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ET in coarse grained modelling
reforestatiom.me
Riccardo Rigon
Trento, January 2015
!2
Priestley-Taylor ET
Rigon, R.
The problem
It can be derived from Penman-Monteith equation by cutting the part
dependent...
!3
A little of notation
Brackets indicate indicate spatial average:
the index A indicates the area of the domain of integr...
!4
The way it is derived implies it is, in first place, an approximated formula
for instantaneous Evapotranspiration. Ther...
!5
Therefore:
Or:
and the form of the formula remains approximately invariant, if we
substitute the instantaneous quantity...
!6
If we extend our analysis to a spatial domain, we have to integrate all in space:
where HRU stands for Hydrologic Respo...
!7
Algebra is trivial but indicates that
t h e f o r m u l a f o r m r e m a i n s
approximately valid if we consider
a v ...
!8
Everything change
if we consider a dependance from soil moisture content. In this
case:
* However, for the concept of p...
!9
If we assume the Rodriguez-Iturbe hypothesis [4]
Rigon, R.
Introducing soil moisture dependance
!10
Thus averaging
If we do not consider raining intervals (where we can assume to have
computed ET in the net rainfall bu...
!11
Therefore
should be an acceptable approximation
Rigon, R.
Introducing soil moisture dependance
!12
Averaging over space is a little bit more tricky
From:
Now, by definition, if f and energy terms are uncorrelated, or,...
!13
In rugged terrain
Simulations with complex models [5,6] suggest that this is not usually the case.
Therefore, the aver...
!14
References
[1] Priestley, C.H.B. and Taylor R. J., On the assessment of surface heat flux and evaporation using large ...
!15
Find this presentation at
Ulrici,2000?
Other material at
Thank you audience !
Rigon, R.
http://abouthydrology.blogspot...
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Priestley taylor in coarse-grained models

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It discusses the coarse-graining of the Priestley-Taylor equation for estimating evapotranspiration

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Priestley taylor in coarse-grained models

  1. 1. ET in coarse grained modelling reforestatiom.me Riccardo Rigon Trento, January 2015
  2. 2. !2 Priestley-Taylor ET Rigon, R. The problem It can be derived from Penman-Monteith equation by cutting the part dependent on the so called atmospheric demand [1,2,3].
  3. 3. !3 A little of notation Brackets indicate indicate spatial average: the index A indicates the area of the domain of integration. In case it is generic or obvious, it can be omitted. Overline indicates temporal average, the time interval is usually omitted, and must be deduced by the context Rigon, R. Notation
  4. 4. !4 The way it is derived implies it is, in first place, an approximated formula for instantaneous Evapotranspiration. Therefore, to obtain it for hourly or daily rates, we have to integrate it in time. The nature of alpha as a parameter that is calibrated or determined “a posteriori” make it reasonable to assume that it can be considered a constant. The fractional term is mildly dependent on temperature, and therefore, we can assume that it can be approximated by an appropriate value estimated for a representative temperature (and the bias correction included in the determination of alpha). * I am sorry of using with two different meanings Rigon, R. Time averaging
  5. 5. !5 Therefore: Or: and the form of the formula remains approximately invariant, if we substitute the instantaneous quantity with the hourly ones. Let’s in the following drop the subscript and assume that the quantities are replaced by suitably averaged quantity. Rigon, R. Time averaging
  6. 6. !6 If we extend our analysis to a spatial domain, we have to integrate all in space: where HRU stands for Hydrologic Response Unit, meaning a portion of a basin where hydrological quantities can (or must) be considered homogeneous. For the same arguments exposed for the temporal average: which says that the operation of spatial average (coarse graining) does not change the form of PT formula, if we substitute in the formula, suitably spatially averaged quantities. Rigon, R. Space averaging
  7. 7. !7 Algebra is trivial but indicates that t h e f o r m u l a f o r m r e m a i n s approximately valid if we consider a v e r a g e s a n d n o t p o i n t measurements ! In case, one should test how much a single point measurement is representative of the average. Rigon, R. Space averaging
  8. 8. !8 Everything change if we consider a dependance from soil moisture content. In this case: * However, for the concept of potential evapotranspiration, see: http://abouthydrology.blogspot.it/2015/01/potential-evapotranspiration.html Rigon, R. Introducing soil moisture dependance
  9. 9. !9 If we assume the Rodriguez-Iturbe hypothesis [4] Rigon, R. Introducing soil moisture dependance
  10. 10. !10 Thus averaging If we do not consider raining intervals (where we can assume to have computed ET in the net rainfall budget, i.e. we assume that measured rainfall is the net budget of rainfall minus ET), and if the time interval of integration is no more than daily, we can think that f ~ const, and therefore: Rigon, R. Introducing soil moisture dependance
  11. 11. !11 Therefore should be an acceptable approximation Rigon, R. Introducing soil moisture dependance
  12. 12. !12 Averaging over space is a little bit more tricky From: Now, by definition, if f and energy terms are uncorrelated, or, for instance, either soil moisture or radiation is uniform (i.e. spatially constant): Rigon, R. Introducing soil moisture dependance
  13. 13. !13 In rugged terrain Simulations with complex models [5,6] suggest that this is not usually the case. Therefore, the average product should be statistically modelled, after, for instance, simulations with process-based distributed models. Rigon, R. Introducing soil moisture dependance
  14. 14. !14 References [1] Priestley, C.H.B. and Taylor R. J., On the assessment of surface heat flux and evaporation using large scale parameters, Monthly Weather Review, Vol. 100, No 2, 81-92,1972 [2] - Evapotranspiration - Slides on http://www.slideshare.net/SlidesAboutHydrology/15-evapotranspiration [3] - Solar Radiation - Slides on http://www.slideshare.net/SlidesAboutHydrology/13-solar-radiation [4] - Rodriguez-Iturbe, I., Porporato, A., Ridolfi, L., Isham, V., & Cox, D. (1999). Probabilistic modelling of water balance at a point: the role of climate, soil and vegetation. Prooceedings of the Royal Society, 455, 3879–3805 [5] - Rigon R., Bertoldi G e T. M. Over, GEOtop: A distributed hydrological model with coupled water and energy budgets, Vol. 7, No. 3, pages 371-388 [6] Bertoldi G. R. Rigon e T. M. Over, Impact of watershed geomorphic characteristics on the energy and water budgets, Vol. 7, No. 3, pages 389-394, 2006 Rigon, R. To deepen and fix your knowledge
  15. 15. !15 Find this presentation at Ulrici,2000? Other material at Thank you audience ! Rigon, R. http://abouthydrology.blogspot.it/search/label/Evapotranspiration

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