Title: THE STATISTICAL ANALYSIS OF WET AND DRY SPELLS BY BINARY DARMA 1,1 MODEL IN SPLIT,CROATIA
1THE STATISTICAL ANALYSIS OF WET AND DRY SPELLS
BYBINARY DARMA (1,1) MODEL IN SPLIT,CROATIA
- Ksenija Cindric
- Meteorological and Hydrological Service of
Croatia - BALWOIS 2006 Conference, Ohrid
2- 1. Introduction
- 2. The binary DARMA(1,1) model
- Some properties of the DAR(1) and DARMA(1,1)
models - Estimation of parametres
- The distribution of run lengths
- 3. Wet and dry sequences in Split
- 4. Conclusions
31. Introduction
- extreme precipitation events - floods and
droughts are of the vital interest - great spatial and temporal variability of the
precipitation amount - precipitation analysis
complicated (large number of statistical values) - daily precipitation amount data vs. wet and dry
spells in estimating dry(wet)ness of particular
month - DAR(1) (First-order Markov chain) and DARMA(1,1)
models are used and compared - autocorrelation coefficient (acc) - annual
course, Split Marjan,1948-2000 period
4 52. The binary DARMA(1,1) modelSome properties
of the DAR(1) and DARMA(1,1)
- special cases of the more general class of
DARMA(p,q) - DARMA sequence Xn is formed by a probabilistic
linear combination of sequence Yn of i.i.d. rv
in such a way that its marginal distribution is
given by - p(k) P(Yn k), k 0,1,
- DAR(1) r.v. is defined
- Xn
- rk r1k , k 1
An-1, w.p. r Yn, w.p. 1- r
6- DARMA(1,1) r.v. is defined
- Xn
- rk crk-1 , k 1
- - first-order acc c (1-b) (r b -2 r b)
- acf of the daily precipitation sequence - measure
of persistence - one of the most important
statistical property when considering dry and wet
spells length - c can be taken as a model parameter rather
than b.
Yn, w.p. b An-1, w.p. 1- b
7Estimation of parametres
- empirical distribution of run lengths of dry and
wet spells gt mean run lengths m0 and m1 -
-
-
p(0)1-p1
8The distribution of run lengths
- probability distribution of the run lengths of
zeros (T0) - P(T0 n) PXk 0 for all k ? 1,n and Xn1
1 ? X0 1, X1 0, n 1,2, - P( X0 1, X1 0,, Xn 0)
- P(X0 1, X1 0,, Xn 0, Xn1 0) / P X0
1, X1 0 - P(T1 n) analogous
- - transition probabilities are 2x2 matrices and
can be obtained by models parameters, Chang et
al.(1984)
93. Wet and dry sequences in Split
- wet dry day
- Xn
- Example ...0 1 1 1 1 1 1 1 0...
1, if Rn 1 mm 0, if Rn lt 1 mm
May
June
10Table 1. Mean run lengths of wet and dry spells
and estimated parameters for the binary
DARMA(1,1) model. Split Marjan, 1948-2000
11Figure 1. Annual course of the first-order
autocorrelation coefficient (c) for Observatory
Split-Marjan, 1948-2000
12Figure 2. Empirical and theoretical cumulative
frequencies of dry spells in for I, III, VII and
XII. Observatory Split Marjan, 1948-2000
13(No Transcript)
144. Conclusions
Split-Marjan (1948-2000)
- acc one of the most important parameter of
precipitation regime (measure of persistence) - cold period warm period
-
- future work analyse spatial distribution of
acc to the whole Croatian or even Balcanic
territory
15Acknowledgements - wish to thank to Dr. J. Juras
for many valuable suggestions
- References
- Buishand, R.A., 1978 The binary DARMA(1,1)
process as a model for wet and dry sequence.
Dept. of Math., Agricultural Univrsity,
Wageningen, 49 pp. - Chang, T. J., M. L. Kavvas and J. W. Delleur,
1984a Daily precipitation modelling by discrete
autoregressive moving average processes. Water
Resour. Res., 20, 565 580. - Chang, T. J., M. L. Kavvas and J. W. Delleur,
1984b Modeling of sequences of wet and dry days
by binary discrete autoregressive moving average
processes. J. Clim. Appl. Meteor., 23, 1367
1378. - Gabriel, K. R., and J. Neumann, 1962 A Markov
chain model for daily rainfall occurrence at Tel
Aviv. Quart. J. Roy. Meteor. Soc., 88, 90 95. - Juras, J. 1989 On modelling binary
meteorological sequences with special emphasis on
frequencies of warm and cold spells. Rasprave,
24, 29 37. - Juras, J. 1995 Methods for estimating the
temporal variability of rainfall. Ph.D. Thesis,
University of Zagreb, 160 pp.
16- The End
- Thank you for
- your attention