

- Open Access
- [post-views]
- Authors : Prakasam. S, Venkatesh. A
- Paper ID : IJERTV14IS040069
- Volume & Issue : Volume 14, Issue 04 (April 2025)
- Published (First Online): 11-04-2025
- ISSN (Online) : 2278-0181
- Publisher Name : IJERT
- License:
This work is licensed under a Creative Commons Attribution 4.0 International License
Fuzzy Mathematical Fatigue Life Model for the Effect of North West India Rainfall
Prakasam. S
Assistant Professor of Mathematics,
A. V. V. M. Sri Pushpam College (Autonomous) (Affiliated to Bharathidasan University, Tiruchirappalli),
Thanjavur (Dt), Tamilnadu, India.
Venkatesh. A
Assistant Professor of Mathematics,
A. V. V. M. Sri Pushpam College (Autonomous) (Affiliated to Bharathidasan University, Tiruchirappalli),
Thanjavur (Dt), Tamilnadu, India.
ABSTRACT:
In this paper, we use the mathematical Fatigue Life distribution model to calculate the rainfall in the northwestern states of India, namely Uttar Pradesh, Uttarakhand, Delhi, Punjab, Himachal Pradesh, Jammu and Kashmir, and Rajasthan, and see which year received the most rainfall.
-
INDRODUCTION:
The North West Indian subdivisions by the Meteorological Department include 7 states in India.
-
Uttar Pradesh
-
Uttarakhand
-
Delhi
-
Punjab
-
Himachal Pradesh
-
Jammu & Kashmir
-
Rajasthan
-
History of North West India:
Rainfall and temperature are the most important environmental factors influencing crop growth, development, and yield. The northwestern (NW) part of India is one of the main regions of food grain production of the country. North-East India displays, to a large extent, the character of tropical climate, especially in the valleys. The region has a monsoon climate with heavy to very heavy rains, confined within four summer months from June to September. There are three distinct seasons in the region: winter, summer, and the rainy season.
-
Uttar Pradesh:
Uttar Pradesh is a state in India, stretches back several millennia. The region shows the presence of human habitation dating back to between 85,000 and 73,000 years ago. Additionally, the region seems to have been domesticated as early as 6,000 BC. After independence in 1947, the United Provinces were renamed Uttar Pradesh in 1950.
Uttar Pradesh is a state in northern India. With over 241 million inhabitants, it is the most populated state in India as well as the most populous country subdivision in the world more populous than all but four other countries outside of India and accounting for 16.5 percent of the total population of India. The state is divided into 18 divisions and 75 districts. On 9 November 2000, a new state, Uttaranchal (now Uttarakhand), was created from Uttar Pradesh's western Himalayan hill region. The two major rivers of the state, the Ganges and its tributary Yamuna, meet at the Triveni Sangam in Prayagraj (formerly Allahabad), a Hindu pilgrimage site. Other notable rivers are Gomti and Saryu. The forest cover in the state is 6.1 per cent of the state's geographical area.
The climate of Uttar Pradesh (U.P) is primarily defined as humid subtropical with dry winter (Cwa) type with parts of Western U.P. as hot semi- arid (BSh) type. Alternatively, some authors refer to it as tropical monsoon. Variations do exist in different parts of the large state. The average annual rainfall is approximately 650 millimetres in the southwestern part of UP. The precipitation is around 1000 millimetres in the southeast and east of UP.
-
Uttarakhand:
Uttarakhand is a Himalayan state in North India, nestled between the Tibetan Plateau and the Indo- Gangetic Plains. The name, which means "northern land" or "section" or "northern part" in Sanskrit was made popular in the 80s as part of the wider statehood struggle within the region. Initially, it was believed that due to harsh climate and mountainous terrain, this was a barren and uninhabited land. But after various excavations and the study of ancient literature, it is now established that the history of Uttarakhand goes back to Stone Age. Uttarakhand is popularly referred to as "the land of the gods" (Devbhumi) owing to its huge number of Hindu pilgrimage sites and proximity to Mount Kailash.
Uttarakhand state is located between 28°43 – 31°27 N latitudes and 77°34 – 81°02 E longitudes in the northern part of India. The state is mostly hilly and has international boundary with China (Tibet) in the north and Nepal in the east and state boundary with Himachal Pradesh in the northwest. The state has foothills areas in the south and southwest which are bounded by Uttar Pradesh.
Uttarakhand state has total geographical area of 53,485 sq. km, of which 86% is mountainous and 65% is covered by forest.The state is rich in natural resources especially water and forests with many glaciers, perennial rivers, dense forests and snow- capped mountain peaks. Annual rainfall ranges from 92 to 237 cm.
-
Delhi:
Delhi has been an important political centre of India as the capital of several empires. The recorded history of Delhi begins with the 8th century Tomar Rajputs kingdom. Delhi, city and national capital, and union territory, north-central India. The city of Delhi actually consists of two components: Old Delhi, in the north, the historic city; and New Delhi, in the south, since 1947 the capital of India, built in the first part of the 20th century as the capital of British India.
One of the countrys largest urban agglomerations, Delhi sits astride (but primarily on the west bank of) the Yamuna River, a tributary of the Ganges (Ganga) River, about 100 miles (160 km) south of the Himalayas. The national capital territory embraces Old and New Delhi and the surrounding metropolitan region, as well as adjacent rural areas. Delhi receives an average annual precipitation of 774.4 mm.
The climate of Delhi is an overlap between monsoon-influenced and semi-arid, with high variation between summer and winter temperatures and precipitation. Summer starts in early April and peaks in late May or early June, with average
temperatures near 38 °C (100 °F) although occasional heat waves can result in highs close to 45 °C (113 °F) on some days and therefore higher apparent temperature. The monsoon starts in late June and lasts until mid-September, with about
797.3 mm (31.39 inches) of rain. The average temperatures are around 29 °C (84 °F), although they can vary from around 25 °C (77 °F) on rainy days to 3540 °C (95104 °F) during dry spells.
-
Punjab:
The History of Punjab refers to the past history of Punjab region which is a geopolitical, cultural, and historical region in the northwest of South Asia, comprising western Punjab province in Pakistan and eastern Punjab state in India. It is believed that the earliest evidence of human habitation in Punjab traces to the Soan valley of the Pothohar,between the Indus and the Jhelum rivers, where Soanian culture developed between 774,000 BC and 11,700 BC.
Some two-fifths of Punjabs population is engaged in the agricultural sector, which accounts for a significant segment of the states gross product. Punjab produces an important portion of Indias food grain and contributes a major share of the wheat and rice stock held by the Central Pool . Much of the states agricultural progress and productivity is attributable to the so-called Green Revolution, an international movement launched in the 1960s that introduced not only new agricultural technologies but also high-yielding varieties ofwheat and rice.
Punjab has an inland subtropical location, and its climate is continental, being semiarid to subhumid. In June, the warmest month, daily temperatures in Ludhiana usually reach about 100 °F (upper 30s C) from a low in the upper 70s F (mid-20s C). In January, the coolest month, daily temperatures normally rise from the mid-40s (about 7 °C) into the mid-60s F (upper 10s C). The average annual rainfall is 273 to 676 mm .
-
Himachala Pradesh:
Himachal Pradesh was established in 1948 as a Chief Commissioner's Province within the Union of India. The province comprised the hill districts around Shimla and southern hill areas of the former Punjab region. Thus Himachal emerged as the eighteenth state of the Indian Union. After independence the Chief Commissioner's province of H.P. came into being on 15 April 1948. Himachal became a part C state on 26 January 1950 with the implementation of the Constitution of India. Himachal Pradesh became Union Territory on 1 November 1956. On 18 December 1970 the State of Himachal Pradesh Act was passed by Parliament and the new state came into being on 25 January 1971.
There is a huge variation in the climatic conditions of Himachal Pradesh due to variation in altitude (3606500 metres). The climate varies from hot and sub-humid tropical (450900 metres) in the southern low tracts, warm and temperate (900 1800 metres), cool and temperate (18002400 metres) and cold glacial and alpine (24004800 metres) in the northern and eastern high elevated mountain. Pollution is affecting the climate of almost all the states of India. The average annual rainfall is 1,251(mm). The rainy season start at the end of the month of June.
The spring season starts from mid February to mid April. The weather is pleasant and comfortable in the season. The rainy season start at the end of the month of June. The landscape lushes green and fresh. During the season streams and natural springs are replenished. The average annual rainfall is 1,251(mm).
-
Jammu & Kashmir:
Jammu and Kashmir, also known as Kashmir and Jammu, was a princely state in a subsidiary alliance under British East India Company rule from 1846 to 1858 and under the paramountcy of the British Crown, from 1858 until the Partition of India in 1947, when it became a disputed territory, now administered by three countries: China, India, and Pakistan. Jammu and Kashmir is an State of India with population of Approximate 1.25 Crores. The population of Jammu and Kashmir state is 12,541,302. The density of Jammu and Kashmir state is 56 per sq km. Jammu and Kashmir State is spread over 222,236 Sq Km.
The inter mountainous valley of Kashmir has unique geographical setting and it is located 130 between the Greater Himalayas in the north and Pir Panjal ranges in the south, roughly within the latitude and longitude ranges of 330 55´ to 34o 50´ and 74o 30´ to 75o 131 35´ respectively. The heights of these 132 mountains range from about 3,000 to 5,000 m and the mountains strongly influence the weather and 133 climate of the region.
State of Jammu and Kashmir is home to several Himalayan glaciers. Jhelum, Indus, Tawi, Ravi and Chenab are major rivers flowing through the state. the state of Jammu comprises of three distinct climatic regions: cold arid desert areas of Ladakh, temperate Kashmir Valley, and the humid sub-tropical region of Jammu. The mean annual rainfall in cold arid zone varies from 100 mm to
300 mm received by western disturbance. The average rainfall annually is usually between 700 and 750 mm.
-
Rajasthan:
The history of human settlement in the western Indian state of Rajasthan dates back to
about 100,000 years ago. Around 5000 to 2000 BCE many regions of Rajasthan belonged as the site of the Indus Valley Civilization. Kalibangan is the main Indus site of Rajasthan, here fire altars have been discovered, similar to those found at Lothal. Around 2000 BCE, Sarasvati River flowed through the Aravalli mountain range in the state.
Rajasthan state of northwestern India, located in the northwestern part of the Indian subcontinent. It is bounded to the north and northeast by the states of Punjab and Haryana, to the east and southeast by the states of Uttar Pradesh and Madhya Pradesh, to the southwest by the state of Gujarat, and to the west and northwest by the provinces of Sindh and Punjab in Pakistan.
The capital city is Jaipur, in the east-central part of the state. The Aravalli (Aravali) Range forms a line across the state running roughly from Guru Peak on Mount Abu (5,650 feet [1,722 metres]), near the town of Abu in the southwest, to the town of Khetri in the northeast. About three-fifths of the state lies northwest of that line, leaving the remaining two- fifths in the southeast. Those are the two natural divisions of Rajasthan. The northwestern tract is generally arid and unproductive, although its character shifts gradually from desert in the far west and northwest to comparatively fertile and habitable land toward the east. The region includes the Thar (Great Indian) Desert. The annual rainfall in the East and West Rajasthan is about 64.9 cm and 32.7 cm respectively.
-
-
FATIGUE LIFE DISTRIBUTION
The BirnbaumSaunders distribution, also known as the fatigue life distribution, is a probability distribution used extensively in reliability applications to model failure times. There are several alternative formulations of this distribution in the literature. It is named after Z. W. Birnbaum and S. C. Saunders. The Fatigue life distribution is closed under scalar multiplication and under reciprocation; its median coincides with the BS scale parameter; it has different shapes for its probability density function (PDF), which cover high, medium, and low asymmetry levels .
This distribution was developed to model failures due to cracks. A material is placed under repeated cycles of stress. The jth cycle leads to an increase in the crack by Xj amount. The sum of the Xj is assumed to be normally distributed with mean n and variance n2. The probability that the crack does not exceed a critical length is
where is the cdf of normal distribution. The more usual form of this distribution is:
Here is the shape parameter and is the scale parameter.
-
Proprerties
The BirnbaumSaunders distribution is unimodal with a median of .
Since the general form of probability functions can be expressed in terms of the standard distribution, all of the subsequent formulas are given for the standard form of the function.
2.4 Cumulative Distribution Function
The formula for the cumulative distribution function is
Mean =
²
(1 + )
Variance = ( )² (1 + 5² )
4
2
Given a data set that is thought to be Birnbaum Saunders distributed the parameters' values are best estimated by maximum likelihood.
If T is BirnbaumSaunders distributed with parameters and then T1 is also Birnbaum- Saunders distributed with parameters and 1.
-
Probability density function
The general formula for the probability density function (pdf) is
where is the shape parameter, is the location parameter, is the scale parameter, and s the probability density function of the standard normal distribution.
-
Standard Fatigue Life Distrinution
The case where = 0 and = 1 is called the standard fatigue life distribution. The pdf for the standard fatigue life distribution reduces to
where is the cumulative distribution function of the standard normal distribution.
2.5 Quantile Function
The formula for the quantile function is
where 1 is the quantile function of the standard normal distribution.
-
-
APPLICATION
-
Application – I
In this work, We observe the normal monthly rainfall for the state Uttar Pradesh which is the state of North West India from the month January to December during the year 2012. We present a model of Rainfall for the state Uttar Pradesh in India using the Fatigue Life distribution with two parameters.
We have constructed a model of Rainfall that produces result that qualitatively and quantitatively agree with experimental observation.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
26
5.75
3.95
5.55
0.45
16.35
273.45
233.9
163.7
1.0
0.2
1.9
Table 3.1.1 Rainfall of Uttar Pradesh in 2012
The scale and shape parameters of Fatigue life distribution in Table 3.1.1, = 3.6399 = 8.46115. The triangular fuzzy number is = [ 3.1021, 3.6399, 4.1777 ] and = [ 7.92335, 8.46115, 8.99895 ] are corresponding cuts are = [3.1021+0.5378 , 4.1777-0.5378 ] = [ 7.92335+0.5378 , 8.99895-0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
3.1021
4.1777
7.92335
8.99895
46.04665
87.52908
0.1
3.15588
4.12392
7.97713
8.94517
47.70156
85.00915
0.2
3.20966
4.07014
8.03091
8.89139
49.3978
82.53895
0.3
3.26344
4.01636
8.08469
8.83761
51.13583
80.11801
0.4
3.31722
3.96258
8.13847
8.78383
52.91612
77.74586
0.5
3.371
3.9088
8.19225
8.73005
54.73914
75.42203
0.6
3.42478
3.85502
8.24603
8.67627
56.60536
73.14607
0.7
3.47856
3.80124
8.29981
8.62249
58.51524
70.9175
0.8
3.53234
3.74746
8.35359
8.56871
60.46924
68.73586
0.9
3.58612
3.69368
8.40737
8.51493
62.46784
66.60068
1
3.6399
3.6399
8.46115
8.46115
64.5115
64.5115
Table 3.1.2 Lower and Upper alpha cut for mean
-
Application – II
In this work, We observe the normal monthly rainfall for the state Uttarakhand which is the state of North West India from the month January to December during the year 2012.
We present a model of Rainfall for the state Uttarakhand in India using the Fatigue Life distribution with two parameters.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
53.4
13.4
30.8
46.6
10.7
48.0
389.8
461.2
223.3
8.8
4.6
19.2
Table 3.2.1 Rainfall of Uttarakhand in 2012
The scale and shape parameter of Fatigue life distribution in Table 3.2.1, = 1.6981 = 47.012. The triangular fuzzy number is = [ 1.1603, 1.6981, 2.2359 ] & = [ 46.4742, 47.012, 47,5498 ] are corresponding cuts are = [1.1603+0.5378 , 2.2359-0.5378 ] & = [ 46.4742+0.5378 , 47.5498-0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
1.1603
2.2359
46.4742
47.5498
77.75822
166.4064
0.1
1.21408
2.18212
46.52798
47.49602
80.81887
160.5757
0.2
1.26786
2.12834
46.58176
47.44224
84.02113
154.8949
0.3
1.32164
2.07456
46.63554
47.38846
87.36544
149.3637
0.4
1.37542
2.02078
46.68932
47.33468
90.85229
143.9815
0.5
1.4292
1.967
46.7431
47.2809
94.48212
138.7479
0.6
1.48298
1.91322
46.79688
47.22712
98.25542
133.6624
0.7
1.53676
1.85944
46.85066
47.17334
102.1727
128.7247
0.8
1.59054
1.80566
46.90444
47.11956
106.2343
123.9341
0.9
1.64432
1.75188
46.95822
47.06578
110.4408
119.2902
1
1.6981
1.6981
47.012
47.012
114.7926
114.7926
Table 3.2.2 Lower and Upper alpha cut for mean
-
Application – III
In this work, We observe the normal monthly rainfall for the state Delhi which is the state of North West India from the month January to December during the year 2012. We present a model of Rainfall for the state Delhi in India using the Fatigue Life distribution with two parameters. We have constructed a model of Rainfall that produces result that qualitatively and quantitatively agree with experimental observation.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
4.6
0.1
0.3
13.6
3.6
4.4
57.9
163.5
57.1
4.0
0.6
3.9
Table 3.3.1 Rainfall of Delhi in 2012
The scale and shape parameter of Fatigue life distribution in table 3.3.1 = 3.1529 =4.2156, The triangular fuzzy number is = [ 2.6151, 3.1529, 3.6907 ] & = [ 3.6778, 4.2156, 4.753 ] are corresponding cuts are = [ 2.6151+0.5378 , 3.6907-0.5378 ] = [ 3.6778+0.5378 , 4.7534-0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
2.6151
3.6907
3.6778
47.5498
16.25357
371.394
0.1
2.66888
3.63692
3.73158
47.49602
17.02145
361.6154
0.2
2.72266
3.58314
3.78536
47.44224
17.81556
351.9951
0.3
2.77644
3.52936
3.83914
47.38846
18.63637
342.5328
0.4
2.83022
3.47558
3.89292
47.33468
19.48435
333.228
0.5
2.884
3.4218
3.9467
47.2809
20.35995
324.0802
0.6
2.93778
3.36802
4.00048
47.22712
21.26365
315.0889
0.7
2.99156
3.31424
4.05426
47.17334
22.19592
306.2537
0.8
3.04534
3.26046
4.10804
47.11956
23.15722
297.5741
0.9
3.09912
3.20668
4.16182
47.06578
24.14801
289.0497
1
3.1529
3.1529
4.2156
47.012
25.16877
280.6799
Table 3.3.2 Lower and Upper alpha cut for mean
-
Application – IV
In this work, We observe the normal monthly rainfall for the state Punjab which is the state of North West India from the month January to December during the year 2012. We present a model of Rainfall for the state Punjab in India using the Fatigue Life distribution with two parameters. We have constructed a model of Rainfall that produces result that qualitatively and quantitatively agree with experimental observation.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
35.8
2.9
1.9
20.2
0.8
9.6
67.7
105.1
83.5
2.8
0.4
8.2
Table 3.4.1 Rainfall of Punjab in 2012
The scale and shape parameter of Fatigue life distribution in Table 3.4.1 =2.2535 =7.7669. The triangular fuzzy number is = [ 1.7157, 2.2535, 2.7913 ] & = [ 7.2291, 7.7669, 8.3047 ] are corresponding cuts are
= [1.7157+0.5378 , 2.7913-0.5378 ] & = [ 7.2291+0.5378 , 8.3047-0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
1.7157
2.7913
7.2291
8.3047
17.86899
40.65714
0.1
1.76948
2.73752
7.28288
8.25092
18.68445
39.16718
0.2
1.82326
2.68374
7.33666
8.19714
19.53121
37.71693
0.3
1.87704
2.62996
7.39044
8.14336
20.40973
36.30591
0.4
1.93082
2.57618
7.44422
8.08958
21.32049
34.93365
0.5
1.9846
2.5224
7.498
8.0358
22.26395
33.5997
0.6
2.03838
2.46862
7.55178
7.98202
23.24058
32.30357
0.7
2.09216
2.41484
7.60556
7.92824
24.25084
31.04482
0.8
2.14594
2.36106
7.65934
7.87446
25.29519
29.82296
0.9
2.19972
2.30728
7.71312
7.82068
26.37412
28.63754
1
2.2535
2.2535
7.7669
7.7669
27.48808
27.48808
Table 3.4.2 Lower and Upper alpha cut for mean
-
Application – V
In this work, We observe the normal monthly rainfall for the state Himachal Pradesh which is the state of North West India from the month January to December during the year 2012. We present a model of Rainfall for the state Himachal Pradesh in India using the Fatigue Life distribution with two parameters. We have constructed a model of Rainfall that produces result that qualitatively and quantitatively agree with experimental observation.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
112.1
66.4
43.2
64.1
11.5
25.5
207.1
311.6
152.1
2.9
6.7
31.6
Table 3.5.1 Rainfall of Himachal Pradesh in 2012
The scale and shape parameter of Fatigue life distribution in Table 3.5.1, =1.6073 =35.913. The triangular fuzzy number is = [ 1.0695, 1.6073, 2.1451 ] & = [ 35,3752, 35.913, 36.4508 ] are corresponding cuts are = [1.0695+0.5378 , 2.1451-0.5378 ] = [ 35.3752+0.5378 , 36.4508-0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
1.0695
2.1451
35.3752
36.4508
55.60681
120.3141
0.1
1.12328
2.09132
35.42898
36.39702
57.78038
115.9904
0.2
1.17706
2.03754
35.48276
36.34324
60.06291
111.784
0.3
1.23084
1.98376
35.53654
36.28946
62.45488
107.6945
0.4
1.28462
1.92998
35.59032
36.23568
64.95676
103.7214
0.5
1.3384
1.8762
35.6441
36.1819
67.569
99.86433
0.6
1.39218
1.82242
35.69788
36.12812
70.29207
96.12274
0.7
1.44596
1.76864
35.75166
36.07434
73.12645
92.49619
0.8
1.49974
1.71486
35.80544
36.02056
76.0726
88.9842
0.9
1.55352
1.66108
35.85922
35.96678
79.13098
85.58631
1
1.6073
1.6073
35.913
35.913
82.30206
82.30206
Table 3.5.2 Lower and Upper alpha cut for mean
-
Application VI
In this work, we observe the normal monthly rainfall for the state Jammu & Kashmir which is the state of North West India from the month January to December during the year 2012. We present a model of Rainfall for the state Jammu & Kashmir in India using the Fatigue Life distribution with two parameters.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
120.2
116.7
53.3
112.5
60.1
42.9
121.0
256.4
138.5
14.9
12.7
67.5
Table 3.6.1 Rainfall of Jammu & Kashmir in 2012
The scale and shape parameter of Fatigue life distribution in Table 3.6.1, =0.92999 =64.065 The triangular fuzzy number is = [ 0.39219, 0.92999, 1.46779 ] & = [ 63.5272, 64.065, 64.6028 ] are corresponding cuts are
= [0.39219+0.5378 , 1.46779-0.5378 ] = [ 63.5272+0.5378 , 64.6028-0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
0.39219
1.46779
63.5272
64.6028
68.41285
134.1932
0.1
0.44597
1.41401
63.58098
64.54902
69.90377
129.0795
0.2
0.49975
1.36023
63.63476
64.49524
71.58115
124.1606
0.3
0.55353
1.30645
63.68854
64.44146
73.44548
119.4362
0.4
0.60731
1.25267
63.74232
64.38768
75.49721
114.9057
0.5
0.66109
1.19889
63.7961
64.3339
77.73682
110.5687
0.6
0.71487
1.14511
63.84988
64.28012
80.16477
106.4246
0.7
0.76865
1.09133
63.90366
64.22634
82.78153
102.4732
0.8
0.82243
1.03755
63.95744
64.17256
85.58756
98.71376
0.9
0.87621
0.98377
64.01122
64.11878
88.58333
95.14597
1
0.92999
0.92999
64.065
64.065
91.76931
91.76931
Table 3.6.2 Lower and Upper alpha cut for mean
-
Application – VII
In this work, We observe the normal monthly rainfall for the state Rajasthan which is the state of North West India from the month January to December during the year 2012. We present a model of Rainfall for the state Rajasthan in India using the Fatigue Life distribution with two parameters.
Month
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Rainfall (mm)
1.1
0.0
0.0
6.35
12.05
10.5
104.4
261.8
109.1
0.95
0.0
0.75
Table 3.7.1 Rainfall of Rajasthan in 2012
The scale and shape parameter of Fatigue life distribution =2.53515 =11.39415. The triangular fuzzy number is = [ 1.99735, 2.53515, 3.07295 ] & = [ 10.85635, 11.39415, 11.93195 ] are
corresponding cuts are = [1.99735+0.5378 , 3.07295-0.5378 ] & = [ 10.85635+0.5378 , 11.93195- 0.5378 ]
low
up
low
up
low E(X)
up E(X)
0
1.99735
3.07295
10.85635
11.93195
32.51155
68.26878
0.1
2.05113
3.01917
10.91013
11.87817
33.86032
66.01523
0.2
2.10491
2.96539
10.96391
11.82439
35.25251
63.8135
0.3
2.15869
2.91161
11.01769
11.77061
36.68859
61.66312
0.4
2.21247
2.85783
11.07147
11.71683
38.16902
59.56363
0.5
2.26625
2.80405
11.12525
11.66305
39.69427
57.51456
0.6
2.32003
2.75027
11.17903
11.60927
41.26481
55.51544
0.7
2.37381
2.69649
11.23281
11.55549
42.88111
53.56581
0.8
2.42759
2.64271
11.28659
11.50171
44.54362
51.6652
0.9
2.48137
2.58893
11.34037
11.44793
46.25282
49.81314
1
2.53515
2.53515
11.39415
11.39415
48.00917
48.00917
Table 3.7.2 Lower and Upper alpha cut for mean
-
Discussion
UP
Uttarakhand
Delhi
Punjab
HP
J & K
Rajasthan
0
46.04665
77.75822
16.25357
17.86899
55.60681
68.41285
32.51155
0.1
47.70156
80.81887
17.02145
18.68445
57.78038
69.90377
33.86032
0.2
49.3978
84.02113
17.81556
19.53121
60.06291
71.58115
35.25251
0.3
51.13583
87.36544
18.63637
20.40973
62.45488
73.44548
36.68859
0.4
52.91612
90.85229
19.48435
21.32049
64.95676
75.49721
38.16902
0.5
54.73914
94.48212
20.35995
22.26395
67.569
77.73682
39.69427
0.6
56.60536
98.25542
21.26365
23.24058
70.29207
80.16477
41.26481
0.7
58.51524
102.1727
22.19592
24.25084
73.12645
82.78153
42.88111
0.8
60.46924
106.2343
23.15722
25.29519
76.0726
85.58756
44.54362
0.9
62.46784
110.4408
24.14801
26.37412
79.13098
88.58333
46.25282
1
64.5115
114.7926
25.16877
27.48808
82.30206
91.76931
48.00917
lower E(X)
500
450
400
350
300
250
200
150
100
50
0
Rajasthan
J & K HP
Punjab Delhi
Uttarakhand
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9
alpha value
1
UP
Rainfall
Table 3.8.1 Lower fuzzy mean value of North West India
Fig: 3.8.1 Fuzzy lower mean value of North West India
UP
Uttarakhand
Delhi
Punjab
HP
J & K
Rajasthan
0
87.52908
166.4064
371.394
40.65714
120.3141
134.1932
68.26878
0.1
85.00915
160.5757
361.6154
39.16718
115.9904
129.0795
66.01523
0.2
82.53895
154.8949
351.9951
37.71693
111.784
124.1606
63.8135
0.3
80.11801
149.3637
342.5328
36.30591
107.6945
119.4362
61.66312
0.4
77.74586
143.9815
333.228
34.93365
103.7214
114.9057
59.56363
0.5
75.42203
138.7479
324.0802
33.5997
99.86433
110.5687
57.51456
0.6
73.14607
133.6624
315.0889
32.30357
96.12274
106.4246
55.51544
0.7
70.9175
128.7247
306.2537
31.04482
92.49619
102.4732
53.56581
0.8
68.73586
123.9341
297.5741
29.82296
88.9842
98.71376
51.6652
0.9
66.60068
119.2902
289.0497
28.63754
85.58631
95.14597
49.81314
1
64.5115
114.7926
280.6799
27.48808
82.30206
91.76931
48.00917
Table 3.8.2 Upper fuzzy mean value of North West India
Upper E(X)
1200
1000
800
600
400
200
0
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9
Alpha value
1
rajasthan
J&K HP
punjab delhi uttarakhand
up
Rainfall
Fig: 3.8.2 Fuzzy Upper mean value of North West India
-
-
CONCLUSION
This chapter has provided a brief introduction to the fatigue Life distribution and their application in fuzzy Mathematical modeling. Finally in this paper, if the fuzzy mean is increasing in lower alpha cut values and it decreases in upper alpha cut values. In this work, we observe the normal monthly rainfall of the North West India from the month January to December during the year 2012. Using the Fatigue life distribution we present the lower and upper fuzzy mean value of North West India. In this observation the state Rajasthan has the highest lower and upper mean value in North east India . Finally we conclude that Rajasthan gets highest level of rainfall during the year 2012.
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[10]. Novák, V.; Perfilieva, I.; Moko, J., Mathematical principles of fuzzy logic Dordrecht: Kluwer Academic. ISBN 978-0-7923-8595-0, 1999. [11]. A. Venkatesh, S. Prakasam, A Mathematical Model for the Effect of Parathyroid Hormone using Fuzzy Log- Normal Distribution, International Journal of Recent Technology and Engineering, Volume-7, Issue-6S (2019), pp.971-973. DOI:http://www.doi.org/10.35940/ijrte.F0398.0376S19.
[12]. Prakasam. S, Venkatesh.A, Ramesh.R, Seenivasan. M , Sakthivel. K, A Fuzzy Log- Normal Distribution Model for the Rainfall level of Nmakkal District, Communications on Applied Nonlinear Analysis, Vol 31, No.6s (2024), pp.172-178.DOI: https://doi.org/10.52783/cana.v31.1176
[13]. S. Prakasam, Venkatesh. A, A Fuzzy Mathematical Model for the Parathyroid Hormone Secretion in Health Using LOG Gamma Distribution, Advances in Nonlinear Variational Inequalities, Vol 28, No.1s (2025), pp.470-478. DOI: https://doi.org/10.52783/anvi.v28.2447
[14]. Prakasam. S, Syamala. P, Venkatesh. A, Exploring the Mathematical Landscape of p-adic Numbers: Unveiling Uniqueness and Ostrowskis Theorem, Advances in Nonlinear Variational Inequalities, Vol 28, No.3s (2025), pp.93-108. DOI: https://doi.org/10.52783/anvi.v28.2852 [15]. R. Praveena, P.Gajendran, L. Jeyanthi, S. Prakasam, Khalil Al-Basyouni, K. Sudarmozhi, Fluid Flow Numerical Study Considering the Impact of Deborah Number and Slip Condition, Advances in Nonlinear Variational Inequalities, Vol 28, No. 5s (2025), pp.315-335. DOI: https://doi.org/10.52783/anvi.v28.3907Author: Dr. S. Prakasam
Dr. S. Prakasam is working as an Assistant Professor in A.V.V.M Sri Pushpam College (Autonomous). Thanjavur, Tamilnadu. He awarded Ph.D degree in Mathematics from the Bharathidasan University, Trichy, India. He has more than 15 years of teaching and research experience. He has published two International Books in Mathematics area. He has also published many research papers in National and International various UGC, Scopus and peer- reviewed journals. His areas of research are Mathematical modelling and fuzzy sets.