%\section{Recursive State Estimation} \section{Filtering} \label{sec:filtering} As mentioned before, most smoothing methods require a preceding filtering. Similar to our previous works, we consider indoor localisation as a time-sequential, non-linear and non-Gaussian state estimation problem. Therefore, a Bayes filter that satisfies the Markov property is used to calculate the posterior: % \begin{equation} \arraycolsep=1.2pt \begin{array}{ll} &p(\mStateVec_{t} \mid \mObsVec_{1:t}) \propto\\ &\underbrace{p(\mObsVec_{t} \mid \mStateVec_{t})}_{\text{evaluation}} \int \underbrace{p(\mStateVec_{t} \mid \mStateVec_{t-1}, \mObsVec_{t-1})}_{\text{transition}} \underbrace{p(\mStateVec_{t-1} \mid \mObsVec_{1:t-1})d\vec{q}_{t-1}}_{\text{recursion}} \end{array} \label{equ:bayesInt} \end{equation} % Here, the previous observation $\mObsVec_{t-1}$ is included into the state transition \cite{Ebner-15}. For approximating eq. \eqref{equ:bayesInt} by means of MC methods, the transition is used as proposal distribution, also known as CONDENSATION algorithm \cite{isard1998smoothing}. This algorithm also performs a resampling step to handle the phenomenon of weight degeneracy. In the context of indoor localisation, the hidden state $\mStateVec$ is defined as follows: \begin{equation} \mStateVec = (x, y, z, \mStateHeading, \mStatePressure),\enskip x, y, z, \mStateHeading, \mStatePressure \in \R \enspace, \end{equation} % where $x, y, z$ represent the position in 3D space, $\mStateHeading$ the user's heading and $\mStatePressure$ the relative atmospheric pressure prediction in hectopascal (hPa). Further, the observation is given by % \begin{equation} \mObsVec = (\mRssiVec_\text{wifi}, \mRssiVec_\text{ib}, \mObsHeading, \mObsSteps, \mObsPressure, \mObsActivity) \enspace, \end{equation} % covering all relevant sensor measurements. Here, $\mRssiVec_\text{wifi}$ and $\mRssiVec_\text{ib}$ contain the measurements of all nearby \docAP{}s (\docAPshort{}) and \docIBeacon{}s, respectively. $\mObsHeading$ and $\mObsSteps$ describe the relative angular change and the number of steps detected for the pedestrian. $\mObsPressure$ is the relative barometric pressure with respect to a fixed reference. Finally, $\mObsActivity$ contains the activity, currently estimated for the pedestrian, which is one of: unknown, standing, walking, walking stairs up or walking stairs down. The probability density of the state evaluation is given by % \begin{equation} %\begin{split} p(\vec{o}_t \mid \vec{q}_t) = p(\vec{o}_t \mid \vec{q}_t)_\text{baro} \,p(\vec{o}_t \mid \vec{q}_t)_\text{ib} \,p(\vec{o}_t \mid \vec{q}_t)_\text{wifi} \enspace %\end{split} \label{eq:evalBayes} \end{equation} % and therefore similar to \cite{Ebner-16}. Here, we assume a statistical independence of all sensors and every single component refers to a probabilistic sensor model. The barometer information is evaluated using $p(\vec{o}_t \mid \vec{q}_t)_\text{baro}$, whereby absolute position information is given by $p(\vec{o}_t \mid \vec{q}_t)_\text{ib}$ for \docIBeacon{}s and by $p(\vec{o}_t \mid \vec{q}_t)_\text{wifi}$ for \docWIFI{}.