# Chapter 11 A simple RC model (Python)

As a practical example of linear state-space models, the simplified resistor-capacitor (RC) model structures are a popular choice for either parameter estimation or system identification. When written as a set of stochastic differential equations, they allow accounting for modelling approximations (Madsen and Holst (1995)) and offer a more reproducible parameter estimation than deterministic models that overlook modelling errors (Rouchier, Rabouille, and Oberlé (2018)).

This **Python** tutorial shows an RC model being used to estimate the heat resistance and capacitance of a test house. The model will be implemented twice: the first time in a deterministic formulation, without system uncertainty; the second time in a stochastic formulation, solved by the Kalman filter.

## 11.1 Case study

The experimental test cell used in this study is called the Armadillo Box. It is a demonstration building of 42 m\(^2\) floor area, designed for the 2010 European Solar Decathlon by the ENSAG-GAIA-INES team. The envelope is a light wood framed construction with integrated insulation. Heating and cooling is performed by a “3 in 1” heat pump, and photovoltaic solar panels provide recharge for electric vehicles.

```
import pandas as pd
import numpy as np
import matplotlib.pyplot as plt
= pd.read_csv('data/statespace.csv') df
```

The building is monitored by a variety of sensors, but the present study only uses records of indoor temperature and prescribed heating power, in addition to weather data. The indoor temperature profiles used here have been averaged over several sensors distributed in the living space. The measurement time is 4 days, during which there is a 24 hour heat input.

*Note from the author: I chose not to display the code that generated the figures in this page. This is not just for clarity, but mostly because matplotlib integrates poorly into Rmarkdown documents.*

## 11.2 Modelling

### 11.2.1 RC model

Consider the example of a simple building represented by a 2-resistor, 2-capacitor model structure (2R2C), described in Sec. 10.2.

The equations of this model are: \[\begin{align} C_i \, \mathrm{d} T_i & = \dfrac{1}{R_i}\left(T_e-T_i\right)\mathrm{d}t + \Phi_h \, \mathrm{d}t + A_i \Phi_s \mathrm{d}t + \sigma_i \,\mathrm{d}\omega_i \tag{11.1} \\ C_e \, \mathrm{d} T_e & = \dfrac{1}{R_i}\left(T_i-T_e\right)\mathrm{d}t + \frac{1}{R_o}\left(T_o-T_e\right)\mathrm{d}t + A_e \Phi_s \mathrm{d}t + \sigma_e \, \mathrm{d}\omega_e \tag{11.2} \end{align}\] where \(T_i\), \(T_e\) and \(T_o\) are the indoor, envelope and outdoor temperatures. The envelope temperature is associated with the thermal mass of the opaque surfaces, and does not represent a specific coordinate within the envelope. The model has two states \(T_e\) (unobserved) and \(T_i\) (observed); \(\Phi_h\) (W) is the indoor heating power; \(\Phi_s\) (W/m\(^2\)) is the global horizontal solar irradiance. \(R_i\) (K/W) is the thermal resistance between the indoor air temperature and the envelope, \(R_e\) the resistance between the envelope and the ambient air. \(C_i\) and \(C_e\) (J/K) are the heat capacitances of the interior and the envelope, respectively, and \(A_i\) and \(A_e\) (m\(^2\)) are their solar gain coefficients. \(\{\omega_i\}\) and \(\{\omega_e\}\) are standard Wiener processes and \(\sigma_i^2\) are \(\sigma_e^2\) are their variances. This process noise is a way to account for modelling approximations, unrecognized inputs or noise-corrupted input measurements.

Despite its simplicity, this model structure is able to reproduce the thermal behaviour of a simple unoccupied building. The equations can be written in matrix form: \[\begin{align} \mathrm{d} \begin{bmatrix} T_i \\ T_e \end{bmatrix} & = \begin{pmatrix} -\frac{1}{R_i \, C_i} & \frac{1}{R_i \, C_i} \\ \frac{1}{R_i \, C_e} & -\frac{1}{R_i \, C_e}-\frac{1}{R_e \, C_e}\end{pmatrix} \begin{bmatrix} T_i \\ T_e \end{bmatrix}\, \mathrm{d}t \\ & + \begin{pmatrix} 0 & \frac{1}{C_i} & \frac{A_i}{C_i} \\ \frac{1}{R_o \, C_e} & 0 & \frac{A_e}{C_e} \end{pmatrix} \begin{bmatrix} T_o \\ \Phi_h \\ \Phi_s \end{bmatrix} \, \mathrm{d}t + \mathbf{\sigma} \, \mathrm{d}\omega \tag{11.3} \end{align}\] which is the dynamic model of the following stochastic state-space model, written in continuous-discrete form: \[\begin{align} \mathrm{d}\mathbf{x}(t) & = \mathbf{A}_\mathit{rc} \, \mathbf{x}(t) \, \mathrm{d}t + \mathbf{B}_\mathit{rc} \, \mathbf{u}(t)\,\mathrm{d}t + \mathbf{\sigma}_\theta \mathrm{d}\omega \tag{11.4} \\ \mathbf{y}_t & = \mathbf{C}_\theta \, \mathbf{x}_t + \mathbf{v}_t \tag{11.5} \end{align}\] The state vector \(\mathbf{x}\) includes the temperatures \(T_i\) and \(T_e\) calculated by the model, and \(\mathbf{u}=\left[T_o, \Phi_h, \Phi_s\right]\) is the input vector including boundary conditions and excitations. The second equation is the observation equation. It indicates that the measured quantity \(y_t\) may be different from the output of the state equation. In our case, the observed temperature is only the first component of the state vector, and is encumbered with some measurement error \(\mathbf{v}_t\). In this equation, time is noted as a subscript to indicate that observations come in a discrete sequence.

## 11.3 Deterministic formulation

We first consider the most simple implementation of the model: if the modelling errors \(\{\omega_i\}\) and \(\{\omega_e\}\) are neglected. This is what we call a deterministic formulation, as this hypothesis is equivalent to assuming that the model is absolutely correct in reproducing the behaviour of the house.

Perhaps the easiest way to solve Eq. (11.3) for the temperatures is an explicit discretisation scheme: the indoor and envelope temperatures at time \(t+1\) are functions of all variables at time \(t\):

\[\begin{align} T_i^{(t+1)} & = T_i^{(t)} + \frac{\mathrm{d}t}{C_i} \left( \dfrac{1}{R_i}\left(T_e-T_i\right) + \Phi_h + A_i \Phi_s \right)^{(t)} \tag{11.6} \\ T_e^{(t+1)} & = T_e^{(t)} + \frac{\mathrm{d}t}{C_e} \left( \dfrac{1}{R_i}\left(T_i-T_e\right) + \frac{1}{R_o} \left(T_o-T_e\right) + A_e \Phi_s \Phi_s\right)^{(t)} \tag{11.7} \end{align}\]

In Python, we define this model in a function that takes the inputs \(\mathbf{u}\) as first argument, and the model parameters as other arguments. This syntax is necessary so that we can call Scipy’s `curve_fit`

method later. The function returns the indoor temperature, to be compared with the measurements.

```
= df[['Time', 'T_ext', 'P_hea', 'I_sol']].values
inputs = df['T_int'].values
output
# Function that will calculate the indoor temperature for a given value of R and C
def simpleRC(inputs, Ri, Ro, Ci, Ce, Ai, Ae):
= inputs[:, 0]
time = inputs[:, 1]
to = inputs[:, 2]
phi_h = inputs[:, 3]
phi_s
= np.zeros(len(time))
ti = np.zeros(len(time))
te
# Initial temperatures
0] = output[0]
ti[0] = ( Ri*to[0] + Ro*ti[0] ) / (Ri + Ro)
te[
# Loop for calculating all temperatures
for t in range(1, len(output)):
= time[t] - time[t-1]
dt = ti[t-1] + dt / Ci * ( (te[t-1]-ti[t-1])/Ri + phi_h[t-1] + Ai*phi_s[t-1] )
ti[t] = te[t-1] + dt / Ce * ( (ti[t-1]-te[t-1])/Ri + (to[t-1]-te[t-1])/Ro + Ae*phi_s[t-1] )
te[t]
return ti
```

We can find the optimal parameters \(\theta=(R_i, R_o, C_i, C_e, A_i, A_e)\) by minimizing the sum of squared residuals between the measured indoor temperature and the output of the function we just defined. This is equivalent to what the `curve_fit`

method of Scipy does here.

The method requires initial parameter values. They can be picked by running a few simulations first until the predictions are approximately in the right range. This step is not detailed here.

```
import scipy.optimize as so
= so.curve_fit(f=simpleRC,
p_opt, p_cov =inputs,
xdata=output,
ydata=(0.01, 0.01, 1e6, 1e7, 5, 5))
p0
# Saving results into a dataframe and displaying it
= pd.DataFrame(index=['Ri', 'Ro', 'Ci', 'Ce', 'Ai', 'Ae'])
res1 'avg'] = p_opt
res1['std'] = np.diag(p_cov)**0.5
res1[print(res1)
```

```
## avg std
## Ri 4.091570e-03 0.000125
## Ro 5.038526e-02 0.004552
## Ci 5.344581e+06 225321.203258
## Ce 1.761891e+07 841478.831398
## Ai 1.861247e-01 0.055401
## Ae -1.571828e+00 0.096530
```

The estimated parameters seem consistent with our expectations. We can compare the profile of measured indoor temperature with the output that the model predicts given the identified optimal parameters.

## 11.4 Stochastic formulation

In more realistic applications, the phenomena that impact the energy balance of a building are far more complex than what such a simple model may predict. We extend the RC model structure in order to include effects of solar irradiance, ventilation, several time constants of inertia… But there is a limit to how complex a model can be made, before parameter identification becomes infeasible.

If a model does not fully describe the thermal behaviour of the building, and this discrepancy is not somehow explicitely accounted for, then the parameter estimates and predictions will be biased and unreliable. Stochastic state-space models are a way to account for modelling uncertainties and are now standard practice in the field of building energy performance assessment.

### 11.4.1 Specification

The basics of linear state space models has been explained in Sec. 10.2 and the principle of the Kalman filter in Sec. 10.3. In the following block, a class `RC`

is defined which implements these equations for any RC model. Any new RC model can then be inherited from this class, by specifying its matrices \(\mathbf{A}_\mathit{rc}\), \(\mathbf{A}_\mathit{rc}\) and \(\mathbf{A}_\mathit{rc}\), and the covariance matrices of the modelling and measurement errors \(\mathbf{Q}\) and \(\mathbf{R}\) (see eq. (11.4) and (11.5)).

```
from scipy.linalg import expm
from numpy.linalg import inv
class RC(object):
"""This is the generic class for any RC model structure"""
def __init__(self):
pass
def discretize(self, dt):
""" This method applies the discretisation equations shown in the previous chapter
It is only function of the time step size dt
"""
= self.N_states
n # Discretisation
= expm(self.Ac * dt)
F = np.dot(inv(self.Ac), np.dot(F - np.eye(n), self.Bc))
G = self.Cc
H # System error covariance matrix (continuous Qc and discrete Q)
= expm(np.block([[-self.Ac, self.Qc], [np.zeros(np.shape(self.Ac)), self.Ac.T]]) * dt)
foo = np.dot(foo[n:2 * n, n:2 * n].T, foo[0:n, n:2 * n])
Q # Measurement error covariance matrix (discrete)
= self.Rc / dt
R
return F, G, H, Q, R
def prediction(self, x_0, t, u, y=None, update=False):
""" This method predicts the indoor temperature.
If update=True, the function will apply all steps of the Kalman filter
and return the mean state, covariances of innovations and the likelihood
If update=False, the function will only predict states and their variance,
as if no measurements were available. Use this for forecasting.
x_0: initial state vector
t: vector of time coordinates
u: input vector
y: measurement vector (only required if update=True)
"""
= len(t)
N_time
# Initialisation of all arrays that will be used in the calculations
# Mean and variance of the states calculated at the prediction step
= np.zeros((N_time, self.N_states))
x_avg_predict = np.zeros((N_time, self.N_states, self.N_states))
x_var_predict 0] = x_0
x_avg_predict[0] = np.eye(self.N_states)
x_var_predict[
= np.zeros((N_time, self.N_states))
x_avg_update = np.zeros((N_time, self.N_states, self.N_states))
x_var_update 0] = x_0
x_avg_update[0] = np.eye(self.N_states)
x_var_update[
= np.zeros(N_time) # prediction errors (innovations)
epsilon = np.zeros(N_time) # innovation covariances
Sigma = np.zeros(N_time) # log-likelihood to be minimized
loglike
for i in range(1, N_time):
# Matrices of the current time step (depend on the time step size dt)
= t[i] - t[i - 1]
dt = self.discretize(dt)
F, G, H, Q, R
# KALMAN 1: Prediction step
= np.dot(F, x_avg_update[i-1]) + np.dot(G, u[i])
x_avg_predict[i] = np.dot(F, np.dot(x_var_update[i-1], F.T)) + Q
x_var_predict[i]
if update:
# KALMAN 2: Residuals and Kalman gain
= y[i] - np.dot(H, x_avg_predict[i])
epsilon[i] = np.dot(H, np.dot(x_var_predict[i], H.T)) + R
foo = foo
Sigma[i] = np.dot(x_var_predict[i], np.dot(H.T, np.linalg.inv(foo)))
K = -0.5 * epsilon[i] ** 2 / Sigma[i] - 0.5 * Sigma[i] * 2 * np.pi
loglike[i] # KALMAN 3: Update and weight
= x_avg_predict[i] + np.dot(K, y[i] - np.dot(H, x_avg_predict[i]))
x_avg_update[i] = x_var_predict[i] - np.dot(K, np.dot(H, x_var_predict[i]))
x_var_update[i] else:
= x_avg_predict[i]
x_avg_update[i] = x_var_predict[i]
x_var_update[i]
# Returns
if update:
# If the Kalman update was used, return
= np.dot(H, x_avg_predict.T).flatten()
X = Sigma.flatten()
S return X, S, loglike
else:
= np.dot(H, x_avg_predict.T).flatten()
X_avg = np.dot(H, np.dot(x_var_predict, H.T)).flatten()
X_var return X_avg, X_var
```

The 2-resistor, 2-capacitor model drawn above is then inherited from this `RC`

class. Upon definition, it takes its parameters as arguments.

```
class tite(RC):
def __init__(self, Ri, Ro, Ci, Ce, Ai, Ae, qi, qe, r):
""" Model inputs: ambient temperature, heating, solar irradiance"""
# Model parameters
self.Ri = Ri # The first resistance (K/W) of the model, on the indoor side
self.Ro = Ro # The second resistance (K/W) of the model, on the outdoor side
self.Ci = Ci # Heat capacity (J/K) connected to the indoor temperature
self.Ce = Ce # Heat capacity (J/K) connected to the envelope temperature
self.Ai = Ai # Solar aperture coefficient directed to the indoor temperature
self.Ae = Ae # Solar aperture coefficient directed to the envelope temperature
self.qi = qi # Standard deviation of the modelling error on Ti
self.qe = qe # Standard deviation of the modelling error on Ti
self.r = r # Standard deviation of the measurement error
# Number of states
self.N_states = 2
# Matrices of the continuous system
self.Ac = np.array([[-1/(Ci*Ri), 1/(Ci*Ri)],
1/(Ce*Ri), -1/(Ce*Ri) - 1/(Ce*Ro)]])
[self.Bc = np.array([[0, 1 / Ci, Ai / Ci],
1/(Ce*Ro), 0, Ae/Ce]])
[self.Cc = np.array([[1, 0]])
# System and measurement error covariance matrices
self.Qc = np.diag([qi**2, qe**2])
self.Rc = np.array([[r ** 2]])
```

Notice that this model has four additional parameters compared to the deterministic formulation above: the variance of the modelling errors on each state `qi`

and `qe`

, and the measurement error `r`

.

### 11.4.2 Training

We now need to find the parameters that will offer the best fit between predictions of the 2R2C model and indoor temperature measurements. We will simply use the `curve_fit`

method from Scipy again.

In order to facilitate convergence, an initial parameter value is first defined. Then, the optimiser will act on an evaluation function that receives each parameter as argument, and returns the likelihood value. Some parameters are log-transformed in order to allow the search over larger scales.

```
# Definition of an evaluation function that takes "normalized" values or each parameter
def evaluation(df, Ri, Ro, Ci, Ce, Ai, Ae, qi, qe, r, xe0):
# Reading the dataframe given as argument
= df['Time'].values
t = df[['T_ext', 'P_hea', 'I_sol']].values
u = df['T_int'].values
y
# Model specification and initial condition
= tite(Ri, Ro, Ci, Ce, Ai, Ae, qi, qe, r)
model = [y[0], xe0]
x_0
# Model prediction, without Kalman update
= model.prediction(x_0, t, u, y, update=True)
X, S, L
# We only need the likelihood for the minimize method
return X
```

```
from scipy.optimize import curve_fit
# Curve fitting happens here. popt and pcov are the mean and covariance of parameter estimates
= curve_fit(evaluation,
popt, pcov = df,
xdata = df['T_int'],
ydata = np.append(res1['avg'], [1e-3, 1e-3, 1e-1, 20]) ,
p0 ='lm')
method
= pd.DataFrame(index=['Ri', 'Ro', 'Ci', 'Ce', 'Ai', 'Ae', 'qi', 'qe', 'r', 'xe0'])
res2 'avg'] = popt
res2['std'] = np.diag(pcov)**0.5
res2[
print(res2)
```

```
## avg std
## Ri 2.799801e-03 0.000125
## Ro 1.680273e-02 0.001284
## Ci 3.773714e+06 152372.536275
## Ce 1.469854e+07 876101.583123
## Ai 1.561966e-01 0.045091
## Ae -3.933333e-02 0.124889
## qi 8.516594e-09 0.000244
## qe 6.275908e-06 0.008552
## r -2.055527e-02 28.008709
## xe0 2.992531e+01 0.562491
```

Notice that `Ae`

, the solar gain coefficient on the envelope capacity, has an average value lower than its standard deviation: this parameter is likely not influential on the outcome.

### 11.4.3 Diagnostics and residuals analysis

In order to evaluate the agreement between the fitted model and the data, let us first simply view the model output in prediction mode (without Kalman update at every time step).

```
# Model specification with the mean of optimised parameters
= tite(*res2['avg'][:-1])
model_opt
# Initial states
= df['Time'].values
t = df[['T_ext', 'P_hea', 'I_sol']].values
u = df['T_int'].values
y = [y[0], res2['avg']['xe0'] ]
x_0
# Prediction without Kalman update, to be compared with the data
= model_opt.prediction(x_0, t, u, y=None, update=False) x_avg, x_var
```

The model fits the data well. The 95% confidence intervals are relatively narrow, indicating a good confidence in the prediction.

Another important criterion on which to judge the fitted model is the autocorrelation function (ACF) of the one-step ahead prediction residuals. In order to view these residuals, the prediction function should be run with the Kalman updating switched on, so that the states it returns are one-step ahead predictions only.

```
= model_opt.prediction(x_0, t, u, y, update=True)
X, S, L
# eps_ are the one-step ahead prediction residuals
= y - X
eps_ # Let's only take every other value, so that we have time lags of one hour.
= eps_[::2]
eps_
# Correlation function of two time series. Can be used for the autocorrelation of a single time series
def crosscorrelation(x, u):
"""
http://stackoverflow.com/q/14297012/190597
http://en.wikipedia.org/wiki/Autocorrelation#Estimation
"""
= len(x)
n = x-x.mean()
x = u-u.mean()
u = np.correlate(x, u, mode = 'full')[-n:]
r return r/(x.std()*u.std()*(np.arange(n, 0, -1)))
# Autocorrelation of the residuals (only keeping the first 50 lags)
= crosscorrelation(eps_, eps_)[0:50]
ACF = np.linspace(0,49,50) lags
```

The residuals are low, except from one important peak at 24h lag. This suggests that an important influence occuring with a period of 24 hours has been insufficiently accounted for by the model.

### References

*Energy and Buildings*22 (1): 67–79.

*Building and Environment*134: 181–90.