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Rainfall Trend Analysis in The Lower Gangetic Plain: A Study on Selected Rainfall Stations of Maldah District, West Bengal, India


Affiliations
1 Department of Geography, University of Kalyani, Nadia 741 235, India
 

Changes in rainfall pattern are of significance in terms of water resource management, hydrological modelling, environmental hazard management and agricultural planning. In the present study I assess the annual and seasonal rainfall trend, including concentration in eight rainfall stations in Maldah district, located in the lower Gangetic plain of West Bengal, India during 1985–2015. Besides the Mann–Kendall test and Theil–Sen’s estimator for assessing the trend of rainfall, precipitation concentration index (PCI) has been used to examine intra-annual rainfall variability. The study reveals decreasing trend of annual and monsoon rainfall in seven rainfall stations. Among them, significant trend is found in five and four rainfall stations respectively. This is followed by pre-monsoon and post-monsoon rainfall characterized with decreasing trend in five and eight rainfall stations respectively. The results of PCI show fluctuation of rainfall distribution in the district from moderate to strong irregular during the study period. However, decreasing trend of annual PCI values in the seven rainfall stations, with significant value in one of them, implies a tendency towards moderate rainfall distribution in the respective stations. Nevertheless, Chanchal- I rainfall station solely showed increasing annual PCI value and thereby an affinity towards strong irregular distribution of rainfall. Despite decrease in annual and seasonal rainfall, increase of pre-June (May) and post-September (October) rainfall prolonged the rainy season, which is responsible for drainage congestion as well as seasonal inundation in low-lying areas of the district.

Keywords

Precipitation Concentration Index, Rainfall Stations, Trend Analysis, Water Resource Management.
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  • Parthasarathy, B., Interannual and long-term variability of Indian summer monsoon rainfall. Proc. Indian Acad. Sci – Earth Planet. Sci., 1984, 93(4), 371–385.
  • Das, P. K., Chakraborty, A. and Seshasai M. V. R., Spatial analysis of temporal trend of rainfall and rainy days during the Indian summer monsoon season using daily gridded (0.5 × 0.5) rainfall data for the period of 1971–2005. Meteorol. Appl., 2014, 21(3), 481–493.
  • May, W., Simulation of the variability and extremes of daily rainfall during the Indian summer monsoon for present and future times in a global time-slice experiment. Climate Dyn., 2004, 22(2– 3), 183–204.
  • Pattanaik, D. R. and Rajeevan, M., Variability of extreme rainfall events over India during southwest monsoon season. Meteorol. Appl., 2010, 17(1), 88–104.
  • Huang, J., Sun, S., Xue, Y. and Zhang, J., Changing characteristics of precipitation during 1960–2012 in Inner Mongolia, northern China. Meteorol. Atmos. Phys., 2015, 127(3), 257–271.
  • Ghosh, S., Luniya, V. and Gupta, A., Trend analysis of Indian summer monsoon rainfall at different spatial scales. Atmos. Sci. Lett., 2009, 10, 285–290.
  • Census of India, District Census Handbook: Maldah, Village and Town wise Primary Census Abstract (PCA), Series 20, Part XII-B, Directorate of Census Operations, Government of West Bengal, 2011.
  • Tandon, S. K., Sinha, R., Gibling, M. R., Dasgupta, A. S. and Ghazanfari, P., Late Quaternary evolution of the Ganga Plains: myths and misconceptions, recent developments and future directions. Golden Jubilee Mem. Geol. Soc. India, 2008, 66, 259–299.
  • Sengupta, J. C., West Bengal District Gazetteers: Malda, Director, District Gazetteers, Government of West Bengal Press, Calcutta, 1969.
  • Oliver, J. E., Monthly precipitation distribution: a comparative index. Prof. Geogr., 1980, 32(3), 300–309.
  • Luis, M. D., González-Hidalgo, J. C., Brunetti, M. and Longares, L. A., Precipitation concentration changes in Spain 1946–2005. Nat. Hazards Earth Syst. Sci., 2011, 11(5), 1259–1265.
  • Mann, H. B., Nonparametric tests against trend. Econometrica: J. Econ. Soc., 1945, 13, 245–259.
  • Kendall, M., Rank Correlation Methods, Charles Griffin. San Francisco, CA, USA, 4th edn, 1975.
  • Liuzzo, L., Bono, E., Sammartano, V. and Freni, G., Analysis of spatial and temporal rainfall trends in Sicily during the 1921–2012 period. Theor. Appl. Climatol., 2016, 126(1–2), 113–129.
  • Salmi, T., Määttä, A., Anttila, P., Ruoho-Airola, T. and Amnell, T., Detecting trends of annual values of atmospheric pollutants by the Mann–Kendall test and Sen’s slope estimates – the Excel template application MAKESENS. In Publications on Air Quality No. 31, Finnish Meteorological Institute, Helsinki, Finland, 2002.
  • Theil, H., A rank invariant method of linear and polynomial regression analysis, Part 3. Netherlands, Akademie van Wettenschappen, Proceedings, 1950, 53, 1397–1412.
  • Sen, P. K., Estimates of the regression coefficient based on Kendall’s tau. J. Am. Stat. Assoc., 1968, 63(324), 1379–1389.
  • Tabari, H., Talaee, P. H., Ezani, A. and Some’e, B. S., Shift changes and monotonic trends in autocorrelated temperature series over Iran. Theor. Appl. Climatol., 2011, 109(1–2), 95–108.
  • Dinpashoh, Y., Jhajharia, D., Fakheri-Fard, A., Singh, V. P. and Kahya, E., Trends in reference crop evapotranspiration over Iran. J. Hydrol., 2011, 399(3), 422–433.
  • Von Storch, H., Misuses of statistical analysis in climate research. In Analysis of Climate Variability: Applications of Statistical Techniques (eds Storch, H. V. and Navarra, A.), Springer, Berlin, Germany, 1995, pp. 11–26.
  • Tabari, H. and Talaee, P. H., Analysis of trends in temperature data in arid and semi-arid regions of Iran. Global Planet. Change, 2011, 79(1), 1–10.
  • Rivard, C. and Vigneault, H., Trend detection in hydrological series: when series are negatively correlated. Hydrol. Process., 2009, 23(19), 2737–2743.
  • Yue, S., Pilon, P., Phinney, B. and Cavadias, G., The influence of autocorrelation on the ability to detect trend in hydrological series. Hydrol. Process., 2002, 16(9), 1807–1829.
  • Durbin, J. and Watson, G. S., Testing for serial correlation in least squares regression. I. Biometrika, 1950, 37(3/4), 409–428.
  • Durbin, J. and Watson, G. S., Testing for serial correlation in least squares regression. II. Biometrika, 1951, 38(1/2), 159–177.
  • Durbin, J. and Watson, G. S., Testing for serial correlation in least squares regression. III. Biometrika, 1971, 58(1), 1–19.
  • Naidu, C. V., Durgalakshmi, K., Krishna, K. M., Rao, S. R., Satyanarayana, G. C., Lakshminarayana, P. and Rao, L. M., Is summer monsoon rainfall decreasing over India in the global warming era? J. Geophys. Res., 2009, 114(D24), 1–16.
  • Malik, N., Bookhagen, B. and Mucha, P. J., Spatiotemporal patterns and trends of Indian monsoonal rainfall extremes. Geophys. Res. Lett., 2016, 43(4), 1710–1717.
  • Paul, S., Ghosh, S., Oglesby, R., Pathak, A., Chandrasekharan, A. and Ramsankaran, R. A. A. J., Weakening of Indian summer monsoon rainfall due to changes in land use land cover. Sci. Rep., 2016, 6, 32177; doi:10.1038/srep32177.

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  • Rainfall Trend Analysis in The Lower Gangetic Plain: A Study on Selected Rainfall Stations of Maldah District, West Bengal, India

Abstract Views: 149  |  PDF Views: 62

Authors

Suman Kumar Kundu
Department of Geography, University of Kalyani, Nadia 741 235, India

Abstract


Changes in rainfall pattern are of significance in terms of water resource management, hydrological modelling, environmental hazard management and agricultural planning. In the present study I assess the annual and seasonal rainfall trend, including concentration in eight rainfall stations in Maldah district, located in the lower Gangetic plain of West Bengal, India during 1985–2015. Besides the Mann–Kendall test and Theil–Sen’s estimator for assessing the trend of rainfall, precipitation concentration index (PCI) has been used to examine intra-annual rainfall variability. The study reveals decreasing trend of annual and monsoon rainfall in seven rainfall stations. Among them, significant trend is found in five and four rainfall stations respectively. This is followed by pre-monsoon and post-monsoon rainfall characterized with decreasing trend in five and eight rainfall stations respectively. The results of PCI show fluctuation of rainfall distribution in the district from moderate to strong irregular during the study period. However, decreasing trend of annual PCI values in the seven rainfall stations, with significant value in one of them, implies a tendency towards moderate rainfall distribution in the respective stations. Nevertheless, Chanchal- I rainfall station solely showed increasing annual PCI value and thereby an affinity towards strong irregular distribution of rainfall. Despite decrease in annual and seasonal rainfall, increase of pre-June (May) and post-September (October) rainfall prolonged the rainy season, which is responsible for drainage congestion as well as seasonal inundation in low-lying areas of the district.

Keywords


Precipitation Concentration Index, Rainfall Stations, Trend Analysis, Water Resource Management.

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DOI: https://doi.org/10.18520/cs%2Fv119%2Fi6%2F1031-1038