Sizing Storage for Reliable Renewable Integration: A Large Deviations Approach
Vivek Deulkar, Jayakrishnan Nair, Ankur A. Kulkarni

TL;DR
This paper models the reliability of renewable energy systems with storage using a Markov modulated fluid queue, providing insights into storage sizing to meet reliability targets, supported by real-world wind data case studies.
Contribution
It introduces a formal probabilistic model for assessing reliability of renewable-plus-storage systems and characterizes the asymptotic behavior of load loss probability as storage capacity grows.
Findings
Derived fundamental limits of reliability for renewable-storage systems.
Provided a method to determine storage size for desired reliability levels.
Validated the model with real-world wind power data.
Abstract
The inherent intermittency of wind and solar generation presents a significant challenge as we seek to increase the penetration of renewable generation in the power grid. Increasingly, energy storage is being deployed alongside renewable generation to counter this intermittency. However, a formal characterization of the reliability of renewable generators bundled with storage is lacking in the literature. The present paper seeks to fill this gap. We use a Markov modulated fluid queue to model the loss of load probability (LOLP) associated with a renewable generator bundled with a battery, serving an uncertain demand process. Further, we characterize the asymptotic behavior of the LOLP as the battery size scales to infinity. Our results shed light on the fundamental limits of reliability achievable, and also guide the sizing of the storage required in order to meet a given reliabilityâŚ
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Sizing Storage for Reliable Renewable Integration: A Large
Deviations Approach
Vivek Deulkar, Â Jayakrishnan Nair and Ankur A. Kulkarni Vivek and Jayakrishnan are with the Department of Electrical Engineering, Indian Institute of Technology Bombay, Mumbai, India. Ankur is with the Systems and Control Engineering group, Indian Institute of Technology Bombay, Mumbai, India. The authors can be reached at [email protected], [email protected], [email protected]. A preliminary version of this paper will be presented at IEEE PowerTech 2019[1].
Abstract
The inherent intermittency of wind and solar generation presents a significant challenge as we seek to increase the penetration of renewable generation in the power grid. Increasingly, energy storage is being deployed alongside renewable generation to counter this intermittency. However, a formal characterization of the reliability of renewable generators bundled with storage is lacking in the literature. The present paper seeks to fill this gap. We use a Markov modulated fluid queue to model the loss of load probability () associated with a renewable generator bundled with a battery, serving an uncertain demand process. Further, we characterize the asymptotic behavior of the as the battery size scales to infinity. Our results shed light on the fundamental limits of reliability achievable, and also guide the sizing of the storage required in order to meet a given reliability target. Finally, we present a case study using real-world wind power data to demonstrate the applicability of our results in practice.
I Introduction
Electric supply is an indispensable part of modern life and is thus required to meet extremely stringent requirements of reliability. Classically, loss of load has been caused due to operational reasons, such as a generator undergoing maintenance, grid conditions, such as the overdrawing of power, or due to extraneous circumstances, such as natural calamities. With increasing penetration of renewable generation, the natural variability of the output of these generators adds a new, supply-side cause for the loss of load. Fortunately, with the growing capacity of renewable generation, we are also witnessing a softening of storage prices. Thanks to this, an increasing number of renewable generators are countering their variability, not with conventional, fast-ramping generation, but rather with storage [2, 3]. Thus, we believe that the renewable generator of the future will not be a standalone renewable generator, but rather a renewable generator bundled with a battery.
Keeping in mind reliability as one of the central concerns of the electricity infrastructure, the introduction of a battery-renewable generator bundle raises some basic questions. To begin, how does one account for this bundle in calculations for system reliability? How does this reliability change with increasing variability of the renewable source (wind or solar)? How does this change with increasing capacity of the battery? If one targets a certain level of reliability, how much battery storage is required to attain this level? And finally, are there fundamental limitations on the performance of a bundle, in the sense that are there levels of performance that are simply unattainable?
A momentâs thought reveals that answers to these questions cannot be obtained by only considering one snapshot in time. To understand this, consider the hypothetical scenario where there is no battery and only a renewable generator attached to a constant load. Then the loss of load probability () would be simply the probability that the instantaneous output of the generator drops below the load, which one could potentially calculate via meteorological data. However, introducing storage changes the picture dramatically. Even while the instantaneous output of the generator may drop to a low level, there may well be charge left in the battery to meet the load requirements, and thus, using the bundle, the load could still be met. But the battery is charged by the excess output of the renewable generator, whereby the charge in the battery at any time depends on the history of generation (and load) realized until that time. It is easy to see that characterization of the in this case is a nontrivial matter.
This paper develops an analytical framework for characterizing the of a battery-renewable generator bundle. Our framework yields crisp answers to the sizing questions raised above. For a target level of reliability, it provides order-optimal estimates of the minimum battery size one requires to meet that reliability level, in terms of the statistical properties of the renewable source and the load. It also reveals that there are hard impossibilities: for certain ranges of these statistical parameters, no amount of battery suffices to bring the to zero. These results could be applied in conjunction with a costing exercise to ascertain the right battery size to be bundled with a renewable generator. One could also potentially use our characterization of the steady-state within a larger calculation of network-level reliability.
We model the net generation, i.e., the renewable generation minus the demand, as a continuous time Markov chain evolving over a finite state space. The battery serves as a buffer of finite capacity that is charged at the available rate when the net generation is positive and is discharged at the deficit rate when the net generation is negative. The battery charging process is subject to âboundary conditionsâ: it cannot be charged above its capacity and cannot be discharged below zero. Any positive net generation produced when the battery is fully charged is unusable. The is then the long run fraction of time the battery is discharged to zero. We find that when the drift, i.e., the steady-state average net generation, is negative, then a battery of any finite size results in an that remains bounded away from zero. In other words, the cannot be made arbitrarily small by choosing a large enough battery size when the drift is negative. However, when the drift is positive, the drops exponentially with battery size, allowing it to be made arbitrarily close to zero by choosing a suitably large battery size. The rate of decrease of with increase in battery size is dictated by a large deviations decay rate, which can also be characterized as the smallest positive generalized eigenvalue of the rate matrix associated with the net generation. This decay rate characterization can in turn be used to estimate the battery size required to achieve a given target
This paper is organized as follows. In Section II, we develop the mathematical model for the renewable source, load and the battery. In Section III, we characterize the asymptotics of the as the battery size scales to infinity. This serves as the basis of our sizing estimates. We then do a case study in Section IV where these results are tested and validated on real data of wind generation.
II Model and Preliminaries
Consider a storage battery of capacity which is charged or discharged by a net generation process associated with rate , where and denote, respectively, the generation and demand at time . The energy content of the battery, denoted by evolves as a regulated process having upper cap and lower cap [math]. Thus, evolves as
[TABLE]
Note that a fully charged battery cannot be charged further with a rate . Similarly an empty battery cannot be discharged further with a rate . Excluding these two boundary cases, the rate of change of the battery level is governed by the net generation rate . We assume that the rate is dependent on the state of a background Markov process, which collectively captures supply (generation) side variability as well as demand side variability.
Let denote the background Markov process. We assume that is an irreducible, time-reversible, continuous-time Markov chain (CTMC) over a finite state space . For every state , we associate a net generation rate with which the battery is charged or discharged. Thus, i.e., the rate of charging/discharging of the battery is a function of the state of the background CTMC It is easy to see now that is a Markov process that evolves over the state space . Note that this model also captures charge/discharge rate constraints on the battery; these would simply be reflected in the range of values taken by the net generation rates
The above mathematical model, wherein the occupancy of a buffer (or battery) is modulated by a background Markov process, is referred to in the queueing literature as a Markov Modulated Fluid Queue (MMFQ); see [4, 5]. In this paper, we use a finite-buffer MMFQ model to analyse the reliability of a renewable generator bundled with a battery.
Next, we describe how to characterize the invariant distribution of the Markov process which then leads to a characterization of the loss of load probability ( Note that we are assuming that the process has no state where the net generation rate is zero. This allows us to partition the state space as follows: , where
[TABLE]
We assume that both and are non-empty.111Indeed, if either or is empty, then the battery would forever remain completely charged or completely discharged.
Let denote the steady state of the Markov process We capture the invariant distribution of this process as follows:
[TABLE]
The invariant distribution is governed by the ODE
[TABLE]
where denotes the transition rate matrix associated with the CTMC and (see [4, 5]).222Since for all exists. The invariant distribution can now be computed using the following boundary conditions:
[TABLE]
where denotes the invariant distribution of the CTMC
The probability that the battery content is less than or equal to in steady state is given by . This probability is of particular relevance for . Indeed, the quantity is the long run fraction of time the battery is empty, and is also the long run fraction of time that the demand remains unfulfilled. In other words, this is the loss of load probability (), i.e.,
[TABLE]
The which can only be expressed in closed form for very simple cases (see below), can be computed numerically by solving the ODE (2) using the boundary conditions (3). However, this computation does not provide insights into the structural dependence of the on the supply-side and demand-side uncertainty (captured by the CTMC ) and the capacity of the battery. In Section III, we analyse the large battery asymptotics of the which sheds light on the limits of reliability achievable in a given setting, as well as the storage capacity required to achieve a certain (small) target.
Finally, we define a quantity that plays a key role in the large battery asymptotics, namely the drift associated with the supplyside and demandside uncertainty. The drift is defined as the steady state average net generation, i.e.,
[TABLE]
Note that (respectively, ) implies that the time-average generation is less than (respectively, greater than) the time-average demand.
We conclude this section by considering the special case where the background CTMC has only two states. This simple scenario, which admits a closed form characterization of the motivates the general large buffer asymptotics derived in Section III.
II-A Two state example
Consider the special case , where the generation alternates between two values [math] and while the demand takes a constant value . Specifically, we set In this case,
[TABLE]
where are the state transition rates for the generation process.
In this case, the drift is given by and the can be shown to be
[TABLE]
It is easy to see that is a strictly decreasing function of However, the limiting behavior of the as depends critically on whether the drift is positive or negative. When , then
[TABLE]
This means that the remains bounded away from zero for any finite In other words, when the drift is negative, an less than is simply unattainable no matter how large the battery capacity. This is consistent with Theorem 1 in Section III, which establishes a positive lower bound on the for any battery size when the drift is negative.
On the other hand, when
[TABLE]
where and 333We use to mean that This implies that when the drift is positive, the decays exponentially with the battery size, implying that an arbitrarily small target is achievable with a large enough battery. Moreover, we note that the decay rate is in fact the positive eigenvalue of . This is consistent with Theorem 2 in Section III, which establishes an exponential decay (in the battery size) of the when the drift is positive.
III Large Battery Approximations
In this section, we analyse the behavior of the as the battery size scales to infinity. Our results shed light on the feasibility of meeting reliability targets, and also guide the sizing of the battery required to meet a given reliability target.
As suggested by the two-state example in Section II, the asymptotic behavior of the as depends on whether the drift is positive or negative. Accordingly, we consider these cases separately.
III-A Negative drift: Asymptotic lower bound
We now consider the case i.e., the time-average generation is less than the time-average demand. One would therefore expect that cannot be made arbitrarily small in this case. This is proved formally in Theorem 1, which also provides a lower bound on the that is achievable with any finite battery size.
Let . Note that since we assume that is non-empty; is simply the maximum rate of discharge of the battery.
Theorem 1**.**
If then for any value of Moreover,
[TABLE]
with equality if
Theorem 1 is a consequence of the law of large numbers for Markov chains. It states that when the steady state average demand exceeds the steady state average generation, then an less than or equal to is unattainable no matter how large a battery we deploy. Moreover, this bound is loose in general; it is tight when the background CTMC has only a single state of discharge. The proof of Theorem 1 can be found in Appendix A.
Connection with the two state example: In the two-state example considered in Section II, note that and In this example, when recall that indeed, with
III-B Positive drift: asymptotics
We now consider the case i.e., the time-average generation exceeds the time-average demand. In this case, one might expect that it is possible, with a large enough battery, to store the excess generation when the instantaneous generation exceeds demand, and to use this stored energy to almost always fulfil the deficit when the instantaneous generation drops below the demand. Theorem 2 shows that this is indeed the case, and that the decays exponentially with the battery size (when the drift is positive). Moreover, Theorem 2 provides two characterizations of this exponential rate of decay: one from large deviations theory, and the other as the smallest positive eigenvalue of
We now introduce some preliminaries required to state our large deviations decay rate characterization (Theorem 2). We uniformize (see [6] for background on uniformization of CTMCs) the background Markov process such that the outgoing rate out of each state equals
[TABLE]
recall that denotes the rate matrix corresponding to 444The th entry of a matrix is denoted as Let denote the sequence of intervals between state transitions in this uniformized chain; note that is an i.i.d. sequence of random variables.555 refers to the exponential distribution with mean . Let denote the embedded Markov chain corresponding to the (uniformized) Markov process is now a time homogeneous discrete time Markov chain (DTMC); we denote by the transition probability matrix corresponding to this DTMC. We make the following observations.
The DTMC is independent of the sequence 2. 2.
which denotes the invariant distribution corresponding to the background Markov process is also the invariant distribution corresponding to the embedded DTMC
Define
[TABLE]
The process satisfies a large deviations principle (this follows from the Gartner-Ellis conditions [7]; see Appendix B), with a rate function that is defined in terms of the following function.
[TABLE]
That is well defined, i.e., the limit in the above definition exists as an extended real number for all is shown in Lemma 4 in Appendix B.
Theorem 2**.**
If then
[TABLE]
where
[TABLE]
Moreover, also equals the smallest positive eigenvalue of
Theorem 2 states that the decays exponentially with respect to the battery size with decay rate This ensures that any arbitrarily small target be achieved with a suitably large battery. Additionally, Theorem 2 provides an explicit characterization of this exponential rate, which can in turn be used to estimate of the battery size required in order to meet a given (small) target; we address battery sizing in detail as part of our case study (see Section IV).
Connection with the two state example: Recall that in the two state example considered in Section II, we saw that when where is the only positive eigenvalue of
Proof of Theorem 2
We analyse the large buffer asymptotics of the via the reversed system [5], which is obtained by interchanging the role of generation and demand. Thus, and where we use the superscript to represent quantities in the reversed system. Moreover, Since the original system is associated with a positive drift (), the reversed system is associated with negative drift ().
The associated with the original system is captured in the reversed system as follows.
[TABLE]
Here, denotes the stationary buffer occupancy in the reversed system with an infinite buffer. Note that is well defined since The equality in (5), which states that the long run fraction of time the battery is empty in the original system equals the long run fraction of time the battery is full in the reversed system, was first shown in [5]. The inequality follows from a straighforward sample path argument; by coupling the background process between the finite and infinite buffer systems, taking it is not hard to show that for all
The asymptotics of have been established via a direct analysis of the invariant distribution of the process in [5]:
[TABLE]
where and is the smallest positive eigenvalue of
In light of (5) and (6), it suffices to prove the following statements.
Lemma 1**.**
Let be the steady state battery occupancy level of the infinite battery of the reversed system described above.
[TABLE]
Lemma 2**.**
Let be the steady state battery occupancy level of the finite battery of the reversed system described above.
[TABLE]
Lemmas 1 and 2 are proved in Appendix B-A and Appendix B-B respectively, using large deviations arguments.
IV Case Study
In this section, we demonstrate the applicability of the results presented in Section III in practice. We fit a Markov model to a real-world trace of wind power generation, allowing us to validate the predictions from our analytical results against empirical observations. Further, we address the question of battery sizing in order to meet a given reliability target.
IV-A Data collection
We collected time series data corresponding to three years of wind power generation (December 2014 to December 2017) within the jurisdiction of the Bonneville Power Administration (BPA) (see [8]). The data samples are five minutes apart, and range from 0 to 4500 MW.
As expected, the data is highly non-stationary in nature, exhibiting diurnal as well as seasonal variations. Since our Markov modeling is best suited to stationary data, we extracted the samples corresponding to the months of February and March from 9PM to 3AM for fitting a Markov model; this restricted dataset is henceforth referred to as the âstationary wind dataâ. For comparison, we also fit a Markov model to the entire (highly non-stationary) time series.
IV-B Data processing and Markov modeling
We now describe how we fit a Markov model to the above wind data.666This has been attempted before by several authors, including [9, 10, 11, 12]. However, these prior works evalaute the âfitâ quality of their Markov models using the mean and auto-correlation function. In contrast, we match the reliability implied by the Markov model against the empirical reliability, which is a more direct indicator of the usefulness of the model. We first quantize the data into bins, the bin edges being (in MW): [0, 60, 120, 180, 240,300, 450, 600, 900, 1200, 1500, 1800, 2100, 2400, 2700, 3000, 3300, 3600, 3900, 4200, 4500]. This non-uniform binning is done to ensure a roughly even distribution of samples across bins. The bins constitute the state space for our Markov model.
Given this state space, we obtain the empirical transition probability matrix as follows:
[TABLE]
is the maximum likelihood estimator of the transition probability matrix corresponding to a discrete-time Markov chain (DTMC) model for the wind power sampled at intervals. To obtain a continuous-time Markov chain (CTMC) description, we note that the transition rate matrix of the CTMC is related to as follows: . Using the first-order Taylor series approximation for small , we get , where is the identity matrix.777This Taylor approximation is valid to long as is smaller than the typical transition times of the CTMC. Accordingly, we set . This matrix defines a CTMC description of the wind power data.
To define the net generation corresponding to each state, we assume a constant demand over time. Thus, the net generation rate corresponding to bin equals where denotes the bin-center corresponding to bin Note that we can control the drift by varying
IV-C Evaluating the goodness of fit
We now evaluate the quality of our Markov models by comparing the implied by these models with the empirical implied by the data. This also allows us to demonstrate the applicability of the conclusions of Theorems 1 and 2 in practice. In Figures 1 and 2, we plot the as a function of the battery size setting 1800 MW () and 1200 MW (), respectively. We do this for the âstationary wind dataâ as well as the entire time series. Specifically, we plot the following quantities:
- â˘
Simulated (cont. time) : This is the computed by simulating the CTMC model for wind power generation obtained from the data.
- â˘
Simulated (discrete time) : This is the computed by simulating the DTMC model for wind power generation obtained from the data, taking the generation to be constant over 5 minute intervals.
- â˘
Empirical : This is the computed by simulating the battery evolution using the wind power generation trace, again assuming the generation to be constant over 5 minute intervals.
Note that in all the plots, the simlulated from our CTMC model closely matches the simulated from the DTMC model. This essentially validates our first order Taylor approximation for fitting the transition rate matrix from the empirical transition probability matrix Moreover, we note that the simulated from the Markov models more closely matches the empirical for the stationary wind data than for the entire time series. This suggests that the Markov models are a better fit on the stationary data than on the complete, highly non-stationary time series. In practice, this means we should fit different Markov models to capture wind variability in different parts of the day in each season.
Focusing specifically on Figure 1, which corresponds to the negative drift scenario, we make the following observations.
- â˘
The empirical as well as simulated converges, as becomes large, to a value which is lower bounded by the bound specified in Theorem 1.
- â˘
The empirical is less than the implied by the Markov models. In other words, our models tend to overestimate the
- â˘
The corresponding to a given battery size888We plot battery size in SI units (Joules). However, the engineering practice is to measure battery capacity in kiloWatt-hour (kWh), where 1 kWh J.
is greater for the entire time series as compared to the stationary data, suggesting that the former dataset is more âvariableâ than the latter.
Focusing next on Figure 2, which corresponds to the positive drift scenario, we note that the decays to zero as becomes large, consistent with Theorem 2. Moreover, we see that the Markov models tend to overestimate the (as before). To illustrate the exponential decay of with battery size clearly, we plot the simulated from the CTMC model on a log-linear scale in Figure 3. Note that the plot looks asymptotically linear (establishing the exponential decay), with a slope that closely matches the decay rate from Theorem 2.
IV-D Battery sizing
The above results support our claim that when the decays exponentially with battery size with a decay rate equal to In other words, when is large, the may be approximated as
[TABLE]
This further implies that the battery size required to maintain the at is given by
[TABLE]
Since the pre-factor in (7) is unknown here, a natural approximation would be to estimate the battery size required as
[TABLE]
Clearly, we would expect the above estimate to be accurate upto an additive offset. Moreover, we would expect that the error of our estimate would be small in relative terms for smallÂ
To validate (8), consider the CTMC model for the stationary wind data, with MW. For this model, we compare the minimum storage size required to bring the simulated below with the estimate (8); see the left panel of Figure 4. Notice the constant offset between the two curves, as predicted. However, we note the (unknown) offset results in a roughly 40% error in battery size requirement when For lower values of the relative error would of course be smaller. This means that for moderate values of reliability target the estimate (8) can be used to make ballpark estimates of the storage size required.
However, (7) can also be used for relative storage sizing as follows: Note that (7) suggests that shrinking the be a factor of would require an increase in battery size of To validate this approximation, we consider the following baseline scenario. Setting MW with the stationary wind data, and J, the simulated equals In the right panel of Figure 4, we plot the additional battery size required to make the versus using the above approximation, as well as by simulating the CTMC model. Note that the approximation is remarkably accurate, even for moderate values of
This shows that (7) is an accurate description of the as becomes large, and can be used in practice to guide battery sizing decisions.
V Concluding Remarks
In this paper, we developed an analytical framework for characterizing the reliability of a renewable generator bundled with a battery. We analysed how the reliability, captured by the scales as the battery size increases. Our results highlight the achievable limits of reliability, and provide useful guidelines for sizing storage in practice.
While we have used as the reliability metric throughout this paper, it should be noted that our conclusions extend readily to another related metric, i.e., lost load rate (), which is defined as the long run rate of unserved load, i.e.,
[TABLE]
Since there exists positive constants and such that
[TABLE]
our asymptotic characterizations of as extend readily to Indeed, when When decays exponentially with with the same decay rate as the one characterized in Theorem 2 for
This work motivates future research along several directions. We believe our formulations are a natural first step to analyse the economies of scale that would result from sharing of storage, between renewable generators or electricity prosumers; we show a result along these lines in [13]. Another direction is performing a similar reliability calculation with for a network of generators, taking into account transmission constraints. Finally, we note that our work motivates more sound stochastic modeling of renewable generation, to improve the real-world applicability of analytical reliability characterizations (as in the present paper).
Appendix A Proof of Theorem 1
The proof of Theorem 1 is based on energy conservation of the battery content together with the law of large numbers applied to the background Markov process.
Let be the total amount of wasted energy due to battery overflow in the interval Similarly, let be the total amount of unserved energy demand in the same interval (during loss of load). Let be the net demand served over the interval and be total generation over the same interval. Finally, define
[TABLE]
Recall that Let . With these notations we have the following result.
Lemma 3**.**
. If the drift is negative, i.e., then .
Proof:
Applying energy conservation, we get
[TABLE]
[TABLE]
Since the battery capacity is finite, and law of large numbers for Markov chains implies that . Therefore we get
[TABLE]
It is easy to see that
[TABLE]
where denotes the stationary buffer occupancy in an infinite buffer system seeing the same net generation process.
When the drift is negative, as , decays exponentially with (see [5]), which implies that
[TABLE]
With this result we now prove Theorem 1.
Proof:
It is not hard to see that
[TABLE]
From Lemma 3, Therefore,
[TABLE]
When the background CTMC has only a single state of discharge, i.e., , then . From Lemma 3, which gives us
[TABLE]
Appendix B Decay rate for
B-A Proof of Lemma 1
Let the sequence denote the buffer occupancy in the infinite buffer reversed system, sampled at the transition instants of the (uniformized) background process We have
[TABLE]
where Since the discrete-time process is obtained by sampling the continuous-time process at the instants of a Poisson process (of rate ), the PASTA property (see [14]) implies that the time averages corresponding to both coincide. Moreover, (9) is a Lindley recursion (see [15]) with negative drift (since ). The logarithmic asymptotics of thus follow (see Theorem 3.1 in [15]) once we verify that the function is well defined and satisfies the Gartner-Ellis conditions [7]. This is done in Lemma 4 below.
The function is characterized as follows.
Lemma 4**.**
[TABLE]
where is the Perron Frobenious eigenvalue corresponding to the matrix defined as
[TABLE]
where recall that is the transition probability matrix of the embedded Markov chain . Moreover, is convex and differentiable over and
[TABLE]
Proof.
Throughout the proof, we assume It is not hard to see that if
Define The vector can be expressed inductively as follows.
[TABLE]
Thus, Denoting the law of the Markov process at time [math] by the row vector
[TABLE]
That
[TABLE]
now follows from the Perron Frobenius theorem [7, Theorem 3.1.1].
That is convex follows from the fact that it is pointwise limit of convex functions. Its differentiability follows from the differentiability of Perron Frobenius eigenvalue of a non-negative matrix with respect to its entries. That follows from Lemma 3.2 in [15].
Finally, to show (10), we use where is a symmetric non-negative matrix defined as
[TABLE]
(see Theorem 2 in [16]). It therefore suffices to show that as and which follows trivially from the observation that along each of the above limits (note that all diagonal entries of are positive).
B-B Proof of Lemma 2
Lemma B-B follows from standard techniques in large deviations theory that show that the decay rates associated with and as are the same under very general conditions; see [17] and [15, Section 6.5].
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