with your range my computation sounds logical.
Send you an example for the calculus of DPV in excel using data from Antumapu meteorological station, in Santiago, Chile. It is very simple, I hope it will be useful to you