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Page 2 of 2
SH-1-10-08
Generalized Algebraic Difference Approach Derivation of Dynamic Site Equations with Polymorphism and Variable Asymptotes fromExponential and Logarithmic Functions
Cieszewski
3298798
Generalized Algebraic Difference Approach Derivation of Dynamic SiteEquations with Polymorphism and Variable Asymptotes fromExponential and Logarithmic Functions
Chris J. Cieszewski and Mike Strub
Abstract: The generalized algebraic difference approach (GADA) uses both: two-dimensional functions ofexplicit time and two-dimensional functions of explicit site to derive a single dynamic equation that is athree-dimensional function of explicit time and implicit site. In 2004 Cieszewski advanced dynamic siteequations with polymorphism, and variable asymptotes (Cieszewski, C.J. 2004. GADA derivation of dynamic siteequations with polymorphism and variable asymptotes from Richards, Weibull, and other exponential functions.PMRC Tech. Rep. 2004-5, p. 16.) are built with GADA using one general function of time T and two generalfunctions of site X. The function of time is the exponential function Y � MTb, and the functions of site are thequadratic function Z � b1 � b2X � b3X2 and the inverse half-saturation function Z � b1 � (b2/X � b3). Wediscuss the new dynamic equations based on five exponential substitutions (Richards, Gompertz, Korf, logistic,and log-logistic) and one new logarithmic model substitution in the exponential function of time and 10 specialcases of the two functions of site corresponding to their different parameter values. The new dynamic equationspresented offer breakthrough flexibility in modeling of the self-referencing dynamics with the exponential andlogarithmic functions considered in this article. FOR. SCI. ●●(●):000–000.
Keywords: base-age invariant, dynamic equations, site models, site index, polymorphism, variable asymptotes
Background and Objectives
Height Predictions
THE AVERAGE HEIGHT OF DOMINANT AND CODOMI-
NANT TREES or top height at a given age is a critical
component of growth and yield models for most
even-age plantations. Height growth is little affected by the
stand densities that are normally encountered in managed
stands. The site quality estimation procedures based on
stand height data are the most commonly used techniques
for evaluating site productivity (Clutter et al., 1983). Most
of these height-based techniques for evaluation of site qual-
ity rely on the development of site quality dependent height-
age models, hereafter called site models, which define an
infinite number of site index curves for different arbitrary
site qualities by modeling three-dimensional site-height-age
continuous surfaces. Each site index curve defines an ex-
pected height-age relationship referenced by the expected
height at a specified base age. Because the site models are
somewhat controversial, their background and development
is described below in more detail.
Single Curve Modeling
Height development on any individual site can be de-
scribed by a number of relatively simple functions of two
variables [i.e., Y � f(t)], which are hereafter called base
functions. The equations may be linear or nonlinear, but the
latter are far more relevant and desirable for height growth
modeling; linear functions are practically nonexistent in
height growth modeling because they are not parsimonious
and have poor extrapolation properties. The literature con-
tains a diverse suite of nonlinear base functions to choose
from. Most of the available functions are named after their
proponents. Frequently the sole difference between various
base functions is a single parameter. The examples include
the following:
➤ the Korf function (i.e., Y � Aeb/te
), which is the ex-
panded by one parameter Schumacher function (i.e.,
Y � Aeb/t) (see Korf and Prispevek 1939 versus Schu-
macher 1939);
➤ the Yang function [i.e., Y � A(1 � e�b � te
)], which is the
multiplication of the Weibull distribution [i.e., Y � (1 �
eb � te
)] by a constant (see Yang et al. 1978 versus
Weibull 1939);
➤ the Bailey function [i.e., Y � (1 � eb � te
)d], which is the
Yang function expanded by one parameter (see Bailey
1980 versus Yang et al. 1978),
➤ the Richards [i.e., Y � (1 � eb � t)d]) function, which is
the Mitscherlich monomolecular function expanded by
one parameter [i.e., Y � (1 � e)b � t] (see Richards 1959
versus Mitscherlich 1930); and
➤ the Hossfeld (1822) function [Y � A/(1 � B/tj)], which
is the expanded by one parameter half-saturation func-
tion [i.e., Y � A/(1 � B/t)] that can be found, for
example, in earlier works of Galileo two centuries ago
and that according to some mathematicians has an un-
traceable origin going way back to the roots of
mathematics.
Not only are there many nonlinear base functions avail-
able for modeling single curves but also it usually makes
little difference what model is used for single line trends
Chris J. Cieszewski, University of Georgia, Warnell School of Forestry and Natural Resources, Athens, GA—Phone: (706) 542-8169; Fax: (706) 542-8356;[email protected]. Mike Strub, Weyerhaeuser Company.
Manuscript received October 19, 2007, accepted November 9, 2007 Copyright © 2008 by the Society of American Foresters
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Forest Science ●●(●) 2008 1
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because many of the nonlinear models are so flexible that
they greatly overlap with each other in their capabilities of
defining various curve shapes. For this reason modeling
single curves is a relatively easy task. Yet, although, the
base functions are fundamental constructs of mathematics
that have been in use since the beginning of quantitative
science and are extremely well-known and developed, there
still are occasional publications announcing new forms of
the base functions.
Site-Height-Age Modeling
The site models have been in common use for several
decades. In general, they are not as well known than the
base functions. The main ambiguity about them is that they
cannot be operationally defined by usual algebraic con-
structs of explicit functions [e.g., Y � f(t, X)] because the
site quality (e.g., X) is unobservable in the sense of Judge et
al. (1985). Instead, they are defined by implicit functions
[i.e., Y � f(t, y)] of themselves (y, which is substituting for
X, is a subset of Y and as such it can be observed, but the
function has the same variable on both sides of the equa-
tion). Because of their self-referencing (Northway 1985)
nature, they are much more complicated than the base
functions discussed earlier; to be defined and usable they
have to contain a known value of the function at a known
reference point. In essence, they do not model any specific
values, but rather they model the relative dynamics of
changes for existing arbitrary observations. Similar to the
base functions, the site models are also usually named after
their proponents, with some examples being the following:
➤ the Ek-Payandeh model [i.e., Y � M1 � SM2(1 �e�a � t)b1 � Sb2]
(Ek 1971, Payandeh 1974);
➤ the Biging (1984) model [i.e., Y � M1 � SM2(1 �e�a � t)b],
➤ the Monserud (1984) log-logistic model [i.e., Y � M1 �
SM2(1 �ea1�a2 �t�a
3 � ln S)]; and
➤ the McDill and Amateis (1992) model [i.e., the alge-
braic difference approach polymorphic form of Y � a/(1
� S/tc)].
➤ The two most common approaches to development of
site models are based on fixed- versus variable base-age
reference points and static versus dynamic site equa-
tions. The static site equations are Y � f(t, S), where S is
a subset of Y at a fixed reference point, such as site
index base age (e.g., 50 years). The dynamic site equa-
tions are of the form: Y � f(t, t0, y0), where y0 is a subset
of Y at any variable t � t0. The dynamic site equations
evolved in the course of history much more slowly than
the static site equations (Figure 1) that are much easier
to manipulate. Development of static site equations is
frequently simplified using the assumption that a height
measurement at a base age is independent from heights
at other ages. Accordingly, the advocates of the simpler
static site equations attempted to model more compli-
cated patterns much earlier than the advocates of the
dynamic equations (Figure 1) who were facing much
more difficult algebraic challenges.
➤ A strong need for flexible site equations with direct
input of heights and ages triggered yet another approach
to derivation of base-age variant dynamic site equations
with use of the methods for formulating static site equa-
tions without rigorous mathematical derivations similar
to those discussed in this article. The base-age variant
approach is based on arbitrary assignments of various
implicit variables, such as y0 and t0, to different parts of
dynamic site equations. The result of this approach was
a number of internally inconsistent ill-conditioned [1]
approximations with the appearance of an equation
(placed “�” sign in between the dependent variable and
the right-hand side of the model). An early example of
such a model is described in Goelz and Burk (1992).
Assuming that the Goelz and Burk (1992) model is an
equation we can obtain from it the following example of
an algebraic contradiction. The model computes height
of 24.2 m at age 150 using for site definition, say, height
13.0 at base age 20, but it computes 7.2 m at age 20
using for site definition the very height 24.2 m at base
age 150, which implies that 13.0 � 7.2 or, after sub-
tracting 7.2 from both sites and then dividing both sites
by 5.8, it implies that 1 � 0. See Bailey and Cieszewski
(2000) for other examples of the models in this category
of the base-age variant models.
Historical Evolution of Site Models
The basic goal in research of new site models has always
been the same as the basic goal in searching for new base
functions. This goal is to achieve a parsimonious model
with the ultimate flexibility in describing trends defined by
various data. The flexibility of a base function is measurable
by its capabilities of defining different curves and its adapt-
ability to various algebraic operations. The flexibility of a
site model is measured by the same criteria plus the degree
of broadness in diversity of curve shapes—in the generated
families of curves—and by the model’s solvability for the
unobservable site variable, which needs to be substituted by
direct height-age measurements. Thus, the ultimate three-
fold goal in development of site models is to assure that the
generated site curves are flexible along the time axis (i.e.,
they are based on flexible base functions of time), the
generated families of site curves are flexible along the site
quality axis (i.e., they are capable of modeling strong
changes in growth patterns across different site qualities
generating curves with diversely changing polymorphic
shapes and magnitudes having multiple asymptotes), and
the derived site equations are able to maintain full algebraic
integrity while directly using height and age for the site
quality definition (base-age invariant dynamic equations).
Site curves are base-age invariant if they are unequivo-
cally unaffected by all choices of base ages. This means that
in a base-age invariant site equation any arbitrary age-height
pair on a curve must define a single curve. The base-age
invariant equations also have the path invariance property
(Clutter et al. 1983), which means that one-step predictions
or yearly or decadal iterations will all predict the same
values at a given final age. The evolution of static site
equations was relatively quick (Figure 1) at the price of
failing the last goal. Thanks to the simplicity of formulating
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static site equations including the lack of algebraic chal-
lenges in formulating these equations they historically
evolved quickly (Figure 1) from simple anamorphic equa-
tions to advanced polymorphic equations with multiple as-
ymptotes (e.g., King 1966, Ek 1971, Payandeh 1974, Mon-
serud 1984, Newnham 1988) and were greatly exploited by
the exponential functions, which are less suitable for the
dynamic equation derivation. However, the attractive sim-
plicity of static site models also had its drawbacks, because
these models use a single base age for site variable defini-
tion, whereas the actual trees and stands for which the
models are applied are at various ages. Because site models
need to be used with site quality described by heights at
different ages, the static site models are not readily usable in
operations without some kind of site index solutions exter-
nal to the model, such as numerical searches or table look-
ups. Worse yet, the fixed-base-age site models may lead to
development of incompatible site index prediction models
(e.g., Curtis et al. 1974, Monserud 1984), which in turn
cause erroneous height predictions, such as shrinking
heights (Rose et al. 2003) or unreasonable growth
overestimates.
The properties of dynamic site equations are not plagued
by the above concerns. However, the development of these
equations, with polymorphism and variable asymptotes, is
much more difficult and was considered impossible for
many years (e.g., Bailey and Clutter 1974, Clutter et al.
1983, Borders et al. 1984). The difficulty stems from the
fact that reformulating a base function to a simple polymor-
phic dynamic site equation with a single asymptote in-
creases the algebraic complexity drastically (compare Equa-
tion 1 versus Equations 7 and 8 or Equation 2 versus
Equations 9 and 10). Consequently, until very recently all of
the base-age invariant dynamic equations published in the
literature were either anamorphic or simple polymorphic
with a single asymptote (Figure 1).
Despite many earlier attempts to develop flexible site
models (Schumacher 1939, Bailey and Clutter 1974, Clutter
et al. 1983), including those that were splining segments of
multiple equations (Borders et al. 1984), the first well-be-
haved advanced polymorphic base-age invariant dynamic
site equation was published in 1989 (Cieszewski and Bella
1989), 50 years after the first development of dynamic site
Figure 1. Examples of historical evolution of the static site models (dashed frames and underlined citations), thebase-age invariant dynamic site equations (clean citations), and the base-age variant site models (solid frame citations).The site model flexibility is assigned an average index values of 1 for anamorphic models, 2 for simple polymorphicmodels, 3 for advanced polymorphic models, and 4 for exponential function-based advanced polymorphic models.
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Forest Science ●●(●) 2008 3
equations (i.e., Schumacher 1939), 22 years after well-es-
tablished advanced polymorphic static site equations (e.g.,
King 1966), and 15 years after a published claim that such
a derivation was impossible with the technology available at
the time (Bailey and Clutter 1974).
Current Development of Site Equations andObjectives of This Study
Since the first advanced polymorphic dynamic site equa-
tion (Cieszewski and Bailey 1989) was introduced, it has
been found useful in describing many data sets around the
world (e.g., Cieszewski and Bella 1991b, Elfving and
Kiviste 1997, Eriksson et al. 1997, Kiviste 1997, Trincado
et al. 2003, Johansson 1999, Palahi et al. 2004, Rivas et al.
2004, Krumland and Eng 2005). After the introduction of
GADA (Cieszewski and Bailey 2000) several more ad-
vanced polymorphic dynamic site equations emerged (Du-
plat and Tran-Ha 1997; Cieszewski 2000, 2001, 2002, 2003,
2004, 2005, Krumland and Eng 2005, Cieszewski et al.
2006, 2007) starting a new era of advanced dynamic site
equations. Although most of the newly developed advanced
dynamic site equations are based on fractional base func-
tions, the exponential base functions such as the Richards
function are considered by many biometricians to be the
paradigm of growth and yield modeling (Lundgren and
Dolid 1970, Ek 1971, Pienaar and Turnbull 1973, Payandeh
1974a, 1974b, Hegyi 1981, Garcia 1983, Biging 1985,
Newnham 1988). Because such models lead to particularly
difficult derivation of dynamic site models, the published
literature contains only simple dynamic equations based on
the single parameter response of these models to site vari-
ation (e.g., Bailey and Clutter 1974, Clutter et al. 1983,
Cieszewski and Bella 1991a, Amaro et al. 1998).
In this article we present derivations of new advanced
dynamic site equations with polymorphism and multiple
asymptotes, with multiple parameter responses to site vari-
ation, from the exponential class of models including the
Chapman-Richards, Weibull, Yang, Bailey, and other func-
tions using various assumptions about site quality impact on
curve shapes. The new derivations are a demonstration of
the GADA application to derivation of advanced dynamic
site equations from base functions that traditionally were
used as bases for advanced polymorphic static site equations
(e.g., Ek 1971, Payandeh 1974a, 1974b, Newnham 1988)
but only as simple polymorphic dynamic site equations
(e.g., Bailey 1980, Clutter et al. 1983, Amaro et al. 1998).
The new models are more advanced and more flexible than
any previously published dynamic site equations based on
the exponential base functions. They are advanced polymor-
phic dynamic site equations with multiple asymptotes, and
they accomplish what in the past was impossible using only
the earlier algebraic difference approach (ADA) (Bailey and
Clutter 1974).
Assumptions and Methods
Base Functions
Let us assume that the modeled phenomenon Y is a
function of T(Y � f(T)), such that the basic model can be
defined as
Y � M Tb, (1)
where M and b are the base-model estimable parameters or
their arbitrary transformations. Table 1 contains various
examples of different functions defined by model 1, depend-
ing on the assumed definitions of T. Following are examples
of derivations of various dynamic site equations, based on
the above base model 1 and the definitions of the generic
variable T in Table 1 defined by Equations 2–6, as well as
any other possible transformations of the variable T, which
can be easily added by the reader.
ADA Derivations
Because model 1 is defined in a flexible manner, we can
derive from it various dynamic equations with different
levels of complexity. Let us assume that Y0 defines the
reference point at time T0. The ADA-based dynamic equa-
tion based on solutions for M is then an anamorphic model
of the following form:
YM � Y0�T/T0�b. (7)
The ADA-based polymorphic dynamic equation (with a
single asymptote) based on the solutions for the parameter b
is
Yb � M T�ln�Y0/M�/lnT0�. (8)
An example of another polymorphic model with a single
asymptote, based on the parameter a1 varying with site
productivity is the ADA reparameterization of model 1,
which, for example, for the Bailey (1980) function and
Cieszewski and Bella (1991a) function (Equation 2) is
Ya � M�1 � ���Y0
M��1/b�
� 1��t0��a2�
ta2�b
, (9)
where, according to Equation 2, T � 1 � e��a1 ta2�.
An equivalent polymorphic dynamic equation (Equation 2)
with a single asymptote for the same base function based on
using the solution for parameter a2 has the form,
Ya � M�1 � exp�� � a1
� �ln�-�Y0/M�1/b � 1�
ln�e�a1�ln� x�/ln�t0����b
. (10)
In the above examples, the ADA solutions are based on
assumptions of single parameter responses to the site pro-
ductivity variation. This approach results in either anamor-
phic models with variable asymptotes or polymorphic mod-
els with a single asymptote. To derive models with both
polymorphism and variable asymptotes, more than one pa-
rameter has to be a function of site productivity. The site
productivity responses in M and in b can be mixed, and in
the next section several derivations of models with both of
these parameters responding to site quality are presented.
Responses in parameter a of model 1 cannot be com-
bined with any other parameters. When the exponentiated
parameter a varies with site productivity, none of the other
two parameters M or b can be used (together with a) to
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4 Forest Science ●●(●) 2008
AQ: C
T1
AQ: D
model the site productivity responses because when M or b
is a function of X and the exponentiated a is also a function
of X, the model cannot be solved for X in a closed-form
solution. For this reason the only useful model with param-
eter a varying with site productivity is the ADA reparam-
eterization of model 1 similar to Equations 9 and 10 above
for the examples of a Chapman-Richards special case re-
sulting from combining Equation 1 and any of the special
cases of Equation 2.
GADA Derivations
To derive polymorphic models with variable asymptotes
it is necessary to apply the GADA presented by Cieszewski
(1994) and Cieszewski and Bailey (2000), which allows for
definition of site responses in multiple parameters. With use
of this approach the site responses in the Richards function
can be modeled using both parameters m and b. To facilitate
such derivation model 1 is reparameterized into a form more
suitable for manipulation of these two parameters (using em
instead of M and taking the log of the function) as follows:
Y � emTb, (11)
LY � m � b LT,
where LY is the natural logarithm of Y and LT is the natural
logarithm of T defined by any of the Equations 2–6.
If we assume that the site productivity can be defined by
an unobservable variable X, a few examples of assumptions
about the relationships between the parameters m and b and
the unobservable variable X are the parameters m and b are
linear functions of X, which means m can be proportional to
b or linearly inversely proportional to b; the parameter m is
a linear function of X, whereas the parameter b is an inverse
fractional function of X, which means that the parameters
are nonlinearly proportional to each other’s inverse, or the
parameters m and b are quadratic functions of X, which
means they can be in various flexible relationships to each
other.
Linear Assumptions
The simplest assumption is that both parameters are
linear functions of the unobservable site variable X:
m � m1 � m2 X, (13)
b � b1 � b2 X, (14)
which requires the solution for the unobservable variable X
in the equation,
LY � ml � m2 X � (b1 � b2 X)LT. (15)
The general solution for the above relationship is
X � ��LY � m1 � b1 LT
m2 � b2 LT. (16)
The self-referencing dynamic equation can be defined
using one known reference point, but to make the equation
parsimonious one of the parameters multiplying X should be
fixed. Because X is arbitrary, we can redefine it to make theTab
le1.
Dif
fere
nt
def
init
ion
sof
Tre
sult
ing
invar
ious
exponen
tial
funct
ions
def
ined
by
Equat
ion
1
Equat
ion
Nam
eof
model
/cit
atio
nD
efin
itio
nof
TR
esult
ing
subst
ituti
on
tom
odel
1
2(a
llfo
rb
�0)
Cie
szew
ski
and
Bel
la(1
991a)
;S
chnute
(1981):
a2
�1;
for
only
a1
�0,
also
:B
aile
y(1
980):
a2
Bail
ey
�1/a
2;
Ric
har
ds
(1959):
a2
�1;
Wei
bull
(1939):
b�
1,
M�
1;
Yan
get
al.
(1978):
b�
1
T�
�1�
e�a
1•t1
/a2
for
a1�
0
t1/a
2 for
a1
�0
Y�
�M�1
�e
�a1•t
1/a
2
�b
for
a1
�0
M1tb
/a2
ifa1
�0
3L
ogis
tic
(Rober
tson
1923)
T�
1
1�
e�
at
Y�
M�
1
1�
e��
at��b
4K
orf
and
Pri
spev
ak(1
939);
Sch
um
acher
(1939):
b�
1T
�e
�1
/tY
�M
(e1
/t)b
5G
om
per
tz(M
edaw
ar1940)
T�
e�
ea•t
Y�
M(e
�e
�a
t )b
6L
og-l
ogis
tic
(Monse
rud
1984)
T�
1
1�
e��
aln
�t��
Y�
M�
1
1�
e��
a1ln
�t��
b
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Forest Science ●●(●) 2008 5
model more parsimonious in one of the following ways,
according to which the Equations 1, 13, 14, and 16 offer the
following specific cases of dynamic equations.
CASE A (b1 � 0 and b2 � 1: the model must be
polymorphic):
Y � e�m1�m2 X0)TX0, (17)
where
X0 � �� LY0 � m1
m2 � LT0
. (18)
CASE B (m1 � 0 and m2 � 1: the asymptote must vary with
site productivity):
Y � eX0T�b1�b2 X0), (19)
where
X0 � �� LY0 � b1 LT0
1 � b2 LT0
. (20)
Inverse-Saturation Assumptions
The site parameters can be conditioned to be consistently
proportional to each other’s inverse over the site productiv-
ity dimension by the following definitions:
m � m1 � m2 Xi (21)
b � b1 �b2
X � b3, (22)
which define
LY � m1 � m2 X � �b1 �b2
X � b3�LT. (23)
There are two general solutions to Equation 23. The solution
more likely to be positive is
X � 0.5� � � 2 m2 b3 � ��2 �4 m2 LT b2
m2,
(24)
where
� � m1 � LY � m2 b3 � LT b1. (25)
Equation 23 defines a polymorphic model with variable
asymptotes. Similar to the previous example, because X is
arbitrary we can redefine this model to make it more par-
simonious, getting rid of redundant parameters. Two spe-
cific examples of parsimonious dynamic equations with
polymorphism and variable asymptotes implied by Equa-
tions 1, 21, 22, and 24 are presented below.
CASE A (b2 � 1 and b3 � 0: the model must be
polymorphic but may have a single asymptote if m2 � 0):
Y � e�m1�m2 X0)T�b1�1/X0), (26)
where the specific point solution using a known reference
point is
X0 � 0.5�� � ��2 � 4 LT0 m2
m2, (27)
and
� � LT0 b1 � LY0 � m1. (28)
Case B (m1 � 0 and m2 � 1: the model may be anamorphic
if b2 � 0):
Y � eX0T�b1�b2/X0�b3) (29)
where the specific point solution using a known reference
point is
X0 � �b3 � 0.5� � 0.5��2 � 4 LT0b2, (30)
and where
� � LT0b1 � LY0 � b3. (31)
Quadratic Assumptions
Finally, we assume a generic case of site productivity
influence on the model parameters, in which the site param-
eters can be inconsistently proportional over time, or in-
versely proportional, to each other, and their relationship
may be changing over time more than once. Such a com-
plicated relationship can be modeled, for example, by de-
fining m and b as proportional to different quadratic func-
tions of the unobservable site variable X:
m � m1 � m2 X � m3 X2, (32)
b � b1 � b2 X � b3 X2, (33)
which used in Equation 12 implies the general relationship,
LY � m1 � m2 X � m3 X2
� (b1 � b2 X � b3 X2)LT . (34)
The general solution for X in Equation 34 has two cases of
which that more likely to be greater than zero is
X �� � � ��2 � 2�b1 LT � m1 � LY�w
w, (35)
where
� � b2 LT � m2, (36)
and
w � 2 b3 LT � 2 m3. (37)
As in the earlier examples the self-referencing dynamic
equations can be defined using one known reference point,
but to assure that the final dynamic equation is parsimoni-
ous at least one of the parameters multiplying X should be
fixed. Six examples of specific variants of parsimonious
dynamic equations implied by the above Equations 1, 32,
33, and 35 are presented below.
CASE A (b � X: the model must be polymorphic without
the quadratic term or the intercept in b):
Y � e�m1�m2 X0�m3 X0
2
TX0, (38)
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6 Forest Science ●●(●) 2008
X0 �1
2
�� � ��2 � 4�m1 � LY0�m3
m3, (39)
where the specific point solution using a known reference
point is
and
� � m2 � LT0. (40)
CASE B (b2 � 1: the model must be polymorphic but the
quadratic term in b may be eliminated):
Y � e�m1 � m2 X0 � m3 X0
2)T(b1�X0�b3 X
0
2), (41)
where the specific point solution using a known reference
point is
X0 �� � � ��2 � 2�b1 LT0 � m1 � LY0�w
w,
(42)
and where
� � m2 � LT0, (43)
and
w � 2 b3 LT0 � 2 m3. (44)
CASE C (b3 � 1: the model must be polymorphic with fixed
quadratic term in b):
Y � e�m1�m2 X0�m3 X0
2)T(b1�b2 X0�X
0
2), (45)
where the specific point solution using a known reference
point is
X0 �� � � ��2 � 2�b1 LT0 � m1 � LY0�w
w,
(46)
and where
� � LT0b2 � m2, (47)
and
w � 2 LT0 � 2 m3. (48)
CASE D (m � X: the model must have variable asymptotes
with quadratic site response function in b):
Y � eX0T�b1�b2 X0�b3 X02) (49)
where the specific point solution using a known reference
point is
X0 �� � � ��2 � 2�b1 LT0 � LY0�w
w, (50)
and where
� � LT0b2 � 1, (51)
and
w � 2 LT0b3. (52)
CASE E (m2 � 1: the model must have variable asymptotes
with potentially either linear or quadratic site response
function in m):
Y � e�m1 � X0 � m3 X0
2
T(b1�b2 X0�b3 X0
2), (53)
where the specific point solution using a known reference
point is
X0 ��� � ��2 � 2�b1 LT0 � m1 � LY0�w
w, (54)
and where
� � LT0b2 � 1, (55)
and
w � 2 LT0b3 � 2 m3. (56)
CASE F (m3 � 1: the model must have variable asymptotes
with quadratic site response functions in m and potentially
in b but not necessarily):
Y � em1�m2 X0�X0
2)T(b1�b2 X0�b3 X
0
2) (57)
where the specific point solution using a known reference
point is
X0 �� � � ��2 � 2�b1 LT0 � m1 � LY0�w
w,
(58)
and where
� � LT0b2 � m2, (59)
and
w � 2 LT0b3 � 2. (60)
Discussion
Site-dependent modeling of self-referencing relation-
ships is more than a century old. Traditionally, forest
growth and yield modelers have used fixed base-age site
equations requiring iterative numerical searches for opera-
tional use (e.g., Ek 1971, Payandeh 1974b, Monserud
1984). Others tried to overcome the limitations of the earlier
simple dynamic equations by joining (splining) predictions
from multiple models into a common prediction system
(e.g., Bruce et al. 1984). Others (see examples in Bailey and
Cieszewski 2000 and in Haight 2001) have attempted to
derive base-age invariant dynamic equations producing in-
stead base-age variant models, such as Goelz and Burk
(1992), that generate different curves depending on selec-
tion of different base ages, as we discussed earlier in the
Background and Objectives section.
Derivation of advanced dynamic equations with poly-
morphism and variable asymptotes from the Richards-like
exponential functions is nontrivial. In recent years the dy-
namic equations have been becoming more frequently used,
although only a few modelers have so far used advanced
dynamic site equations with both polymorphism and vari-
able asymptotes based on the exponential functions (i.e.,
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Forest Science ●●(●) 2008 7
AQ: E
Duplat and Tran-Ha 1997, Cieszewski 2004, Krumland and
Eng 2005). The main challenge in developing dynamic
equations from the exponential functions lies in finding
suitable combinations of exponential and logarithmic func-
tions that can be mixed with other multiparameter functions
while providing appropriate close form solutions for the site
variable and allowing for derivation of proper base-age
invariant, closed form dynamic equations. The number of
possible base-age invariant dynamic equations that can be
derived with GADA is tightly controlled by the availability
of close form analytical solutions for the cross-sectional
component of the three-dimensional site equations. No
proper dynamic equations can be derived without such
solutions, and, therefore, the number of possible derivations
in this method is rather limited. Most of the practically
viable GADA-based solutions that are applicable to the
Richards-like family of exponential functions are presented
here. Although the solutions offered here were not possible
before the introduction of GADA, future improved methods
of dynamic equation derivation may offer other ways of
deriving base-age invariant dynamic equations with many
more solutions.
The advanced dynamic equations presented here have
broad potential for applications with various types of
growth data. Because these equations have been published
previously only in an internal report (i.e., Cieszewski 2004),
they have been practically unknown and have found rela-
tively little use so far. Nevertheless, several scientists have
explored the use of these new models for different species in
the United States and Europe. For example, Barrio Anta et
al. (2006) have found the Cieszewski (2004) model based
on the hybrid of a linear inverse function mixed with the
Korf function, which is defined by Equations 4 and 29 with
b3 � 0 the best for development of a basal area growth
system for maritime pine in northwestern Spain, and Adame
et al. (2006) found the Cieszewski (2004) model based on a
hybrid of the linear function mixed with the Bailey (1980)
model, which is here defined by Equations 2 and 19, the
best for modeling dominant height growth and site index
curves for rebollo oak (Quercus pyrenaica Willd.) in north-
west Spain. Barrio Anta et al. (2006) have considered some
of the equations presented here for modeling loblolly pine
height growth but in the end concluded that the Cieszewski
(2003) model fitted their data best.
Model selection among the multitude of possible equa-
tions depends on the data analyzed and the modeler’s ex-
perience and preferences. Given a high level of nonlinearity
in the modeled trends, there is no simple procedure leading
to finding and identifying the most suitable model. Gener-
ally, there are two main traditional approaches to model
selection, which can be described as top down and bottom
up. The top-down approach is based on fitting the most
flexible model and narrowing down its parameter space to
identify the most parsimonious solution. The most suitable
approaches for this are Equations 41, 45, 53, and 57. This
approach is typically very difficult and unstable with many
problems associated with lack of convergences, local con-
vergences, instability of parameters and excessive comput-
ing time required for finding the best parameter estimates.
However, its advantage is that in the hands of a skilled
practitioner it allows exploration of the greatest range of
possibilities in a relatively short time and identification of a
simpler model without missing its true trends, which can be
easily hidden by data artifacts associated with drawbacks of
various simple models. Schnute (1981) gives a good over-
view example of this type of approach and the consider-
ations associated with it. Because of the large potential for
local convergences, this approach should be repeated mul-
tiple times by using various initial parameter values.
The bottom-up approach is generally simpler. It starts out
dealing with multiple models that are simpler and easier to
fit than those used in the top-down approach. However, the
chance of missing the best possible fit in analysis is higher
because it never fully explores the whole multidimensional
space of the general model functionality. This approach can
also be very time-consuming because it requires fitting a
multitude of models, which will tempt the practitioner to
follow different paths of exploration and pose various chal-
lenges in choosing the best model of those with equal fit but
distinctly different behavior. In the end there is no golden
rule making developing self-referencing models easy. The
bottom line is the experience of the researcher in under-
standing numerical limitations of computer searches and in
familiarity with the modeled phenomena and what are their
most distinguishing and essential characteristics.
The functions defined in Table 2 contain two main
classes of GADA models, of which one is based on the
half-saturation function and one on the quadratic function.
The 10 different formulas in this table correspond to differ-
ent variants of the same models, which will behave similarly
within well-defined ranges of their parameters, but which
will have different convergence behavior at the limits of
definability of their parameter. Selection of the most suit-
able model form depends on data and model fitting behav-
ior. For example, if the initial analysis were done with
model 41 and the parameters m3, b1, and b3 turned out to be
redundant, the final selection would be model 17, which
would be more parsimonious than the original model.
Sample Applications
The two most typical applications of the material pre-
sented here are the fitting of the models to other data or to
other models (data) and the use of the methodology pre-
sented for derivation of other models not presented here. We
give some examples of such applications below.
Example of Top-Down Approach to ModelFitting Using Monserud (1984) Data
The Richards (1959) function is considered the paradigm
of growth and yield modeling, and it has been used for many
different species and variables around the world. Yet, Mon-
serud (1984) found that this model was not able to describe
inland Douglas-fir height growth satisfactorily. Site models
can fail to describe site-dependent height growth well be-
cause of lack of description of the temporal changes in the
height growth as a function of time, lack of description of
the cross-sectional changes in height as a function of site, or
both of these.
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8 Forest Science ●●(●) 2008
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T2
Because it is not clear which of the above was the reason
that Monserud (1984) found the Richards base function
unsuitable for his site model development, we choose the
temporal model definition equation (Equation 2) in Table 1
as one of the more general variants based on the Cieszewski
and Bella (1991a) function, which includes the Richards
(1959) function as a special case submodel. For the cross-
sectional definition of the model we choose Equation 49 in
Table 2 as one of the more general variants of the Cieszew-
ski (2004) models.
Next, we use the Monserud (1984) model to generate the
pseudo-data in Table 3 with the following equation and
parameters:
H ��S�
1 � exp�� � � ln�Age) � ln�S��, (61)
where � � 42.397, � � 0.3,488, � � 9.7,278, � � 1.2934,
and � 0.9779, H is height at age, and S is the site index
at base age 50 years.
In the course of model fitting it became evident that the
parameter b3 in Equation 49 was not contributing to the fit,
and, therefore, it was set to b3 � 0. As a result, the model
was collapsed to the form of Equation 19 (Table 2). We
made attempts to reduce the model further by trying to force
one of the parameters a1 or a2 to equal 1, but these attempts
appeared to have a relatively high cost in the sum or squared
residuals, which was the fitting criterion. On the other hand,
to improve the estimation properties for the model we had
reparameterized Equation 2 to have parameters a1 and a2 as
receptacles (i.e., T � 1 � e�ta2/a1
) of their values in Table 2.
The final model fit the Monserud (1984) model data well
Table 2. General GADA formulations of polymorphic dynamic equations with variable asymptotes based on the exponential class of base modelsincluding Richards, Weibull, Yang, and Bailey functions as special cases
Equation The main formulation The corresponding subequations
16 Y � e�m1 � m2 X0) TX0
X0 � �� LY0 � m1
m2 � LT0
18 Y � eX0T�b1 � b2 X0�
X0 � �� LY0 � b1 LT0
1 � b2 LT0
25 y � e�m1 � m2 X0�T�b1 � 1/X0�
X0 � 0.5� v � �v2 � 4 LT0m2
m2v � LT0b1 � LY0 � m1
28 Y � eX0T�b1 � b2/X0 � b3)X0 � � b3 � 0.5� � 0.5��2 � 4 LT0b2
v � LT0b1 � LY0 � b3
37 Y � e�m1 � m2 X0 � m3 X02�TX0
X0 �1
2
� v � �v2 � 4�m1 � LY0�m3
m3v � m2 � LT0
40 Y � e�m1 � m2 X0 � m3 X02)T(b1 � X0 � b3 X0
2)
X0 �� v � �v2 � 2�b1 LT0 � m1 � LY0�w
wy � m2 � LT0
w � 2b3 LT0 � 2 m3
44 Y � e�m1 � m2 X0 � m3 X02
)T(b1 � b2 X0 � X02)
X0 �� � � �v2 � 2�b1 LT0 � � LY0�w
wv � LT0b2 � m2
w � 2 LT0 � 2 m3
48 Y � eX0T�b1 � b2 X0 � b3 X02
X0 �� v � �v2 � 2�b1 LT0 � LY0�w
wv � LT0b2 � 1
w � 2 LT0b3
52 Y � e�m1 � X0 � m3 X02)T(b1 � b2 X0 � b3 X0
2
X0 �� � � ��2 � 2�b1 LT0 � m1 � LY0�w
wv � LT0b2 � 1
w � 2LT0b3 � 2 m3
56 Y � e�m1 � m2 X0 � X02�T�b1 � b2 X0 � b3 X0
2�
X0 �� v � �v2 � 2�b1 LT0 � m1 � LY0�w
w
v � LT0b2�m2
w � 2 LT0b3 � 2
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Forest Science ●●(●) 2008 9
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T3
(Figure 2) having a root mean square error equal to 0.205
foot (0.138 m), which is much below the usual measurement
error and the regression prediction error. The final model
had the form,
H � e���V�W b2)/(1�W b1)](1 � e(a2/a1)(b2-b1V)/1�W b1)
, (62)
where
W � ln�1 � e�t0a2
/a1�� and V � ln� 1
H0�;
H is the prediction of height at age t; H0 is a known
reference height at age t0; a1, a2, b1, and b2 are the model
estimable parameters with the estimated values of 9.998,
0.6399, �1.519, and 10.216; and the code for the model is
H � exp{-(ln(1/H0)�ln(1-exp[-1/a1�t0�a2])�b2)/�1
� ln(1-exp(-1/a1�t0�a2))�b1)} � (1-exp(-1/a1�
t�a2))�[-(b1�ln(1/H0)-b2)/(1�ln(1-exp(-1/a1�t0�a2))�b1)].
The top-down approach to model fitting described above
allowed us to find a parsimonious and reasonably well-fit-
ting model for the data considered and to confirm that even
in the presence of an overly flexible cross-sectional defini-
tion of the site model, the Richards (1959) base function is
not flexible enough to model the age-dependent height
growth changes in inland Douglas-fir stands identically to
the Monserud (1984) model.
Example of Extending the Approach to DeriveOther Models Based on Logarithmic Functions
The methodology presented here can be applied to any
base equations that can have a similar structure identified as
defined by Equation 1. Consider, for example, the following
logarithmic equation, which is particularly suitable for mod-
eling early rapid height growth of intensively managed
loblolly pine plantations:
H � a ln�Ctb � d�, (63)
that can be rewritten as
H � a ln�ectb � d�. (64)
By setting Y � e(H/a) � d, we define an equation similar to
Equation 1, that is,
Y � ectb. (65)
After we assume that t � T the above model can be
applied directly with the solutions presented in Table 2 to
formulate appropriate dynamic equation of the form Y �
ef1(X)tf2(X), which subsequently can be used with the solu-
tions for X as a dynamic equation Y � fL(t, t0, y0). After that
point the function fL needs to be reformulated to its original
untransformed form:
H � a ln�ef1�X�tf2�X� � d�, (66)
with an appropriate solution (Table 2) for X:
X0 � f3�t0, Y0�, (67)
where Y0 � e(H0/a) � d which completes the derivation of
the dynamic equation from the logarithmic function.
Summary
This report provides a description of a relatively simple
exercise in algebra that solves problems that lingered, un-
solved despite various attempts for most of the 20th century
(more than 70 years). We present some traditional ADA-
based dynamic equations that are either anamorphic or
Table 3. Pseudo-data of height growth above breast height generated using the Monserud (1984) height model
Age
Site index base age 50
40 50 60 70 80 90
10 17.75 15.32 12.96 10.67 8.46 6.3515 28.28 24.56 20.90 17.30 13.81 10.4420 38.62 33.72 28.86 24.04 19.30 14.6925 48.46 42.55 36.62 30.69 24.80 19.0030 57.70 50.92 44.06 37.14 30.19 23.2935 66.29 58.78 51.12 43.32 35.43 27.5040 74.23 66.11 57.77 49.22 40.48 31.6245 81.55 72.93 64.02 54.81 45.33 35.6250 88.30 79.26 69.86 60.09 49.95 39.4855 94.51 85.13 75.33 65.07 54.36 43.2060 100.23 90.58 80.43 69.76 58.55 46.7865 105.50 95.62 85.20 74.18 62.53 50.2170 110.36 100.31 89.65 78.34 66.30 53.5075 114.85 104.66 93.81 82.25 69.89 56.6680 119.01 108.70 97.70 85.93 73.28 59.6785 122.86 112.47 101.35 89.40 76.50 62.5590 126.44 115.98 104.76 92.66 79.56 65.3195 129.76 119.25 107.95 95.74 82.46 67.95100 132.86 122.32 110.96 98.64 85.21 70.47105 135.74 125.18 113.78 101.38 87.82 72.88110 138.44 127.87 116.43 103.97 90.31 75.19115 140.96 130.39 118.93 106.42 92.67 77.39
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10 Forest Science ●●(●) 2008
F2
polymorphic with single asymptotes and many new GADA-
based dynamic equations with both polymorphism and vari-
able asymptotes. Equations 7 and 8 represent ADA general
formulations, each of which defines five different models
depending on which of the relationships in Table 1 is used
to define the variable T in the model considered. Table 2
contains two main classes of GADA-based general formu-
lations that are based on the half-saturation and quadratic
functions. Each class has several variants of the models
relating to the limiting parameter values of the models and
a model convergence toward other models. Each of the 10
model variants in Table 2 can be applied with any of the five
different functions T in Table 1 to define a dynamic equa-
tion with polymorphism and variable asymptotes. The mod-
els presented are suitable for site-dependent height growth
modeling as well as for any other growth and yield model-
ing involving the use of unobservable variables substituted
by the self-referencing type of model definition. The models
presented can be used as implicitly defined integral equa-
tions, such as site index models, or as difference equations
(Tait et al. 1988, Cieszewski and Bella 1993) and applied in
a state-space approach to growth modeling (Garcia 1994),
which iterate on an annual basis interacting with dynami-
cally changing environmental factors.
Unlike the mathematically malformed and ill-condi-
tioned, internally inconsistent base-age variant models in
the works refuted in Bailey and Cieszewski (2000), the
equations provided here were derived with a process of rigid
algebraic operations, are mathematically sound, and can be
used in any mathematically sound implementation (e.g.,
iterated on an annual or periodic basis, in single- or multi-
ple-step predictions, as well as in forward or backward
computations). If used as site models, the equations pro-
vided can be treated as both height and site index equations
that are compatible with each other. All models presented
Figure 2. Fit of Cieszewski (2004) cross-sectional model 18 with time series model 2a (Fit Ch-R) to the Monserud (1984)height model data (Mon_H.
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Forest Science ●●(●) 2008 11
here are base-age invariant, path-invariant, parsimonious,
internally consistent, and mathematically sound.
Endnote
[1] This terminology follows a time-honored tradition in mathematics,according to which situations that elude simple analysis are dismissedby pejorative such terms as “improper,” “inadmissible,” “degener-ate,” “irregular,” and so on (Simmons 1972).
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