# Initial Error Growth and Predictability of Chaotic Low-dimensional Atmospheric Model

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## Abstract

The growth of small errors in weather prediction is exponential on average. As an error becomes larger, its growth slows down and then stops with the magnitude of the error saturating at about the average distance between two states chosen randomly. This paper studies the error growth in a low-dimensional atmospheric model before, during and after the initial exponential divergence occurs. We test cubic, quartic and logarithmic hypotheses by ensemble prediction method. Furthermore, the quadratic hypothesis suggested by Lorenz in 1969 is compared with the ensemble prediction method. The study shows that a small error growth is best modeled by the quadratic hypothesis. After the error exceeds about a half of the average value of variables, logarithmic approximation becomes superior. It is also shown that the time length of the exponential growth in the model data is a function of the size of small initial error and the largest Lyapunov exponent. We conclude that the size of the error at the least upper bound (supremum) of time length is equal to 1 and it is invariant to these variables. Predictability, as a time interval, where the model error is growing, is for small initial error, the sum of the least upper bound of time interval of exponential growth and predictability for the size of initial error equal to 1.

## Keywords

Chaos planetary atmospheres prediction methods error analysis modeling## 1 Introduction

Due to the fact that the atmosphere is a chaotic dynamical system, the growth of small errors in weather prediction is exponential. In the case of sufficiently small initial error, the governing equations can be linearized, which leads to exponential growth of the error. Generally, whether an error is small enough to guarantee the exponential growth depends on the specific meteorological conditions and/or the model under study. The issue of small errors growth in the context of the model studied in this paper was also addressed in[1, 2, 3, 4, 5]. For a more comprehensive introduction to the problem of weather predictability we refer readers to the book of Palmer and Hagedorn[6].

If the system which governs the change of the error is linear, then the exponential growth will continue unabated. The earth’s atmosphere is a non-linear system and as the error becomes larger, the growth rate decreases. Eventually, all systematic growth should stop and the size of the error should be equal to the average size of the distance of two randomly chosen states.

Predictability and average initial error growth for numerical weather prediction models (NWPM) are still in the focus of researchers, e.g. [7, 8]. Analysis of the last mentioned growth was firstly performed by Lorenz[9] in 1969. He introduced a quadratic hypothesis which is based on the assumption that if the principal nonlinear terms in the atmospheric equations are quadratic, then the nonlinear terms in the equations governing the field of errors will also be quadratic but he could not prove this theory, because the method that has to be adopted (for NWPM we know just model state and we do not know the real state) gives limited number of initial error sizes and limited available data for valid approximation. This problem is still present. In this case, it is a logical step to use a less complex experimental model that gives the possibilities to choose “real” and model states and to choose the number of approximated data. The present study attempts to examine this hypothesis, using the low-dimensional atmospheric model introduced by Lorenz in 1996[10].

Even for systems with exponential error growth, it does not start right from the initial time, and we observe the transient behavior instead. After the transient behavior dies out and exponential growth follows, the time length of this part will be governed by the size of small initial error and by the model parameters. Predictability, as a time interval where the model error is growing, is also expected to be a function of the above mentioned errors and parameters. We also investigate this phenomenon.

Some results on the topic were published by us in a more compact form in [1].

## 2 Model

*N*variables

*X*

_{1}, ⋯,

*X*

_{ N }connected by governing equations:

*X*

_{ n }

_{−2},

*X*

_{ n }

_{−1},

*X*

_{ n },

*X*

_{ n+}

_{1}are unspecified (i.e., unrelated to actual physical variables) scalar meteorological quantities,

*F*is a constant representing external forcing, and

*t*is time. The index is cyclic so that

*X*

_{ n−N }=

*X*

_{ n+N }=

*X*

_{ n }, and the variables can be viewed as existing around a circle. The nonlinear terms of (1) simulate advection. The linear terms represent mechanical and thermal dissipation. The model can quantitatively describe the weather system to a certain extent; but instead of the well-known Lorenz’s model of atmospheric convection[11], (1) cannot be derived from any atmospheric dynamic equations. The motivation was to formulate the simplest possible set of dissipative chaotically behaving differential equations that share some properties with the “real” atmosphere. In [2, 3], the reasoning for usability of such a model was discussed in more detail.

*N*= 36, so each sector covers 10 degrees of longitude. Parameters

*F*were selected equal to 8, 9 and 10, successively. We first choose arbitrary values of the variables, and use a fourth order Runge-Kutta method with a time step Δt = 0.05 or 6 hours, we integrate forward for 14400 steps, or 10 years. We then use the final values, which should be more or less free of transient effect. For individual parameters

*F*, we estimate the global largest Lyapunov exponents

*λ*

_{max}by the method of numerical calculation presented in [12]. We gradually get

By the definition in [9], a bounded dynamical system with a positive Lyapunov exponent is chaotic. Because all values of the largest Lyapunov exponents of the model are positive and the system is bounded[2, 3, 4], its chaoticity has been established for all three values of *F*. Strictly speaking, we also need to exclude the asymptotically periodic behavior, but such a task is impossible for numerical simulation to fulfill. The choice of parameters *F* and time unit = 5 days is made to obtain the same values of the largest Lyapunov exponents as the state of the art models of complete global atmospheric circulation.

## 3 Ensemble prediction method

*e*

_{ n }

_{0}and letting \(X_{n0}^\prime = {X_{n0}} + {e_{n0}}\) be the “observed” initial value of

*N*variables. We then integrate forward from the true and the observed initial state, for 50 days (

*K*= 200 steps), obtaining

*N*sequences

*X*

_{ n }

_{0}, ⋯,

*X*

_{ n }and \(X_{n0}^\prime, \cdots, X_{nK}^\prime \). After that, we let \({e_{nk}} = X_{nK}^\prime - {X_{nk}}\) for all values of

*k*and

*n*. To get more representative values, we make a total of

*M*= 250 runs in the same manner by letting new values of

*X*

_{ n }

_{0}be the old values of

*X*

_{ nK }in each run. Finally, we let

*N*values, where

*τ*=

*kΔt*is the predictable range and

*M*values. The logarithmic average is chosen because of its suitability for comparison with growth governed by the largest Lyapunov exponent. For further information, see [13, 14, 15].

## 4 Quadratic hypothesis

*E*(

*t*) is a distance at time

*t*between two originally nearby trajectories; and

*a, b*are constants. The quadratic hypothesis is also used to describe the behavior of initial error growth, for example in [16, 17].

### 4.1 Method

Because we want to study behavior of (2), we make differences \({y_k} = {{\left( {E\left( {\tau + \Delta t} \right) - E\left( \tau \right)} \right)} \over {\Delta t}}\) points \({x_k} = {{\left( {E\left( \tau \right) + E\left( {\tau + \Delta t} \right)} \right)} \over 2}\), where *E* is average initial error growth calculated from the ensemble prediction method (Section 3).

*x*

_{ k },

*y*

_{ k }). The interpolation equations are

Equation (2) represents the examined quadratic hypothesis. The alternative forms (3) and (4) are added, because Lorenz[9] noticed that the cubic and quartic equations would also fit his data. Equation (5) is chosen because if \(Q\left( t \right) = \ln \left( {\overline {E\left( t \right)} } \right)\) with *Ē* being the normalized *E*, then \({{{\rm{d}}Q\left( t \right)} \over {{\rm{d}}t}} = a\left( {1 - {{\rm{e}}^{Q\left( t \right)}}} \right)\) represents the quadratic hypothesis. In [18], it was assumed that linear fit \({{{\rm{d}}Q\left( t \right)} \over {{\rm{d}}t}} = - aQ\left( t \right)\) is superior to the quadratic hypothesis. Parameters *a* and *b* in (2–5) are examined and discussed in the next section.

### 4.2 Results

*e*

_{0}exhibit different behaviors of an error growth. To study that, we selected six magnitudes of \(||{e_0}||\) for each \(F:\, \Vert e_{0,1} \Vert = 0.0001,\, \Vert e_{0,2} \Vert = 0.001,\, \Vert e_{0,3} \Vert = 0.01,\, \Vert e_{0,4} \Vert = 0.1,\, \Vert e_{0,5} \Vert = 0.6,\, \Vert e_{0,6} \Vert = 1\), where ∥ · ∥ marks the Euclidean norm. The interpolation equations were tested for all three values of parameter

*F*and initial error

*e*

_{0}. Table 1 shows the RMS error between values obtained from the ensemble prediction and from the interpolation equations. The error is divided by the average value of \({{\left( {E\left( {\tau + \Delta t} \right) - E\left( \tau \right)} \right)} \over {\Delta t}}\). Fig. 1 displays the error growth rate \({{{\rm{d}}E} \over {{\rm{d}}t}}\) versus

*E*for all parameters

*F*and for

*e*

_{0,2},

*e*

_{0,4}and

*e*

_{0,5}. Each interpolation equation gives specific values of

*a*and

*b*for particular

*F*and e

_{0}. Our aim is to find a general description of

*a*and

*b*by well-known parameters of the system. The early growth rate should be close to \({{{\rm{d}}E} \over {{\rm{d}}t}} = {\lambda _{\max }}E\). That means

*a*=

*λ*

_{max}for all interpolation equations. Results for (2–4) are the following. The constant

*a*measures the growth rate of small errors, the quadratic (cubic, quartic) term has to be negative if

*a*is positive, since it is the only factor that can stop the growth. If

*E*is normalized such that the value which it approaches as

*t → ∞*is unity,

*b = a*. For unnormalized \(E,b = {{{\lambda _{\max }}} \over {{E^ * }}}\) for (2), \(b = {{{\lambda _{\max }}} \over {{E^ * }^2}}\) for equation (3) and \(b = {{{\lambda _{\max }}} \over {{E^ * }^3}}\) for (4), where

*E**denotes the saturation value for

*E*. For (5), then \(b = {1 \over {{E^ * }}}\).

RMS error between values obtained from the ensemble prediction and from the interpolation equations. The error is divided by the average value of \({{\left( {E\left( {\tau + \Delta t} \right) - E\left( \tau \right)} \right)} \over {\Delta t}}\) displayed in percent. Gray cells mark values with the best results

Percent error | |||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|

Interpolation equation | Initial error | 0.0001 | 0.001 | 0.01 | 0.1 | 0.6 | 1 | ||||||||||||

| 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | |

| 16 | 19 | 12 | 13 | 11 | 13 | 16 | 12 | 14 | 16 | 15 | 14 | 34 | 27 | 29 | 47 | 41 | 36 | |

| 23 | 27 | 22 | 23 | 22 | 20 | 21 | 22 | 25 | 29 | 25 | 27 | 40 | 38 | 38 | 53 | 50 | 51 | |

| 30 | 29 | 32 | 30 | 29 | 28 | 28 | 33 | 32 | 37 | 32 | 35 | 48 | 44 | 43 | 60 | 52 | 55 | |

| 20 | 21 | 19 | 22 | 23 | 21 | 22 | 22 | 22 | 22 | 25 | 21 | 26 | 21 | 23 | 39 | 31 | 34 |

*a*and

*b*would make the inaccuracy of cubic and quartic hypotheses even greater. Therefore, we will from now on work only with quadratic and logarithmic hypotheses. Table 2 shows the RMS error between values obtained from the ensemble prediction and from (2–5), where parameters

*a*and

*b*are the expected theoretical values. We can see a higher increase of the percent error for (5) than for (2). The difference between Table 2 and Table 1 is displayed in Table 3.

The RMS error between values obtained from the ensemble prediction and from (2, 5), where parameters *a* and *b* are the expected theoretical values. The error is divided by the average value of \({{\left( {E\left( {\tau + \Delta t} \right) - E\left( \tau \right)} \right)} \over {\Delta t}}\) displayed in percent

Percent error | |||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|

Interpolation equation | Initial error | 0.1 | 0.1 | 0.1 | 0.1 | 0.6 | 1 | ||||||||||||

| 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | |

| 32 | 25 | 29 | 30 | 20 | 19 | 22 | 20 | 16 | 18 | 13 | 15 | 34 | 29 | 28 | 48 | 45 | 40 | |

| 97 | 89 | 94 | 83 | 85 | 82 | 73 | 77 | 84 | 73 | 63 | 72 | 42 | 41 | 46 | 39 | 36 | 34 |

Percent error | |||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|

Interpolation equation | Initial error | 0.0001 | 0.001 | 0.01 | 0.1 | 0.6 | 1 | ||||||||||||

| 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | |

| 16 | 6 | 17 | 17 | 9 | 6 | 6 | 8 | 2 | 2 | 2 | 1 | 0 | 2 | 1 | 1 | 4 | 4 | |

| 67 | 68 | 75 | 61 | 62 | 61 | 51 | 55 | 62 | 51 | 38 | 51 | 16 | 20 | 23 | 0 | 5 | 0 |

## 5 Exponential growth and predictability

Usability of the exponential model of initial error growth is depended on the size of initial error as well as the model parameter *F*. In the introduction, we mentioned that the exponential growth \({E_{\exp }}\left( t \right) = {e_0}{{\rm{e}}^{\left( {{\lambda _{\max }}t} \right)}}\) governed by the largest Lyapunov exponent *λ* _{max} occurs in the case of a sufficiently small initial error *e* _{0}. In this section, we present sizes of this initial error and therefore the usability of the exponential model.

Predictability *t* _{ p } is the time interval where systematic growth of initial error occurs and the size of this error is smaller than the average size of the distance of two randomly chosen states. This section also focuses on the dependence of *t* _{ p } on the size of initial error, parameter *F* and on the possible connection between predictability and exponential growth.

### 5.1 Method

*E*obtained from the Lorenz’s model and exponential growth (Fig. 2), we can hardly decide whether the exponential growth happens or not. We could get same guesses for predictable time read from graphs of time evolution of

*E*(Fig. 2), but we would rather relate it to a better specified value instead of the saturated value

*E**. In both cases we want to get more precise values and accuracy, therefore we have to introduce a more sophisticated method. This method was developed from the assumption that if the exponential growth is present, then the ratio of the two average errors

*E*calculated from ensemble prediction method (Section 3) in two following time steps Δ

*t*is

*G*(

*τ*) = 0. Through the use of

*G*, we analyze exponential growth and predictability.

### 5.2 Results

*G*is calculated for a variety of initial errors

*e*

_{0}and parameters

*F*. We again choose six magnitudes of ∥

*e*

_{0}∥ for each parameter

*F*: ∥

*e*

_{0,1}∥ = 0.0001, ∥

*e*

_{0,2}∥ = 0.001, ∥

*e*

_{0,3}∥ = 0.01, ∥

*e*

_{0,4}∥ = 0.1, ∥

*e*

_{0,5}∥ = 0.2, ∥

*e*

_{0,6}∥ = 1, where ∥ · ∥ marks the Euclidean norm. In Table 4, the time interval

*t*

_{ e }, during which results from ensemble prediction method are close to the theoretical exponential growth, is displayed for each initial error

*e*

_{0}and each parameter of

*F*. In the same table, predictability

*t*

_{ p }(length of time interval where

*E*is growing) is also displayed. Fig. 3 shows time evolution of function

*G*for all

*F*and

*e*

_{0,2},

*e*

_{0,4},

*e*

_{0,5}.The experimental data oscillate around theoretically expected values, and therefore intervals

*t*

_{ e }and

*t*

_{ p }are measured as the length with similar oscillation around theoretically expected values rather than an exact match. Table 4 and Fig. 3 also illustrate that the exponential growth is present for

*e*

_{0}which is smaller than

*e*

_{0,4}= 0.1 and never starts at the beginning of the growth. There is always a wave that precedes it (it can also be seen in Table 3) and its length is similar throughout the spectrum of

*F*and

*e*

_{0}. To analyze this behavior further, we focus on the dependence of the least upper bound (supremum)

*t*

_{ e,u }of time interval

*t*

_{ e }and predictability

*t*

_{ p }on natural logarithm of initial errors from

*e*

_{0,1}to

*e*

_{0,4}for all parameters of

*F*(Fig. 4) and on natural logarithm of initial errors from

*e*

_{0,1}to

*e*

_{0,6}(Fig. 5) in the second case.

Time interval *t* _{ e }, where results from the ensemble prediction method are close to theoretical exponential growth (N means negative result) and predictability *t* _{ p } (time intervals, where *E* is growing) for each initial error *e* _{0} and each parameter F

| 0.0001 | 0.001 | 0.01 | 0.1 | 0.2 | 1 | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|

| 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 | 8 | 9 | 10 |

| (6; 27) | (5; 23) | (4;20) | (5; 21) | (5; 18) | (4; 15) | (5;14) | (4;11) | (4; 10) | 6 | 5 | 4 | N | N | N | N | N | N |

| 49 | 40 | 32 | 42 | 34 | 27 | 35 | 27 | 22 | 28 | 21 | 17 | 25 | 19 | 15 | 20 | 15 | 12+ |

*t*

_{ e,u }as well as between

*t*

_{ p }and ln (

*e*

_{0}). To get more information, we linearly interpolated the experimental data. The interpolation equations

*t*

_{ e,u }(

*e*

_{0}) and

*t*

_{ p }(

*e*

_{0}) for all parameters

*F*were

*c*is close to 0 for all

*F*.Coefficient

*f*is the same as

*t*

_{ p }of

*e*

_{0,6}for all

*F*. Coefficients

*d*and

*h*are similar to each other. Theoretically, possible values for the coefficients come from the definition of exponential growth

If we compare it with *d* and *h*, we see similarity of the results.

*t*

_{ p }(

*t*

_{ e,u }) (Fig. 6) is linear:

If the exponential growth is present, *t* _{ p } is equal to *t* _{ e,u } plus *e* _{0,6} for all parameters of *F*.

## 6 Discussion

*λ*

_{max}is the largest Lyapunov exponent and

*E**is the saturated value of

*E*.

*Ė*, then the quadratic law (2) fits the best for

*e*

_{0}up to about 0.1. For higher values, it is better to use logarithmic law (5). On the other hand, if we want to estimate parameters of the model or use (9, 10) directly, it is, according to Fig. 2, Table 2 and Table 3, better to use (9) for

*e*

_{0}= 〈0; 1〉 and (10) for

*e*

_{0}= 〈1; 2〉. The reason for the difference can be found in Fig. 7. We can estimate that the best result for (2) is the range of

*e*

_{0}between 0.001 and 0.1 and for (5) we obtain the range of

*e*

_{0}between 1 and 1.5. The difference between theoretical and experimental data for parameter

*a*is much higher for (5) than for (2) and parameter

*b*in (5) is inside the logarithmic function and therefore any possible difference would be increased by this function.

*X*

_{1}, ⋯,

*X*

_{ N }vary between approximately −6 and +12. Fig. 8 shows time variations of

*X*during a period of 180 days. The average value \(\overline{X} \) of

*X*

_{ n }is 2, which means that for \( e_0 \leqslant \over{\overline{X}}{2}\), it is better to use (9) and for \( e_0 \geqslant \over{\overline{X}}{2}\) it is better to use logarithmic law (10). This is in good agreement with [18], where the same was suggested. Solutions of (9) and (10) are

The maximum sufficiently small initial error with the exponential growth of *E* (*t*) is *e* _{0} = 0.1 (according to Table 4 and Fig. 3). If we take a look at the validity of quadratic hypothesis with experimental parameters, we can see the same maximal value. We can speculate that it is not a coincidence that a sufficiently small error is directly connected with the quadratic hypothesis, and that if we use a sufficiently small initial error, then the growth will be governed by (9).

The greatest lower bound (infimum) *t* _{ e,l } of the time interval *t* _{ e } has a similar value across the spectrum of *e* _{0} (Table 4), and we did not find any interpolation equation. The behavior of *E* (*t*) from the ensemble prediction approach before the exponential growth takes place has a similar form for all *F* and *e* _{0} (Table 4, Figs. 2 and 3). Errors measured by ensemble prediction approach are approximately decreasing during the first 0.3 days and after 0.5 days it is approximately as large as *e* _{0}. Exponential growth overestimates the error for approximately the first 1.3 days, while underestimates it (till *t* _{ e,l }) later. The maximum of this wave behavior occurs approximately at 2.3 days. Same behavior was also observed for *e* _{0} ⩾ 0.1. To explain it we have to remind the definition of Lyapunov exponent as a long-term average characteristic. As stated in [19, 20], the error growth differs from the one established from Lyapunov exponent for the first few days. That is true not only for low dimensional models, but also for more complex global atmospheric circulation models.

*t*

_{ e,u }of time interval

*t*

_{ e }follows (6), which can be generally written as

*E*

_{ e,u,theoretical}is invariant to all

*e*

_{0}and

*F*. In Fig. 9, we can see that

*E*

_{ e,u }from the ensemble prediction approach is very similar.

*e*

_{0}= 〈0; 1〉 and (10) for

*e*

_{0}= 〈1; 2〉, and again we dare to say that it is not a coincidence that the value of 1 plays a role in both. Equation (7) approximating predictability

*t*

_{ p }(length of the time interval, where

*E*is growing) with theoretical parameters

*f*and

*h*can be written as

*e*

_{0}= 1. We did not find any general expression for \({t_{p,{e_0} = 1}}\). The second part of the expression represents

*t*

_{ e,u,theoretical}and for

*e*

_{0}∈ (0; 0.1), (15) can be rewritten into

_{0}∈ (0; 0.1) the increase in predictability time

*t*

_{ p }is due to the increase in time length of the exponential growth

*t*

_{ e,u }. The maximum predictability governed by (11) is 49 days for

*F*= 8 and

*e*

_{0,1}. The lower predictability, governed by (12), is 12 days for

*F*= 10 and

*e*

_{0,6}(Table 4).

## 7 Conclusion

This article focuses on analyzing the average error growth in a low-dimensional atmospheric model[10]. Theoretical hypotheses with experimental and theoretical coefficients and exponential model are compared with the ensemble prediction method for different initial errors and model parameters. Dependence of predictability and validity of exponential growth on lastly mentioned errors and parameters is also studied.

The important resulting values are 0.1 and 1. Value 0.1 is border for hypotheses with experimental coefficients, and it is also the maximum sufficiently small initial error with exponential growth. If the initial error is smaller than 0.1, then it is better to use quadratic hypothesis. If it is bigger, then the logarithmic hypothesis becomes superior. Value 1 is border for hypotheses with theoretical coefficients, and it is also the size of the error at least upper bound (supremum) of time length of exponential growth for all sufficiently small initial errors and model parameters. If the initial error is smaller than 1, then it is better to use quadratic hypothesis. If it is bigger, then the logarithmic hypothesis becomes superior. Predictability, as a time interval where the model error is growing, is, for small initial error, the sum of the least upper bound of time interval of exponential growth and the predictability for the size of initial error equal to 1 as shown in (16). The least upper bound of time interval of exponential growth is negatively proportional to Lyapunov exponent and directly proportional to natural logarithm of small initial error as shown in (15). Exponential growth does not start from the beginning of error growth and the greatest lower bound of time interval of exponential growth has similar values across the spectrum of sufficiently small initial errors.

It is in relatively good agreement, e.g., [7, 8], with the ability and predictability of the current meteorological models (the predictability is approximately two weeks).

This number (two weeks) itself cannot be transferred to dynamic systems of a different nature (nonlinear oscillators, mechanical systems, etc.). When studying the predictability of other systems it is possible to use the methodology of our article, for example, a combination of approach using Lyapunov exponents and ensemble prediction or estimation error growth depending on its stage.

## References

- [1]H. Bednar A. Raidl, J. Mikšovský. Initial errors growth in chaotic low-dimensional weather prediction model. In
*Proceedings of Nostradamus International Conference on Prediction, Modeling and Analysis of Complex Systems*, Springer, Nostradamus, Ostrava, Czech Republic, vol. 210, pp. 333–342, 2013.Google Scholar - [2]E. N. Lorenz, K. A. Emanuel. Optimal sites for supplementary weather observations: Simulation with a small model.
*Journal of the Atmospheric Sciences*, vol. 55, no. 3, pp. 399–414, 1998.CrossRefGoogle Scholar - [3]E. N. Lorenz. Designing chaotic models.
*Journal of the Atmospheric Sciences*, vol. 62, no. 5, pp. 1574–1587, 2005.CrossRefMathSciNetGoogle Scholar - [4]S. Herrera, D. Pazó, J. Fernández, M. A. Rodríguez. The role of large-scale spatial patterns in the chaotic amplification of perturbations in a Lorenz’96 model.
*Tellus Series A — Dynamic Meteorology and Oceanography*, vol. 63, no. 5, pp. 978–990, 2011.CrossRefGoogle Scholar - [5]H. M. Arnold, I. M. Moroz, T. N. Palmer. Stochastic parametrizations and model uncertainty in the Lorenz’96 system.
*Philosophical Transactions of the Royal Society A — Mathematical Physical and Engineering Sciences*, vol. 371, no. 1991, 20110179, 2013.Google Scholar - [6]T. Palmer, R. Hagedorm.
*Predictability of Weather and Climate*, Cambridge, UK: Cambridge University Press, pp. 1–702, 2006.CrossRefGoogle Scholar - [7]L. S. R. Froude, L. Bengtsson, K. I. Hodges. Atmospheric predictability revisited.
*Tellus Series A — Dynamic Meteorology and Oceanography*, vol. 65, pp. 1–13, 2013.Google Scholar - [8]L. Magnusson, E. Kallen. Factors influencing skill improvements in the ECMWF forecasting system.
*Monthly Weather Review*, vol. 141, no. 9, pp. 3142–3153, 2013.CrossRefGoogle Scholar - [9]E. N. Lorenz. Atmospheric predictability as revealed by naturally occurring analogs.
*Journal of the Atmospheric Sciences*, vol. 26, no. 4, pp. 636–646, 1969.CrossRefGoogle Scholar - [10]E. N. Lorenz. Predictability: A problem partly solved. In
*Proceedings of Seminar on Predictability*, CMWF, Reading, Berkshire, UK, vol. 1, pp. 1–18, 1996.Google Scholar - [11]E. N. Lorenz. Deterministic nonperiodic flow.
*Journal of the Atmospheric Sciences*, vol. 20, no. 2, pp. 130–141, 1963.CrossRefGoogle Scholar - [12]J. C. Sprott.
*Chaos and Time-Series Analysis*, New York, USA: Oxford University Press, pp. 1–507, 2003.MATHGoogle Scholar - [13]A. Trevisan. Impact of transient error growth on global average predictability measures.
*Journal of the Atmospheric Sciences*, vol. 50 no. 7, pp. 1016–1028, 1993.CrossRefMathSciNetGoogle Scholar - [14]R. Q. Ding, J. P. Li. Comparisons of two ensemble mean methods in measuring the average error growth and the predictability.
*Acta Meteorologica Sinica*, vol. 25, no. 4, pp. 395–404, 2011.CrossRefGoogle Scholar - [15]R. Benzi, F. C. Carnevale. A possible measure of local predictability.
*Journal of the Atmospheric Sciences*, vol. 46, no. 23, pp. 3595–3598, 1989.CrossRefMathSciNetGoogle Scholar - [16]E. N. Lorenz. Atmospheric predictability experiments with a large numerical model.
*Tellus*, vol. 34, no. 6, pp. 505–513, 1982.CrossRefGoogle Scholar - [17]L. Bengtsson, K. I. Hodges. A note on atmospheric predictability.
*Tellus*, vol. 58, no. 1, pp. 154–157, 2006.CrossRefGoogle Scholar - [18]A. Trevisan, P. Malguzzi, M. Fantini. On Lorenz’s law for the growth of large and small errors in the atmosphere.
*Journal of the Atmospheric Sciences*, vol. 49 no. 8, pp. 713–719, 1992.CrossRefGoogle Scholar - [19]J. Smagorinsky. Problems and promises of deterministic extended range forecasting.
*Bulletin of the American Meteorological Society*, vol. 50, no. 5, pp. 286–311, 1969.Google Scholar - [20]E. N. Lorenz. Deterministic nonperiodic flow.
*Journal of the Atmospheric Sciences*, vol. 20, no. 2, pp. 130–148, 1963.CrossRefGoogle Scholar - [21]E. W. Weisstein.
*Runge-Kutta method*, [Online], Available: http://mathworld.wolfram.com/Runge-KuttaMethod.html, September 11, 2013. - [22]J. D. Lambert, D. Lambert.
*Numerical Methods for Ordinary Differential Systems: The Initial Value Problem*, New York, USA: Wiley, pp. 149–205, 1991.MATHGoogle Scholar - [23]J. H. E. Cartwright, O. Piro. The dynamics of Runge-Kutta methods.
*Bifurcations Chaos*, vol. 2, no. 3, pp. 427–449, 1992.CrossRefMATHMathSciNetGoogle Scholar - [24]H. Bednář Ensemble Experiments with Low-dimensional Atmospheric Models, Ph. D. dissertation, Charles University in Prague, Czech Republic, 2010.Google Scholar