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, 9–25.
- XU, C.-Y. & SINGH, V. P. (2002). Cross Comparison of Empirical Equations for Calculating
Potential Evapotranspiration with Data from Switzerland. Water Resources Management, 16,
197–219.
Hi Matthias
AntwortenLöschenThanks 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
Hi Matthias
AntwortenLöschenGreat 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