Rainfall probability analysis for Kerala (Record no. 195313)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 05671nam a22002057a 4500 |
| 082 ## - DEWEY DECIMAL CLASSIFICATION NUMBER | |
| Classification number | 630.31 |
| Item number | POO/RA PG |
| 100 ## - MAIN ENTRY--PERSONAL NAME | |
| Personal name | Pooja, A |
| 245 ## - TITLE STATEMENT | |
| Title | Rainfall probability analysis for Kerala |
| 260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT) | |
| Place of publication, distribution, etc | Vellanikkara |
| Name of publisher, distributor, etc | Department of Agricultural Statistics, College of Horticulture |
| Date of publication, distribution, etc | 2020 |
| 300 ## - PHYSICAL DESCRIPTION | |
| Extent | 110p. |
| 502 ## - DISSERTATION NOTE | |
| Dissertation note | MSc |
| 520 3# - SUMMARY, ETC. | |
| Abstract | The study entitled “Rainfall Probability Analysis for Kerala”, was conducted to<br/>estimate the probabilities and amounts of normal, excess and deficit rainfall during<br/>southwest and northeast monsoon periods, to determine the conditional probabilities for<br/>monsoon to be normal, excess and deficit when the monthly rainfall is normal, excess and<br/>deficit and to determine the assured monthly and weekly rainfall in the five agroclimatic<br/>zones of Kerala. Daily rainfall data from 1983 to 2019 collected from the five stations viz.<br/>Vellayani, Kumarakom, Vellanikkara, Pilicode and Ambalavayal representing southern<br/>zone, problem area zone, central zone, northern zone and high range zone respectively<br/>formed the database for the study.<br/>The daily rainfall data were converted to annual, seasonal, monthly and weekly<br/>rainfall data series for further analysis. Significant increasing trend is observed in annual<br/>rainfall at Vellayani. Non-significant increasing trend in annual rainfall is also observed<br/>at Vellanikkara, Pilicode and Ambalavayal. But, Kumarakom exhibited a non-significant<br/>negative trend for annual rainfall. Except the stations of Kumarakom and Vellanikkara,<br/>other stations have non-significant increasing trend in southwest monsoon rainfall. Only<br/>Vellayani has a non-significant increasing trend in northeast monsoon rainfall. All other<br/>stations exhibit declining trend for northeast monsoon rainfall over the period 1983-2019.<br/>The exploratory analysis showed that wide variation exists in rainfall over<br/>different agroclimatic zones. The rainfall variability was visually made possible by the<br/>use of box-and-whisker plots constructed for annual, seasonal, monthly and weekly<br/>rainfall over five stations. The boxplots explained the average and dispersion of rainfall<br/>data in terms of quartiles. In all the stations, annual, southwest monsoon and northeast<br/>monsoon rainfall did not follow normal distribution which was evident from the uneven<br/>boxes and dissimilar whisker lengths. A station-wise comparison showed that annual<br/>rainfall as well as southwest monsoon rainfall increased from south (Vellayani) to north<br/>(Pilicode) of Kerala and northeast monsoon rainfall declined from south to north. Outliers<br/>representing extreme rainfall events were also detected using boxplots which made the<br/>rainfall distribution skewed. At Ambalavayal, extreme annual rainfall (3093 mm) and<br/>extreme southwest monsoon rainfall (2380 mm) happened in 2018 and at Pilicode,<br/>extreme annual rainfall (4803 mm) occurred in 1994.The northeast monsoon witnessed<br/>extreme rainfall in 1992 (764 mm) and 2010 (950 mm), at Vellanikkara. The analysis of<br/>monthly rainfall using boxplots clearly depicted bimodal distribution at Vellayani and<br/>unimodal distribution at Pilicode. Thus, it was appropriate to use median and Inter<br/>Quartile Range (IQR) as the measures of central tendency and dispersion, rather than<br/>mean and standard deviation, as former measures were not affected by extreme<br/>observations.<br/>Conditional probabilities were estimated to determine whether the seasonal<br/>rainfall was excess, normal or deficient when monthly rainfall was excess, normal and<br/>deficient. Excess, normal and deficient rainfalls were defined in terms of quartiles for the<br/>purpose. At Vellayani, there was more than 50 per cent probability for the southwest<br/>monsoon to be in excess if the rainfall in the month of June was excess. At Kumarakom,<br/>there was a 60 per cent chance for receiving excess rainfall in southwest monsoon when<br/>July and September had excess rainfall. Rainfall in June and July determined excess<br/>rainfall in southwest monsoon at Vellanikkara with 70 per cent probability. There was<br/>70 per cent chance to receive excess rainfall during southwest monsoon at Pilicode when<br/>August or September received excess rainfall. Ambalavayal had experienced excess<br/>rainfall with 80 per cent possibility when July had excess rainfall. Similarly, each station<br/>had varying effects of rainfall in October and November towards northeast monsoon<br/>season. This analysis can provide information about when to take precautionary measures<br/>to anticipate the threat of floods and droughts in near future.<br/>The assured amounts of rainfall varied during different months and weeks in each<br/>station. Selection of crops (short duration varieties for low rainfall regions), cropping<br/>pattern and other decision making strategies for harvesting rainfall or drainage<br/>management can be made on the basis of assured rainfall in different months. At<br/>Vellayani, 23rd (4th June to 10th June) and 24th (11th June to 17th June) standard<br/>meteorological weeks (SMWs) are the rainiest weeks. The rainiest week is 28th SMW (9th<br/>July to 15th July) at Kumarakom and Ambalavayal, whereas, it is 24th SMW (11th June to<br/>17th June) at Vellanikkara and Pilicode. On farm operations and crop management plans<br/>like decision of times of sowing, irrigation, fertilizer application, harvesting, etc., could<br/>be executed on the basis of assured weekly rainfall during the different crop periods. |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name as entry element | Rainfall probability |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name as entry element | Agricultural Statistics |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name as entry element | Rainfall analysis |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name as entry element | Kerala |
| 700 ## - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Laly John, C (Guide) |
| 856 ## - ELECTRONIC LOCATION AND ACCESS | |
| Uniform Resource Identifier | https://krishikosh.egranth.ac.in/handle/1/5810225366 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Source of classification or shelving scheme | Dewey Decimal Classification |
| Item type | Theses |
| Not for loan | Collection code | Home library | Current library | Shelving location | Date acquired | Full call number | Barcode | Date last seen | Koha item type |
|---|---|---|---|---|---|---|---|---|---|
| Not For Loan | Reference Book | KAU Central Library, Thrissur | KAU Central Library, Thrissur | Theses | 01/12/2020 | 630.31 POO/RA PG | 174935 | 01/12/2020 | Theses |
