I.Classical probabilities
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1 I.Classical probabilities I.4 Markov chains
2 Markov chains? 2
3 Andrei A. Markov Russian mathematician
4 Markov chains as pedagogic, analytical and prognostic tool. Helps us understand probabilities and their additions and co-variations (also new Bayesian Markov Chain Monte Carlo MCMC techniques) 2. Helps us analyse data in a new and interesting way 3. Provides a good complement to traditional statistical post-processing 4
5 I.4. A simple contingency table? Warning No warning Event occurs Hit (H) Missed event (M) Even does not occur False alarm (F) Correct negative (N) Hit rate (HR) H/(H+M) False alarm rate (FAR) F/(F+N) not F/(F+H) 5
6 A simple contingency table? Following 6 hours rain dry First 6 hours rain 7 28 cases dry 6 72 cases 28 cases 72 cases We note that the climatological rain probability is 28% 6
7 A transition table for rain fall at Stockholm- Arlanda airport (00 typical cases) 62% (7/28) probability of continued rain Following 6 hours rain dry 38% (/28) probability of rain to dry First 6 hours rain 7 28 cases 5% (/72) probability of dry to rain dry 6 28 cases 72 cases 72 cases 85% (6/72) probability of staying dry 7
8 Transition probabilities 62% probability of continued rain Next 6 hours R 38% (/28) probability of rain to dry 5% (/72) probability of dry to rain Last 6 hours R R.38 rain dry 85% (6/72) probability of staying dry 8
9 R R.38 What can we say about the 2 h transition from rain? From to 2-8? rain rain.38 dry rain dry rain dry rain R R
10 R R.38 What can we say about the 2 h transition from dry? From to 2-8? dry dry dry rain dry rain.38 dry rain R R
11 The matrice can also be regarded as an algebraic transition matrix Next 6 hours R Last 6 hours R.38 Then the full force of 3000 years of algebra can be applied, in particular matrix algebra
12 I.4.2 Some matrice algebra 2
13 A brief repetition of matrix algebra...
14 A brief repetition of matrix algebra... ( 2) ( ) ( 3 ) ( 2) ( ) (3 6) 4
15 A brief repetition of matrix algebra...
16 Matrix multiplication yields a forecast Last six hours h 06-2 h 2.38 Forecast 2-8 h later Observed 2-8 h later Verification Last six hours h
17 The matrix multiplication continues... Last six hours h 4.38 Forecast h one day later verification Last six hours h Observed h one day later
18 After repeated multiplications the values converge towards the climate Last six hours h Last six hours h
19 I.4.3 Vector multiplied into the Markov matrice 9
20 Similarities with forecast models: Obs/analysis Model Forecast ( 0) Rain.38 (.38) ( 0 ) Dry.38 ( ) (.70.30) 70% rain 30% dry.38 (.48.52) 20
21 more examples: Obs/analysis Model Forecast (.70.30).38 (.48.52) (.90.0).38 (.58.42).38 ( ) ( 30.70)..which is almost identical with the input vector 2
22 I.4.4 Eigen vectors 22
23 Left eigenvector and -value (.28.72).38 (.28.72) (.28.72) (.28.28).38 (.3.3) eigenvalues 0.47(.28.28) 23
24 Right eigenvector and -value eigenvalues
25 The initial transition matrix can be decomposed into a weighted sum of two new matrices.38 n n 0.47 Eigen value Persistence probabilities Climate probabilities Time folding factor Variability Meteorological interpretation 25
26 Matrix climate matrix + residual.38 n Persistence n Variability % 00 persistence % 20 climate time 26
27 I.4.5 Theoretical and observed period lengths 27
28 .38 Mean period length for rain ( - 0) - 6 hours 5.8 hours Generally (τ) with p ii as the persistence probability of the class: τ t ( pii ) 28
29 Calculated and observed duration of rain and showers Theoretical period length 5.8 h Observed period length 5.9 h Theoretical period length 40 h Observed period length 57 h 29
30 6 hour transition matrix for Arlanda airport weather Ο Θ 0 2/8 3 5/8 6 8/8 Ο.6 Θ
31 0.6 N Ο High persistence for clear sky and rain Ο.0.02 N Θ Θ Low persistence for showers Ο.7.07 N Θ Good persistence for overcast and rain Ο Θ N Very low persistence for variable sky 3
32 END 32
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