551.577 : 556.16 (m1.1) a markov chain model for the occurrences ofdry and wet...

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551.577 : 556.16 (M1. 1) A Markov chain model for the occurrences of dry and wet days J. (Received 19 N()l)Cmber 1975) Department of !;Iati.t ic. ., Gauhali Universilll Ga"l",ti, .-\BST R.o\CT. Study of rainfall data in India began M early &a 188ff with the work of BlanCord. HiA work. was eetendod by Sir Gil btort. Walker. ),(abalAnobia (1 9-10) , in his ('laMio work, broke eoti rt'ly new grounds with BOund lth ti"tica.1 in hill 8t.udy of the rainfall. runo ff and other metecrologieal ft'aturee of the river bui n. of OriNRL. )(oclel!l based on t1 toohl\.stlo prooesSCA and time eeelee are nnw being applied in meteorologlca l studlee. Gabrie l and Neum snn (1002) used e, )(arko\' chain model in a stu dy of weather conditione in Tel Aviv. We UAe here a. similar Chain model fur tb e oceurro nce of dry and wct.da}·11 in Gauhati (Airport)and ten the Btatistical eignlflcencc of the model. ", ) v, = (v o v o A" = 1 ( P, Po ) + (I- po- p,)" ( Po Po + P, P, Po PO+PI -PI Further, lim A" u-s-co o 1 A = 0( I- po Po ) 1 P, I-p , The a-step transition probabilities are given !ly the elements of A". where where v o = p,f (PJ + P, )and v, = Po/ Cpo + p,l 2. M arkov Chain model As con sidered byOabriel and Neumann (1962), a two-s tate Markov chain model has been used to describe the occurrences of l hy and wet days at Gauhati , Assume that the probability of dry (or wet) days depend on the condition (dry or wet) of the previous day. Let, P, [actualday is wet, given that precedin day is dry]=po and P, [actua l day is dry, given that preceding day is wet]=1'I Denote dry day by state 0 and wet day by st..te 1; the occurrences of dry and wet days can then be denoted by an irredueible )Iarkov chain with two ergodic states 0 and 1 ami tran- sition probability matrix This is in agreement with the observation of Parthasarathy (1958). 431 Here the patterns of occurrences of dry and wet days during two periods have been studied. The days are recorded under two categories : dry and wet. A day is called dry if the rainfall during the 24 hours commencing from 0830 1ST on that day is either " il or trace; otherwise. it is termed wet. One of the two period. is from 1 Mareh to 31 )Iay and the other is from 1 J une to 30 September. The period is pre-mon- soon season and the period J nne-September is monsoon season, the monsoon in Gauhati normally commencing in the first week of June and with- dra wing in the beginning of October [Das 1968). Two sets of data of the pre-monsoon season (lIIareh- are considered : set I covering a total of 4X92 = 368 days in the 4 years, 19 67-70 and set II covering a total of 92 days in the year 1971) . Two other sets of data relating to the mon soon (June-September) are taken : set II I cove" a total of 4X122 =488 days in the four years 1967 -70 ami set IV, a total of 122 days in the year 1975. The data are taken from th e records maintained by the Meteorological Centre Oauhati Airport for rainfall at the Gauhati Airport. The total annual rainfall (in mm) and the amount of rainfall (in mm) during the monsoon months (June-September) during 1964-70 are given in Table 1 It may be seen from the above th at the varia- bility of annual rainfall is low ; except for the year 1967 , rainfall for other years lie within 10 per cent of the average amount 1686·37 mm. t, Introdu ction

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Page 1: 551.577 : 556.16 (M1.1) A Markov chain model for the occurrences ofdry and wet daysmetnet.imd.gov.in/mausamdocs/527410.pdf · 2019. 4. 13. · commencing in the first week of June

551.577 : 556.16 (M1. 1)

A Markov chain model for the occurrences of dry and wet days

J . lI~DII1

(Received 19 N()l)Cmber 1975)

Department of !;Iati.t ic.. , Gauhali Universilll Ga"l", ti,

.-\BST R.o\CT. Study of rainfall data in India began M early &a 188ff with the work of BlanCord. HiA work. waseetendod by Sir Gilbtort. Walker. ),(abalAnobia (19-10) , in his ('laMio work, broke eotirt'ly new grounds with BOundlth ti"tica.1ro:ulln in~. in hill8t.udy of the rainfall. runo ff and other metecrologieal ft'aturee of the river buin. of OriNRL.)(oclel!l based on t1 toohl\.st lo prooesSCA and time eeelee are nnw being applied in meteorologlca l studlee. Gabrie l andNeum snn ( 1002) used e, )(arko\' chain model in a stu dy of weath er conditione in Tel Avi v. We UAe here a. similar~[I\rlm \' Chain model furtbe oceurronce of dry and wct.da}·11 in Gauhati (Airport)and ten the Btatistical eignlflcencc ofthe model.

", )v,

= ( vovo

A" = 1 ( P, Po) +(I- po- p,)" ( PoPo + P, P, Po PO+PI -PI

Further, lim A"u-s-co

o 1

A = 0 ( I - po Po )1 P, I-p,

The a-step transit ion probabilities are given !lythe elements of A".

where

where vo= p,f(PJ +P, ) and v, = Po/Cpo+ p,l

2. Markov Chain model

As considered byOabriel and Neumann (1962),a two-state Markov chain model has been usedto describe the occurrences of lhy and wet daysat Gauhati , Assume that the probability of dry(or wet ) days depend on the condit ion (dry orwet) of the previous day.

Let, P, [actualday is wet, given that precedinday is dry]=po and

P, [actua l day is dry, given that precedingday is wet]=1'I

Denote dry day by state 0 and wet day byst..te 1; the occurrences of dry and wet dayscan then be denoted by an irredueible )Iarkovchain with two ergodic sta tes 0 and 1 ami t ran­sit ion probability matrix

This is in agreement with the observation ofParthasarathy (1958).

431

Here the pat terns of occurrences of dry andwet days during two periods have been studied.The days are recorded under two categories :dry and wet. A day is called dry if the rainfallduring the 24 hours commencing from 0830 1STon that day is either " il or trace; otherwise. it istermed wet. One of the two period. is from 1 Marehto 31 )Iay and the other is from 1 J une to 30September. The period Mareh-~lay is pre-mon­soon season and the period J nne-September ismonsoon season, the monsoon in Gauhati normallycommencing in the first week of June and with­drawing in the beginning of October [Das 1968).Two sets of data of the pre-monsoon season (lIIareh­~lay) are considered : set I covering a total of4X92 = 368 days in the 4 years, 1967-70 andset II covering a tota l of 92 days in the year1971). Two other sets of data relating to themonsoon (June-September) are taken : set IIIcove" a to tal of 4X 122=488 days in the fouryears 1967-70 ami set IV, a total of 122 daysin the year 1975. The data are taken from th erecords maintained by the Meteorological CentreOauhati Airport for rainfall at the GauhatiAirport.

The total annual rainfall (in mm) and theamount of rainfall (in mm) during the monsoonmonths (June-September) during 1964-70 aregiven in Table 1

It may be seen from the above that the varia­bility of annual rainfall is low ; except for theyear 1967, rainfall for other years lie within 10per cent of the average amount 1686·37 mm.

t, Introduction

Page 2: 551.577 : 556.16 (M1.1) A Markov chain model for the occurrences ofdry and wet daysmetnet.imd.gov.in/mausamdocs/527410.pdf · 2019. 4. 13. · commencing in the first week of June
Page 3: 551.577 : 556.16 (M1.1) A Markov chain model for the occurrences ofdry and wet daysmetnet.imd.gov.in/mausamdocs/527410.pdf · 2019. 4. 13. · commencing in the first week of June
Page 4: 551.577 : 556.16 (M1.1) A Markov chain model for the occurrences ofdry and wet daysmetnet.imd.gov.in/mausamdocs/527410.pdf · 2019. 4. 13. · commencing in the first week of June
Page 5: 551.577 : 556.16 (M1.1) A Markov chain model for the occurrences ofdry and wet daysmetnet.imd.gov.in/mausamdocs/527410.pdf · 2019. 4. 13. · commencing in the first week of June