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THE STATISTICAL ANALYSIS OF WET AND DRY SPELLS BY BINARY DARMA 1,1 MODEL IN SPLIT,CROATIA

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Title: THE STATISTICAL ANALYSIS OF WET AND DRY SPELLS BY BINARY DARMA 1,1 MODEL IN SPLIT,CROATIA


1
THE 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

3
1. 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
  • ? 4331
  • 1626'
  • h 122 m

5
2. 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
7
Estimation of parametres
  • empirical distribution of run lengths of dry and
    wet spells gt mean run lengths m0 and m1


p(0)1-p1
8
The 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)

9
3. 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
10
Table 1. Mean run lengths of wet and dry spells
and estimated parameters for the binary
DARMA(1,1) model. Split Marjan, 1948-2000
11
Figure 1. Annual course of the first-order
autocorrelation coefficient (c) for Observatory
Split-Marjan, 1948-2000
12
Figure 2. Empirical and theoretical cumulative
frequencies of dry spells in for I, III, VII and
XII. Observatory Split Marjan, 1948-2000
13
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14
4. 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

15
Acknowledgements - 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
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