5.2 Markovian Concepts for Stochastic Rainfall Time Series
5.2.1 Statistical Assumptions for Spike Characterization in a Markovian
probability, π₯π, at time, π. Thus, the transition probability from one regime to another is based on a conditional probability relation. For a Markov process, its future probabilistic state depends only on most its current state. How the process arrives at that state is irrelevant [129]. Thus, the conditional probability of a spike going from stateπto state πin a time interval is a homogeneous time Markov chain process described by:
π(ππ+1=π/ππ=π) =πππβπ, π (5.5) where πππ is the transition probability ππ = π, represents the spike, π in regime, π, at the current time index, π, and ππ+1 = π, represents spike, π , is in a regime, π, at the next time index, π+ 1. Given the spikeβs current regime, the next spike regime will be conditionally independent of the past.
From Markov property it can be presented that given the current spikeβs regime, the next spikeβs regime is conditionally independent of the past. This statement is seen in Figure 5-1 that gives that the system can move from one state to another or continues remaining in the same regime. Figure 5-1 shows the spikes of rainfall rate remains changing within shower regime for the first 17 minutes and then switches to thunderstorm state. Figure 5-1 also show the spikeβs queue parameters such as service, inter-arrival and overlap time of spikes. The inter-arrival time,π‘π, is defined as the time variation between the arrivals of two successive rain clouds/spikes at the identified reference point. The service time, π‘π may be defined as the real duration of the spike. The other parameter, is overlap time π‘π , known as the intercept time between a βdyingβ spike and arriving spike. Overlapping spikes can be seen as a major factor accommodating the regeneration of detectable.
Figure 5-1: Rainfall rate against time in minute on September 3, 2015 at jimma
C. Each spike exists in an event for specified period of time, ππ, before transiting to another regime. ππ is defined as sojourn time of spike and subscript Γ°Δ°ΕΕ° implies the regimes (or states).
ππ =ππ·, ππ, ππ, ππ (5.6)
Figure 5-2. explains the details of the sojourn time; where we depict a simple path of four rainfall rate regimes namely: drizzle (D), widespread (W), shower (S) and thunderstorm (T) to show the duration of spikes in a Markov chain. Figure 5-2 shows that the process starts from regime D at timeπ‘= 0, stays there for an amount of timeππ·, makes an instantaneous state change to stateπat timeπ1, stays there forππamount of time, makes an instantaneous state change to stateπ at timeπ2, and so on.
Figure 5-2: Transition pattern between rain spikes of different rain rate peaks in a typical rain event
Since ππ denotes the sojourn time of rainfall rate spike in state i before transiting to a different regime, the amount of ππ, the time in which the spike spent in one regime before the transition is also a random process. Therefore, the sojourn time could be characterized from a probability distribution point of view. In this work, the sojourn time distribution of rainfall rate spike is determined statistically from experimental dataset for the four rainfall regimes.
D. The transition probability is bounded within 0β€πππ β€1such that,π, π,1, , π π. Each element in πππ implies the probability of switching from a state,π, to state, π, or remain in the same state. All elements of the matrix are greater than or equal to zero. The general state transition matrix available for πΓπmatrix is thus given:
πππ =
β‘
β’
β’
β’
β’
β’
β’
β£
π11 . . π1π . . . . . . . . ππ1 . . πππ
β€
β₯
β₯
β₯
β₯
β₯
β₯
β¦
π, πβπ
In this work, the values of π are 2, 3 and 4 respectively for widespread, shower and thunderstorm events. i.e for widespread events the transition of the spike is between drizzle
among the four rainfall rate regimes.
The state transition matrix available for widespread events is thus given:
ππ€ππππ πππππ=
β‘
β£
ππ·π· ππ·π
ππ π· ππ π
β€
β¦
whereππ·π·, ππ·π, ππ π·, ππ π, are the transition probabilities of drizzle (D), and Widespread (W) spikes. The state transition matrix available for shower events is thus given:
ππ βππ€ππ =
β‘
β’
β’
β’
β£
ππ·π· ππ·π ππ·π
ππ π· ππ π ππ π πππ· πππ πππ
β€
β₯
β₯
β₯
β¦
whereππ·π·, ππ·π, ππ·π, ππ π·, ππ π, ππ π, πππ·, πππ, πππ are the transition probabilities of drizzle (D), Widespread (W) and shower (S) spikes. For thunderstorm events P is given by
ππ‘βπ’πππππ π‘πππ =
β‘
β’
β’
β’
β’
β’
β’
β£
ππ·π· ππ·π ππ·π ππ·π ππ π· ππ π ππ π ππ π
πππ· πππ πππ πππ ππ π· ππ π ππ π ππ π
β€
β₯
β₯
β₯
β₯
β₯
β₯
β¦
whereππ·π·, ππ·π, ππ·π, ππ·π, ππ π·, ππ π, ππ π, ππ π, πππ·, πππ, πππ, πππ, ππ π·, ππ π, ππ π, ππ π, are the transition probabilities of drizzle (D), widespread (W), shower (S) and thunderstorm (T) spikes.
A transition probability matrix could be expressed as a transition diagram. Each node 0 shows a regime of the Markov chain indicating with a text inside; an arrow links state π with π if a transition exists and the probability transition πππ is written on that linking arrow, even if the transition is to the same state [134]. The diagram is also used to present the model definitions; it is easy to see in this diagram the possible jumps between regimes depending on the probability. Figures 5-3, 5-4, 5.5 present the transition probability diagram for a shower and thunderstorm events of Markov chain with its transition matrix.
Figure 5-3: State transition diagrams for spikes of rainfall in widespread
Figure 5-4: State transition diagrams for spikes of rainfall in shower
Figure 5-5: State transition diagrams for spikes of rainfall in thunderstorm
E. The other essential parameter of the Markov chains is the vector π of steady-state, which shows the total occurring percentage of the state in the chain. This vector is equivalent to the kth-power ofπ i.e.,ππΎ. Steady-state behaviour of a Markov chain can be formulated as (5.7). This is given in [135]:
[π1, ...ππ] = [π1, ...ππ]
β‘
β’
β’
β’
β’
β’
β’
β£
π11 . . π1π . . . . . . . . ππ1 . . πππ
β€
β₯
β₯
β₯
β₯
β₯
β₯
β¦
where,ππ, is the steady state probability for n states, whereas the sum of elements within this probability vector at steady state must be unity:
π
βοΈ
π=1
ππ = 1 (5.7)