Considerable rainfall occurs in India during the post-monsoon period from October to December, particularly over north-eastern, eastern and southern regions, and this is of great significance in agricultural and allied sectors. For the first time, we have attempted to provide detailed information on
Principal components of monsoon rainfall in normal, flood and drought years over India
β Scribed by Singh, C.V.
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 286 KB
- Volume
- 19
- Category
- Article
- ISSN
- 0899-8418
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β¦ Synopsis
Daily precipitation data of the monsoon season (June -September) for the period 1940 -1980 from 50 stations is considered in this study. The correlation of individual station rainfall with all India seasonal rainfall is carried out to identify the homogeneity associated with the nature of rainfall activity of individual stations with the rainfall character of the all India seasonal rainfall, taking into account statistical significance. Further, empirical orthogonal function (EOF) analysis is carried out on these data to find out the nature of rainfall distribution in different monsoon categories, namely normal, flood and drought years. The percentages of variance explained in these different categories for normal, flood and drought years are estimated. The technique thus serves to identity spatial and temporal pattern characteristics of possible physical significance.
It has been found that during normal, flood and drought years, the first four (most dominated) principal component with 'significantly positive' correlated stations explains 73%, 77% and 100% of the variance, while the remainder 'weakly correlated' stations explains 58%, 66% and 52% of the variance with all India seasonal mean rainfall.
π SIMILAR VOLUMES
A comparative study has been conducted of the diurnal variations of 3-hourly rainfall for Niamey, located in Niger, in the West African Sahel among four extreme precipitation periods: the wet periods of the 1950s and late 1980s to early 1990s versus the drought periods of the early 1970s and 1980s.
## Abstract The frequency and intensity of meteorological droughts over the IndoβGangetic Region (IGR) of India pertaining to the rice crop during kharif season (June to July to October to November) and the wheat crop during the rabi season (November to December to March) were assessed using the st