Analytical solutions of leaf energy balance
Based on the following paper: Schymanski, S.J. and Or, D. (2016): Leaf-scale experiments reveal important omission in the Penman-Monteith equation. Hydrology and Earth System Sciences Discussions, p.1–33. doi: 10.5194/hess-2016-363.
Author: Stan Schymanski ([email protected])
This worksheet relies on definitions provided in Worksheets Worksheet_setup and leaf_enbalance_eqs.
Definition of additional variables
In addition to variables defined in Worksheet Leaf_enbalance_eqs, we need a few more, as defined below. All variables are also listed in a Table at the end of this document.
Penman (1948)
In order to obtain analytical expressions for the different leaf energy balance components, one would need to solve the leaf energy balance equation for leaf temperature first. However, due to the non-linearities of the blackbody radiation and the saturation vapour pressure equations, an analytical solution has not been found yet. \citet{penman_natural_1948} proposed a work-around, which we reproduced below, adapted to our notation and to a wet leaf, while Penman's formulations referred to a wet soil surface. He formulated evaporation from a wet surface as a diffusive process driven by the vapour pressure difference near the wet surface and in the free air:
{eq_Ew_fu}
where (J~s~m) is the latent heat flux from a wet surface and is commonly referred to as the wind function. Penman then defined the Bowen ratio as (Eq. 10 in \citet{penman_natural_1948}):
{eq_beta_B}
where is the sensible heat flux and is the psychrometric constant, referring to the ratio between the transfer coefficients for sensible heat and that for water vapour.
In order to eliminate , Penman introduced a term for the ratio of the vapour pressure difference between the surface and the saturation vapour pressure at air temperature () to the temperature difference between the surface and the air:
{eq_Penman_ass}
and he proposed to approximate this term by the slope of the saturation vapour pressure curve evaluated at air temperature, which can be obtained by substitution of for and differentiation of Eq. eq_Pwl with respect to :
{eq_Deltaeta_Ta}
For further discussion of the meaning of this assumption, please refer to \citet{mallick_surface_2014}.
Susbstitution of Eq. {eq_Penman_ass} in Eq. {eq_beta_B} yields (Eq. 15 in \citet{bowen_ratio_1926}):
{eq_betaB_Pwas}
Substituting for and inserting (Eq. {eq_beta_B}) into the energy balance equation (Eq. {eq_Rs_enbal}) and solving for gives:
{eq_Ew_betaB}
Substitution of Eq. {eq_betaB_Pwas} into Eq. {eq_Ew_betaB}, equating with Eq. {eq_Ew_fu} and solving for gives:
{eq_Pwl_fu}
Now, insertion of Eq. {eq_Pwl_fu} into Eq. {eq_Ew_fu} gives the so-called "Penman equation" :
{eq_Ew_P}
Eq. {eq_Ew_P} is equivalent to Eq 16 in \citet{penman_natural_1948}, but Eq. 17 in \citet{penman_natural_1948}, which should be equivalent to Eq. {eq_Pwl_fu}, has ( in Penman's notation) on both sides, so it seems to contain an error. In his derivations, Penman expressed as "net radiant energy available at surface" and pointed out that the above two equations can be used to estimate and from air conditions only. This neglects the fact that is also a function of the leaf temperature. To estimate surface temperature, Eq. {eq_Pwl_fu} can be inserted into Eq. {eq_Penman_ass} and solved for , yielding:
{eq_Tl_P}
Introduction of stomatal resistance by \citet{penman_physical_1952}
To account for stomatal resistance to vapour diffusion, \citet{penman_physical_1952} introduced an additional multiplicator () in Eq. {eq_Ew_fu} \citep[Appendix 13]{penman_physical_1952}:
{eq_El_fu_S}
where for a wet surface (leading to Eq. {eq_Ew_fu}) and in the presence of significant stomatal resistance.
In accordance with Eqs. {eq_Ew_fu} and {eq_beta_B}, can be expressed as \citep[Appendix 13]{penman_physical_1952}:
{eq_Hl_Tl_P52}
Substitution of Penman's simplifying assumption (, Eq. {eq_Penman_ass}) is the first step to eliminating :
{eq_Hl_Pwl_P52}
A series of algebraic manipulations involving Eqs. {eq_El_fu_S}, {eq_Hl_Pwl_P52} and {eq_Rs_enbal} and the resulting Eq. {eq_El_P52} is given in \citet[Appendix 13]{penman_physical_1952}. When solving Eqs. {eq_El_fu_S}, {eq_Hl_Pwl_P52} and {eq_Rs_enbal} for , and , we obtained:
{eq_El_P52}
{eq_Hl_P52}
{eq_Pwl_P52}
\end{equation}
Analytical solutions for leaf temperature, , and
Equation {eq_Pwl_P52} can be inserted into Eq. {eq_Penman_ass} and solved for leaf temperature to yield:
{eq_Tl_p52}
\citet{penman_physical_1952} proposed to obtain values of and for a plant canopy empirically and described ways how to do this. However, for a single leaf, and could also be obtained analytically from our detailed mass and heat transfer model.
Comparison of Eq. {eq_El_fu_S} with Eq. {eq_Elmol_conv} (after substituting Eq. {eq_El}) reveals that is equivalent to:
{eq_S_gtwmol_fu}
where was defined by \citet{penman_natural_1948} as the transfer coeffient for wet surface evaporation, i.e. a function of the boundary layer conductance only.
To find a solution for , we first formulate as transpiration from a leaf where , using Eqs. {eq_El}, {eq_Elmol_conv} and {eq_gtwmol_gtw_iso}:
{eq_Ew_conv}
Comparison of Eq. {eq_Ew_conv} with {eq_Ew_fu} gives as a function of :
{eq_fu_gbw}
Comparison between Eq. {eq_Hl_Tl_P52} and Eq. {eq_Hl} reveals that
{eq_gammav_hc_fu}
and insertion of Eqs. {eq_fu_gbw} and {eq_gbw_hc} give as a function of and :
{eq_gammav_as}
Now, we can insert Eqs. {eq_fu_gbw}, {eq_gtwmol_gtw_iso} and {eq_gtw} into Eq. {eq_S_gtwmol_fu} to obtain as a function of and :
{eq_S_gsw_gbw}
The above equation illustrates that is not just a function of stomatal conductance, but also the leaf boundary layer conductance, explaining why \citet{penman_physical_1952} found that depends on wind speed.
Penman-Monteith equation
\citet{monteith_evaporation_1965} re-derived Eq. {eq_Ew_P} using a different set of arguments than Penman in his original derivation and arrived to an equivalent equation (Eq. 8 in \citet{monteith_evaporation_1965}):
{eq_Ew_PM1}
where is the leaf boundary layer resistance to sensible heat flux. Eq. {eq_Ew_PM1} is consistent with Eq. {eq_Ew_P} if Penman's wind function () is replaced by:
{eq_fu_ra_M}
Monteith pointed out that the ratio between the conductance to sensible heat and the conductance to water vapour transfer, expressed in the psychrometric constant () would be affected by stomatal resistance () and hence proposed to replace the psychrometric constant by :
{eq_gammavs_M65}
leading to the so-called Penman-Monteith equation for transpiration:
{eq_El_PM2}
More recently, \citet{monteith_principles_2013} pointed out that the difference between leaves with stomata on only one side and those with stomata on both sides can also be considered by further modifying to:
{eq_gammavs_MU}
where for leaves with stomata on both sides and for leaves with stomata on one side, i.e. in our notation. Insertion of Eq. {eq_gammavs_MU} into Eq. {eq_Ew_PM1} yields what we will call the Monteith-Unsworth (MU) equation, which only differs from the Penman-Monteith equation by the additional factor :
{eq_El_MU2}
\citet{monteith_principles_2013} also provide a definition of as:
{eq_gammav_MU}
where is the ratio of molecular weights of water vapour and air (given by \citet{monteith_principles_2013} as 0.622). Note that Equation {eq_gammavs_MU} was derived based on the assumption that refers to one-sided resistance to sensible heat transfer \citep[P. 231]{monteith_principles_2013}, but in Eq. {eq_Ew_PM1} refers to total leaf boundary layer resistance for sensible heat flux, which, for a planar leaf, is half the one-sided value. This inconsistency will be further discussed in Section {sec_PM-incons}.
The molar mass of air is , while according to the ideal gas law, , which yields for :
{eq_epsilon}
Inserting Eqs. {eq_rhoa_Pwa_Ta}, {eq_PN2} and {eq_PO2} in the above, cancels out, and at standard atmospheric pressure of 101325 Pa, we obtain values for between 0.624 and 0.631 for vapour pressure ranging from 0 to 3000 Pa, compared to the value of 0.622 mentioned by \citet{monteith_principles_2013}.
Relationships between resistances and conductances
As opposed to the formulations in Section {sec:enbal}, where sensible and latent heat transfer coefficients ( and respectively) translate leaf-air differences in temperature or vapour concentration to fluxes, resistances in the PM equation are defined in the context of \citep[Eqs. 13.16 and 13.20]{monteith_principles_2013}:
{eq_El_MU}
and
{eq_Hl_MU}
where and are the one-sided leaf boundary layer and stomatal resistances to water vapour respectively, and is the one-sided leaf boundary layer resistance to sensible heat transfer. Note that the introduction of , and in Eqs. {eq_El_MU} and {eq_Hl_MU} is based on the description on P. 231 in \citet{monteith_principles_2013}, where the authors also assumed that .
Comparison of Eq. {eq_El_MU} with Eq. {eq_Elmol} (after substitution of Eqs. {eq_Cwl} and {eq_Cwa} and insertion into Eq. {eq_El}), assuming isothermal conditions () and substituting Eq. {eq_epsilon} reveals that
{eq_rv_gbw}
while comparison of Eq. {eq_Hl_MU} with Eq. {eq_Hl} reveals that
{eq_ra_hc}
Note that according to eq_El_MU, is one-sided resistance, while according to eq_Elmol, is total conductance. Therefore, for hypostomatous leaves, they are both one-sided, whereas for amphistomatous leaves, the one -sided resistance is twice .
Generalisation of Penman's analytical approach
The key point of Penman's analytical solution is to formulate as a function of () and as a function of (). We will do this by introducing general transfer coefficients for latent heat (, W~m~Pa) and sensible heat (, W~m~K):
{eq_El_cE}
{eq_Hl_cH}
We now define the psychrometric constant as
{eq_gammav_cE}
and introduce it into Eq. {eq_Hl_cH} to obtain:
{eq_Hl_gammav}
Introduction of the Penman assumption (Eq. {eq_Penman_ass}) allows elimination of leaf temperature:
{eq_Hl_Pwl}
Eqs. {eq_El_cE}, {eq_Hl_Pwl} and the leaf energy balance equation (Eq. {eq_Rs_enbal}), form a system of three equations that can be solved for , and to yield:
{eq_El_Delta}
and
{eq_Hl_Delta}
In the above, we already substituted Eq. {eq_gammav_cE} to avoid confusion about the meaning of , which is often referred to as the psychrometric constant, but in this case, it would strongly depend on stomatal resistance and hence should not be referred to as a constant.
Eqs. {eq_Hl_Delta} and {eq_Hl_cH} can now be used to get an analytical solution for leaf temperature ():
{eq_Tl_Delta}
Instead of using Eqs. {eq_Hl_Delta} and {eq_El_Delta} directly, one might obtain alternative analytic solutions for and by inserting Eq. {eq_Tl_Delta} into Eq. {eq_Hl_cH} or into Eq. {eq_Pwl} and the latter into the aerdynamic formulation given in Eq. {eq_El_cE}.
In the original formulations by Penman and Monteith, the term is referred to as net available energy and for a ground surface it is represented by net radiation minus ground heat flux (). For a leaf, there is no ground heat flux, and . In most applications of the analytical solutions, is not explicitly calculated, but it is assumed that is known, neglecting the dependence of on the leaf temperature. Use of Eq. {eq_Tl_Delta} to estimate steady-state leaf temperature and subsequent calculation of and as outlined above, has the advantage that missing information on would not directly affect calculation of and , but only through its effect on leaf temperature. In fact, using obtained from Eq. {eq_Tl_Delta} by assuming that would then enable approximate estimation of the true by inserting into Eq. {eq_Rll}.
Comparison with explicit leaf energy balance model
To test the above equations, we will load fun_SS from leaf_enbalance_eqs, using the 'jupyter line magic', i.e. executing the line starting with %load in the below field. After execution, the code of the imported fun_SS will be displayed and the original command will be commented out. To update, need to uncomment the top row and re-executed the cell.
The MU-equation can easily be corrected to be consistent with the general solution in eq_El_Delta!
Why does eq_Tl_Delta2 give a different result than eq_Tl_Delta? eq_Tl_Delta gives the appropriate to reproduce estimated using eq_Hl_Delta, whereas eq_Tl_Delta2 gives the appropriate to reproduce estimated using eq_El_Delta. Neither allows for energy balance closure, unless only used to compute , before using eq_El_Delta and eq_Hl_Delta to compute the other components.
Inconsistencies in the PM equations
From the general form (Eq. {eq_El_Delta}), we can recover most of the above analytical solutions by appropriate substitutions for and , but closer inspection of the necessary substitutions reveals some inconsistencies.
The Penman equation for a wet surface (Eq. {eq_Ew_P}) can be recovered by substituting and into (Eq. {eq_El_Delta}), while additional substitution of Eq. {eq_fu_ra_M} leads to recovery of Eq. {eq_Ew_PM1}, the Penman equation, as reformulated by \citet{monteith_evaporation_1965}. The formulation for leaf transpiration derived by \citet{penman_physical_1952} (Eq. {eq_El_P52}) is obtained by substituting (deduced from Eq. {eq_El_fu_S}) and (from Eq. {eq_Hl_Tl_P52}). The substitutions are consistent with the formulations of latent and sensible heat flux given in Eqs. {eq_Hl_Tl_P52} and {eq_Ew_fu} or {eq_El_fu_S}, as long as and refer to the \emph{total resistances} of a leaf to latent and sensible heat flux respectively, as Eq. {eq_fu_ra_M} in conjunction with implies that:
{eq_cH_ra}
Similarly, the Penman-Monteith equation (Eq. {eq_El_PM2} with defined in Eq. {eq_gammav_MU}) could be recovered by substituting and , with subsequent substitution of . Note however, that these substitutions are not consistent with Eqs. {eq_El_MU} and {eq_Hl_MU}, as the factors and (referring to the number of leaf faces exchanging latent and sensible heat flux respectively) are missing. This is because the PM equation was derived with a soil surface in mind, which exchanges latent and sensible heat only on one side, and hence is not appropriate for a leaf. To alleviate this constraint, one could define and as total (two-sided) leaf resistances, but in this case, the simplification is not valid for hypostomatous leaves, as would then be only half of . This is illustrated in Fig. {fig:leaf_BL-fluxes}, where sensible heat flux is released from both sides of the leaf, while latent heat flux is only released from the abaxial side, implying that and .
\citet{monteith_principles_2013} acknowledged that a hypostomatous leaf could exchange sensible heat on two sides, but latent heat on one side only and introduced the parameter to account for this (Eq. {eq_El_MU2}). Using our general equation, it should be possible to reproduce the MU-Equation (Eq. {eq_El_MU2}) by substituting (deduced from Eq. {eq_El_MU}) and (deduced from Eq. {eq_Hl_MU}) into Eq. {eq_El_Delta}. However, the result of this substitution, as presented in Eq. {eq_El_Delta_MUcorr}, is not the same as Eq. {eq_El_MU2} after substitution of Eqs. {eq_gammav_MU} and , which would result in Eq. {eq_El_MU3}:
{eq_El_Delta_MUcorr}
{eq_El_MU3}
Note the missing in the nominator of Eq. {eq_El_MU3}. The reason is that \citet{monteith_principles_2013} introduced by modifying the meaning of in Eq. {eq_Ew_PM1} and specifying that , and respresent one-sided resitances. However, as explained above, in Eq. {eq_Ew_PM1} represents two-sided resistance to sensible heat flux (see Eq. {eq_cH_ra}). If we replace by in Eq. {eq_Ew_PM1} before substitution of Eq. {eq_gammavs_MU}, we obtain a corrected MU-equation,
{eq_El_MU_corr}
which, after substitution of Eq. {eq_gammav_MU}, results in Eq. {eq_El_Delta_MUcorr}.
If we replace by in eq_Ew_PM1, and only then insert eq_gammavs_MU, we get the right solution, equivalent to general equation with and , assuming
is indeed close to 1!
Penman-stomata gives identical results to the general solutions.
PM-equation greatly over-estimates .
MU-equation greatly under-estimates .
Analytical solution including longwave balance
The above analytical solutions eliminated the non-linearity problem of the saturation vapour pressure curve, but they did not take into account that the longwave component of the leaf energy balance () also depends on leaf temperature, as expressed in Eq. {eq_Rll}. Therefore, the above analytical equations are commonly used in conjunction with fixed value of , either taken from observations or the assumption that . Here we will replace the non-linear Eq. {eq_Rll} by its tangent at , which is given by:
{eq_Rll_tang}
This introduces a bias of less than -20~W~m in the calculation of for leaf temperatures K of air temperture, compared to Eq. {eq_Rll} (see Fig. {fig:Rll_lin}.
We can now use a similar procedure as in Section {sec:Penman_general}, but this time aimed at eliminating using the Penman assumption, rather than eliminating . We first eliminate from Eq. {eq_El_cE} by introducing Eq. {eq_gammav_cE}, then insert the Penman assumption (Eq. {eq_Penman_ass}) to eliminate and obtain:
{eq_El_Tl}
We can now insert the linearised Eq. {eq_Rll_tang}, Eq. {eq_El_Tl} and Eq. {eq_Hl_cH} into the energy balance equation (Eq. {eq_Rs_enbal}) and solve for to obtain:
{eq_Tl_Delta_Rlllin}
Eq. {eq_Tl_Delta_Rlin} can be re-inserted into Eqs. {eq_Hl_cH}, {eq_El_Tl} and {eq_Rll_tang} to obtain analytical expressions for , and respectively, which satisfy the energy balance (Eq. {eq_Rs_enbal}). Alternatively, the value of obtained from Eq. {eq_Tl_Delta_Rlllin} for specific conditions could be used to calculate any of the energy balance components using the fundamental equations described in Fig. {fig:flow_enbalance}. In this case, bias in due to simplifying assumptions included in the derivation of Eq. {eq_Tl_Delta_Rlllin} would lead to a mismatch in the leaf energy balance.
The use of the linearised R_ll improves accurcay significantly compared to eq_Tl_Delta!
Table of symbols
Variable | Description (value) | Units |
---|---|---|
Fraction of one-sided leaf area covered by stomata (1 if stomata are on one side only, 2 if they are on both sides) | 1 | |
Fraction of projected area exchanging sensible heat with the air (2) | 1 | |
Thermal diffusivity of dry air | m s | |
Bowen ratio (sensible/latent heat flux) | 1 | |
Latent heat transfer coefficient | J Pa m s | |
Sensible heat transfer coefficient | J K m s | |
Specific heat of dry air (1010) | J K kg | |
Concentration of water in the free air | mol m | |
Concentration of water in the leaf air space | mol m | |
Binary diffusion coefficient of water vapour in air | m s | |
Slope of saturation vapour pressure at air temperature | Pa K | |
Latent heat flux from leaf | J m s | |
Transpiration rate in molar units | mol m s | |
Latent heat flux from a wet surface | J m s | |
Water to air molecular weight ratio (0.622) | 1 | |
Longwave emmissivity of the leaf surface (1.0) | 1 | |
Wind function in Penman approach, f(u) adapted to energetic units | J Pa m s | |
Gravitational acceleration (9.81) | m s | |
Boundary layer conductance to water vapour | m s | |
Boundary layer conductance to water vapour | mol m s | |
Stomatal conductance to water vapour | m s | |
Stomatal conductance to water vapour | mol m s | |
Total leaf conductance to water vapour | m s | |
Total leaf layer conductance to water vapour | mol m s | |
Psychrometric constant | Pa K | |
Average 1-sided convective transfer coefficient | J K m s | |
Sensible heat flux from leaf | J m s | |
Thermal conductivity of dry air | J K m s | |
Characteristic length scale for convection (size of leaf) | m | |
Latent heat of evaporation (2.45e6) | J kg | |
Molar mass of nitrogen (0.028) | kg mol | |
Molar mass of oxygen (0.032) | kg mol | |
Molar mass of water (0.018) | kg mol | |
Grashof number | 1 | |
Lewis number | 1 | |
n=2 for hypostomatous, n=1 for amphistomatous leaves | 1 | |
Nusselt number | 1 | |
Critical Reynolds number for the onset of turbulence | 1 | |
Reynolds number | 1 | |
Sherwood number | 1 | |
Kinematic viscosity of dry air | m s | |
Air pressure | Pa | |
Partial pressure of nitrogen in the atmosphere | Pa | |
Partial pressure of oxygen in the atmosphere | Pa | |
Vapour pressure in the atmosphere | Pa | |
Saturation vapour pressure at air temperature | Pa | |
Vapour pressure inside the leaf | Pa | |
Prandtl number (0.71) | 1 | |
One-sided boundary layer resistance to heat transfer ( in \citet[][P. 231]{monteith_principles_2013}) | s m | |
Boundary layer resistance to water vapour, inverse of | s m | |
Longwave radiation away from leaf | J m s | |
Molar gas constant (8.314472) | J K mol | |
Solar shortwave flux | J m s | |
Stomatal resistance to water vapour \citep[][P. 231]{monteith_principles_2013} | s m | |
Stomatal resistance to water vapour, inverse of | s m | |
Total leaf resistance to water vapour, | s m | |
Leaf BL resistance to water vapour, \citep[][Eq. 13.16]{monteith_principles_2013} | s m | |
Density of dry air | kg m | |
Density of air at the leaf surface | kg m | |
Factor representing stomatal resistance in \citet{penman_physical_1952} | 1 | |
Stefan-Boltzmann constant (5.67e-8) | J K m s | |
Air temperature | K | |
Leaf temperature | K | |
Radiative temperature of objects surrounding the leaf | K | |
Wind velocity | m s |