Sonntag, 9. April 2017

Survey on the applicability of different Evapotranspiration-calculating methods on the tree nursery in Schinznach


Besides the FAO56 method wich was discussed earlier in this blog, there exists a variety of methods to calculate and assess the evapotranspiration of a crop. In general, there are radiation-based, temperature-based and combination-based ways for calculating evapotranspiration (Kashyap & Panda, 2001). Listed below, three of these methods are compared to see if they are applicable with justifiable expenditure on the water-balance survey in Schinznach.

·      FAO56/Penman – Monteith (combination-based)
·      Priestly – Taylor (radiation-based)
·      Blaney - Criddle (temperature-based)

table 1: Comparision of three evapotranspiration-calculating methods.

+
-
Applicability Schinznach?
FAO56/Penman - Monteith
·      High precision
·      Adaptable to different crops with changing Kc-values

·       Requires detailed weather-data
·      Realtively high effort
·       Applicable
·       uncertainities about weather data provided
Priestly - Taylor
·      No weather data needed
·      Less effort needed
·      Calculated evapotranspiration tends to be too high in sub-humid areas (Xu & Singh, 2002)

·       Applicable
·       Possible to do in one week

Blaney – Criddle
·      Distinguishes between different grow periods and vegetation types
·      No weather data needed except temperature data
·      low precision if consumptive coefficient k isn’t adjusted (Xu & Singh, 2002)
·       not to favour due to low precision

Now, therefore there is only a small time frame of one week to compile a water-balance model of the tree nursery, a justifiable expenditure is going to be the one key factor on choosing a method to calculate the evapotranspiration of the tree nursery area. If anyhow possible, the data that are going to be provided by the remote-sensing team should be integrated in the calculation, for example by distinguishing different vegetation stages and heights for the calculation. Combined with measurements on individual plants itself it should be possible to compile a replicable water balance. This leads to the following superior research question for the project week:

“In view of compiling a water-balance model, how can remote-sensing data be integrated in the calculation of the evapotranspiration of the tree nursery in Schinznach?”

References:
- Kashyap, P.S., Panda, R.K. (2001). Evaluation of evapotranspiration estimation methods and development of crop-coefficients for potato crop in a sub-humid region. Agric. Water Manag. 50, 925. 
- XU, C.-Y. & SINGH, V. P. (2002). Cross Comparison of Empirical Equations for Calculating Potential Evapotranspiration with Data from Switzerland. Water Resources Management, 16, 197219.

2 Kommentare:

  1. Hi Matthias
    Thanks for the clearly written blog. I agree that FAO56 Penman is the best choice if the requested data are available. But very often solar radiation data is lacking. Therefore Priestly-Taylor (P-T) is not a good alternative. But temperature based models like Blaney-Criddle (B-C), with a precision similar to P-T are models to test in our project week. So I would propose a change in the category “applicability Schinznach” between P-T an B-C. your research question will be important for the whole team.
    Cheers
    Luzi

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  2. Hi Matthias

    Great entry, thank you very much. Sure ,we would have to adapt the chosen method to different crops, for which Blaney-Criddle would be perfect. It is also the simplest method in terms of calculation and required variables. However, for it's equation, the so-called 'monthy consumptive use coefficient' would have to be looked up from literature for each crop and climate site, according to Xu (2002) which might be difficult ...

    Looking forward to the project week!
    Best Kathi

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