Abstract
The Indian subcontinent, due to its enormous variety of geographical features, is associated with inhomogeneity. Hence, in the present study, we have classified the whole Indian subcontinent into four homogeneous regions, such as North India, Central India, South India, and Northeast India, based on the similarity in rainfall characteristics and associations with the regional/global circulation parameters. These four major homogeneous regions have quite different climatological distribution rainfall as well as the degree of variability, depicting the need of individual exploration of them. The rainfall indices are prepared for an extended period of 120 years from 1901 to 2020 to understand the interannual variability of it over these homogeneous regions. The changes in the temporal trend with time are explored by diving the whole time period into four periods of 30 years each, i.e., 1901–1930 (Period 1), 1931–1960 (Period 2), 1961–1990 (Period 3), and 1991–2020 (Period 4). During period 4, a declining trend is seen over North India while other three regions show an increasing trend. Also, the wavelet analysis is carried out to see the periodicity of rainfall pattern and found that the interannual variability is more during the postindustrial period due to the lack of any dominant periodicity. And, finally, we investigated the teleconnection patterns during these four defined periods for all the homogeneous regions with global sea surface temperature where we get the ENSO monsoon relation is weaker during the recent period for all the regions except north India, explaining the reason behind the drying trend over there.
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Data availability
The datasets used in the present study are freely available: (i) IMD gridded rainfall dataset from http://www.imdpune.gov.in/Clim_Pred_LRF_New/Grided_Data_Download.html (Pai et al. 2015). (ii) The ERSST SST dataset from data https://psl.noaa.gov/data/gridded/data.noaa.ersst.v5.html. (iii) Rainfall indices constructed by Parthasarathy et al. (1994) is obtained from Indian Institute of Tropical Meteorology, Pune (IITM, Pune; https://tropmet.res.in) website.
Code availability
Scripts and programming used for the analysis in the current study are available from the corresponding author upon reasonable request.
References
Borah P, Venugopal V, Sukhatme J, Muddebihal P, Goswami B (2020) Indian monsoon derailed by a north atlantic wavetrain. Science 370(6522):1335–1338
Ding Q, Wang B (2009) Predicting extreme phases of the indian summer monsoon. J Clim 22(2):346–363
Goswami BN, Wu G, Yasunari T (2006) The annual cycle, intraseasonal oscillations, and roadblock to seasonal predictability of the asian summer monsoon. J Clim 19(20):5078–5099
Goswami B and Chakravorty S (2017) Dynamics of the indian summer monsoon climate. Oxford Res Encycl Clim Sci
Huang B, Banzon VF, Freeman E, Lawrimore J, Liu W, Peterson TC, Smith TM, Thorne PW, Woodruff SD, Zhang H-M (2015) Extended reconstructed sea surface temperature version 4 (ersst. v4). part i: Upgrades and intercomparisons. J Clim 28(3):911–930
Huang B, Thorne PW, Banzon VF, Boyer T, Chepurin G, Lawrimore JH, Menne MJ, Smith TM, Vose RS, Zhang H-M (2017) Extended reconstructed sea surface temperature, version 5 (ersstv5): upgrades, validations, and intercomparisons. J Clim 30(20):8179–8205
Huang B, Thorne PW, Smith TM, Liu W, Lawrimore J, Banzon VF, Zhang H-M, Peterson TC, Menne M (2016) Further exploring and quantifying uncertainties for extended reconstructed sea surface temperature (ersst) version 4 (v4). J Clim 29(9):3119–3142
Krishnamurthy V, Goswami BN (2000) Indian monsoon–enso relationship on inter-decadal timescale. J Clim 13(3):579–595
Kulkarni A (2012) Weakening of indian summer monsoon rainfall in warming environment. Theoret Appl Climatol 109(3):447–459
Kulkarni J (2000) Wavelet analysis of the association between the southern oscillation and the indian summer monsoon. IJOC, A Journal of RMet Society 20(1):89–104
Kumar PK, Singh A (2021) Increase in summer monsoon rainfall over the northeast india during el niño years since 1600. Clim Dyn 57(3):851–863
Liu W, Huang B, Thorne PW, Banzon VF, Zhang H-M, Freeman E, Lawrimore J, Peterson TC, Smith TM, Woodruff SD (2015) Extended reconstructed sea surface temperature version 4 (ersst. v4): Part ii. parametric and structural uncertainty estimations. J Clim 28(3):931–951
Pai D, Sridhar L, Badwaik M, Rajeevan M (2015) Analysis of the daily rainfall events over india using a new long period (1901–2010) high resolution (0.25× 0.25) gridded rainfall data set. Clim Dyn 45(3):755–776
Parthasarathy B, Kumar KR, Munot A (1993) Homogeneous indian monsoon rainfall: variability and prediction. Proc Indian Acad Sci-Earth Planet Sci 102(1):121–155
Parthasarathy B, Munot A, Kothawale D (1994) All-india monthly and seasonal rainfall series: 1871–1993. Theoret Appl Climatol 49(4):217–224
Prabhu A, Oh J, Kim I-W, Kripalani R, Mitra A, Pandithurai G (2017) Summer mon-soon rainfall variability over north east regions of india and its association with eurasian snow, atlantic sea surface temperature and arctic oscillation. Clim Dyn 49(7):2545–2556
Preethi B, Mujumdar M, Kripalani R, Prabhu A, Krishnan R (2017) Recent trends and tele-connections among south and east asian summer monsoons in a warming environment. Clim Dyn 48(7–8):2489–2505
Rajeevan M, Guhathakurta P, Thapliyal V (2000) New models for long range forecasts of summer monsoon rainfall over north west and peninsular india. Meteorol Atmos Phys 73(3):211–225
Reshma T, Varikoden H, Babu C (2021) Observed changes in Indian summer monsoon rainfall at different intensity bins during the past 118 years over five homogeneous regions. Pure Appl Geophys 178(9):3655–3672
Roxy MK, Ghosh S, Pathak A, Athulya R, Mujumdar M, Murtugudde R, Terray P, Rajeevan M (2017) A threefold rise in widespread extreme rain events over central india. Nat Commun 8(1):1–11
Saha SK, Halder S, Suryachandra Rao A and Goswami B (2012) Modulation of isos by land-atmosphere feedback and contribution to the interannual variability of indian summer monsoon. J Geophys Res: Atmos 117(D13)
Sahoo M and Yadav RK (2021a) Role of equatorial central pacific sea surface temperature in modulating rainfall over north india during indian summer monsoon. Int J Climatol
Sahoo M, Yadav RK (2021) Teleconnection of atlantic nino with summer monsoon rainfall over northeast india. Global Planet Chang 203:103550
Suhas E, Neena J, Goswami B (2012) Interannual variability of indian summer monsoon arising from interactions between seasonal mean and intraseasonal oscillations. J Atmos Sci 69(6):1761–1774
Torrence C, Compo GP (1998) A practical guide to wavelet analysis. Bull Amer Meteor 79(1):61–78
Webster PJ, Magana VO, Palmer T, Shukla J, Tomas R, Yanai M, Yasunari T (1998) Monsoons: Processes, predictability, and the prospects for prediction. JGR Ocean 103(C7):14451–14510
Yadav RK (2016) On the relationship between iran surface temperature and northwest india summer monsoon rainfall. Int J Climatol 36(13):4425–4438
Yadav RK (2021) Relationship between azores high and indian summer monsoon. NPJ Clim Atmos Sci 4(1):1–9
Yadav RK, Roxy MK (2019) On the relationship between north india summer monsoon rainfall and east equatorial indian ocean warming. Global Planet Change 179:23–32
Yadav RK, Srinivas G, Chowdary JS (2018) Atlantic niño modulation of the indian summer monsoon through asian jet. NPJ Clim Atmos Sci 1(1):1–11
Yadav RK, Wang S-YS, Wu C-H, Gillies RR (2020) Swapping of the pacific and atlantic niño influences on north central india summer monsoon. Clim Dyn 54(9):4005–4020
Yadav R (2009a) Changes in the large-scale features associated with the indian summer monsoon in the recent decades. IJOC, A Journal of RMet Society 29(1):117–133
Yadav R (2009b) Role of equatorial central pacific and northwest of north atlantic 2-metre surface temperatures in modulating indian summer monsoon variability. Clim Dyn 32(4):549–563
Acknowledgements
The authors acknowledge anonymous reviewers for their constructive comments and recommendations on ways of improving the manuscript. We are grateful to the Director, Indian Institute of Tropical Meteorology (IITM), and Ministry of Earth Sciences (MoES) for providing the necessary facilities to carry out this study. The authors thank the Pratyush High Power Computing Centre (HPC) staff in IITM, Pune, India, for providing computer resources. We acknowledge all the data sources. MS is thankful to IITM for the research fellowship. The graphical analyses for this study have been done using Python.
Funding
This research is a part of a PhD work of MS carried out at Indian Institute of Tropical Meteorology (IITM) and did not receive any specific grant from any funding agencies.
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MS and RKY have conceived the idea of the study. MS has performed the analysis. The initial draft of the manuscript was written by MS and RKY has contributed towards improving the manuscript with his valuable suggestions.
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Sahoo, M., Kumar Yadav, R. The Interannual variability of rainfall over homogeneous regions of Indian summer monsoon. Theor Appl Climatol 148, 1303–1316 (2022). https://doi.org/10.1007/s00704-022-03978-w
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DOI: https://doi.org/10.1007/s00704-022-03978-w