Recognition: unknown
Prediction and Predictability of the Wet-Season Rainfall over Southeast India
Pith reviewed 2026-05-10 16:20 UTC · model grok-4.3
The pith
Global tropical sea surface temperature patterns enable rainfall forecasts for southeast India up to ten months ahead.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
A global tropical SST climate network reveals high potential predictability for the October-December rainfall over Tamil Nadu, with significant forecast skill possible at lead times up to 10 months. This long-lead predictability stems from SST and rainfall interactions across the tropical Indo-Pacific and equatorial Atlantic regions. At zero lead time, predictability is dominated by North Indian Ocean SST anomalies. The study also identifies an overall increase in monthly rainfall and its variability linked to higher surface temperatures, water vapour, and moisture convergence, attributed to a long-term reduction in convective inhibition, plus an increasing trend in rainy season length due<f
What carries the argument
The global tropical SST climate network, which uses sea surface temperature anomalies and their interactions with rainfall across the tropical Indo-Pacific and equatorial Atlantic to generate long-lead predictions of Tamil Nadu wet-season rainfall.
If this is right
- Skillful seasonal forecasts for Tamil Nadu rainfall can be achieved using global tropical SST patterns at lead times up to 10 months.
- The data-driven methodology supports useful predictions even with the documented rise in rainfall variability.
- Local North Indian Ocean SST anomalies provide the main control on simultaneous (zero-lead) rainfall predictability.
- The length of the rainy season over southeast India is increasing because of earlier monsoon onset and later withdrawal.
- Excess rainfall trends result from long-term reduction in convective inhibition driven by warming and higher moisture.
Where Pith is reading between the lines
- Earlier forecasts could improve agricultural planning and water management decisions in Tamil Nadu by several months.
- The same network approach may apply to other sub-regions of the Indian monsoon that face similar increases in variability.
- Periodic retraining of the network on newer data would likely be needed to preserve skill as non-stationarity continues.
- Direct comparison of the network's predictions against observed rainfall in the most recent independent years would test persistence of the claimed skill.
Load-bearing premise
The observed statistical relationships between global tropical SST patterns and Tamil Nadu rainfall will persist and deliver real forecast skill even as rainfall variability increases and climate conditions become more non-stationary.
What would settle it
Applying the trained global tropical SST network to rainfall observations from years after the training period and checking whether skill at 10-month lead times remains statistically significant above simpler benchmarks or random chance.
read the original abstract
The challenge in predicting sub-regional climate within the Indian monsoon region is exacerbated by its increasing variability in a warming world. While exploring the seasonal predictability of rainfall over the state of Tamil Nadu in southeast India, we identify an overall increase in the monthly rainfall and its variability in recent years due to an increase in surface temperature, water vapour and moisture convergence. We attribute the increasing excess rainfall to a long-term reduction in convective inhibition. We further find an increasing trend in the length of the rainy season due to an earlier onset and a delayed withdrawal of the large-scale monsoon over the southeastern and southwestern regions of southern peninsular India, respectively. Further, the simultaneous (0- month lead) predictability of the primary wet-season (October-December, OND) rainfall over Tamil Nadu is dominated by sea surface temperature (SST) anomalies in the North Indian Ocean. However, a global tropical SST climate network reveals a high potential predictability and potential to realize significant forecast skill at a lead time of up to 10 months. The long-lead predictability arises from SST and rainfall interactions across the tropical Indo-Pacific and equatorial Atlantic regions. Our findings provide a robust data-driven methodology for skillful seasonal rainfall prediction over Tamil Nadu, despite the increasing rainfall variability.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript reports increasing monthly rainfall and variability over Tamil Nadu in recent decades, attributed to rising surface temperatures, water vapor, moisture convergence, and a long-term reduction in convective inhibition. It also documents an extended rainy season via earlier onset and delayed withdrawal. For predictability, simultaneous (0-month lead) OND rainfall is dominated by North Indian Ocean SST anomalies, while a global tropical SST climate network is said to reveal high potential predictability and realizable forecast skill at leads up to 10 months, arising from SST-rainfall interactions across the tropical Indo-Pacific and equatorial Atlantic. The work proposes a data-driven methodology for skillful seasonal prediction despite the noted variability.
Significance. If the central predictability claims hold after proper validation, the paper would offer a useful data-driven framework for long-lead regional rainfall forecasting in southeast India, an agriculturally critical area facing increasing variability. The mechanistic links to reduced convective inhibition and identification of key Indo-Pacific/Atlantic teleconnections provide physical insight into monsoon changes under warming. The emphasis on a global climate network approach is a constructive contribution that could be extended if methods are made transparent and reproducible.
major comments (2)
- [Abstract] Abstract: the headline claim of 'high potential predictability' and 'significant forecast skill' at up to 10-month leads from the global tropical SST climate network is load-bearing for the paper's contribution, yet the manuscript supplies no details on data periods analyzed, network construction (node selection, correlation thresholds, or community detection), statistical model employed, or validation (cross-validation, independent test periods, or skill metrics with error bars). Without these, it is impossible to determine whether reported skill exceeds persistence or is inflated by in-sample fitting.
- [Results] Results section on trends and predictability: the paper documents non-stationary behavior (increasing rainfall variability, earlier onset, delayed withdrawal) driven by thermodynamic changes, but provides no explicit tests of whether the underlying SST-rainfall relationships remain stable (e.g., split-sample correlations before/after trend onset, rolling-window analysis, or training on pre-1990 data and testing on later periods). This directly affects whether historical associations can be expected to deliver realizable long-lead skill.
minor comments (2)
- [Abstract] The abstract refers to 'data-driven methodology' without naming the precise statistical or network-based algorithm (e.g., whether linear regression, random forests, or graph-based prediction is used), which hinders immediate reproducibility.
- Figure captions and text should consistently report the exact years of the observational datasets (e.g., SST and rainfall records) and any detrending or filtering applied.
Simulated Author's Rebuttal
We thank the referee for their constructive and detailed review. The comments highlight important issues of methodological transparency and robustness that we address below. We have revised the manuscript to incorporate the requested details and tests.
read point-by-point responses
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Referee: [Abstract] Abstract: the headline claim of 'high potential predictability' and 'significant forecast skill' at up to 10-month leads from the global tropical SST climate network is load-bearing for the paper's contribution, yet the manuscript supplies no details on data periods analyzed, network construction (node selection, correlation thresholds, or community detection), statistical model employed, or validation (cross-validation, independent test periods, or skill metrics with error bars). Without these, it is impossible to determine whether reported skill exceeds persistence or is inflated by in-sample fitting.
Authors: We agree that the abstract and main text require greater explicitness on these elements to support the predictability claims and enable reproducibility. In the revised manuscript we expand the abstract to reference the key methodological choices and add a dedicated Methods subsection that specifies the data periods, network construction procedure (including node selection, correlation thresholds, and community detection), the statistical model, and the validation approach with skill metrics and uncertainty estimates. We also include direct comparisons to persistence forecasts. revision: yes
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Referee: [Results] Results section on trends and predictability: the paper documents non-stationary behavior (increasing rainfall variability, earlier onset, delayed withdrawal) driven by thermodynamic changes, but provides no explicit tests of whether the underlying SST-rainfall relationships remain stable (e.g., split-sample correlations before/after trend onset, rolling-window analysis, or training on pre-1990 data and testing on later periods). This directly affects whether historical associations can be expected to deliver realizable long-lead skill.
Authors: The referee correctly notes that non-stationarity could affect the reliability of long-lead predictions. Although the manuscript links trends to thermodynamic drivers, it does not include formal stability diagnostics. In the revision we add split-sample correlation analyses (pre- and post-1990), rolling-window correlations, and out-of-sample tests (training on earlier data and evaluating on later periods) to assess whether the key SST-rainfall teleconnections remain stable. These results will be presented in the Results section with accompanying figures. revision: yes
Circularity Check
No significant circularity; claims rest on data-driven network analysis without self-referential reduction shown
full rationale
The abstract presents the global tropical SST climate network as revealing long-lead predictability for Tamil Nadu OND rainfall based on observed SST-rainfall interactions across Indo-Pacific and Atlantic regions. No equations, fitting procedures, or self-citations are quoted that would reduce the claimed predictability or forecast skill to quantities fitted directly from the target data by construction. The paper separately documents non-stationary trends in rainfall and attributes them to physical changes, but these are presented as independent observations rather than load-bearing for the predictability claim. Without explicit reduction of the network-derived skill to the same historical inputs (e.g., via in-sample fitting without validation), the derivation chain remains self-contained and does not match any enumerated circularity pattern.
Axiom & Free-Parameter Ledger
axioms (1)
- domain assumption Sea surface temperature anomalies influence rainfall variability in the Indian monsoon region through moisture and circulation changes
Reference graph
Works this paper leans on
-
[1]
Journal of Earth System Science 120(5):795--805
Acharya N, Kar SC, Kulkarni MA, Mohanty UC, Sahoo LN (2011) Multi-model ensemble schemes for predicting northeast monsoon rainfall over peninsular India . Journal of Earth System Science 120(5):795--805. ://doi.org/10.1007/s12040-011-0111-4
-
[2]
SSRN preprint ://doi.org/10.2139/ssrn.6075477
Aswini MA, Rajkumar J, Janakiram R, Joshua Jacob Rajan Y, Jena BK, Ramakrishnan B (2024) High-Frequency Radar Observations during Cyclone Fengal along the Tamil Nadu Coast . SSRN preprint ://doi.org/10.2139/ssrn.6075477
-
[3]
Journal of Earth System Science 115(3):349--362
Balachandran S, Asokan R, Sridharan S (2006) Global surface temperature in relation to northeast monsoon rainfall over Tamil Nadu . Journal of Earth System Science 115(3):349--362. ://doi.org/10.1007/BF02702047
-
[4]
Boers N, Goswami B, Rheinwalt A, Bookhagen B, Hoskins B, Kurths J (2019) Complex networks reveal global pattern of extreme-rainfall teleconnections . Nature 566(7744):373--377. ://doi.org/10.1038/s41586-018-0872-x
-
[5]
Journal of Hydrology 624:129975
Chakra S, Ganguly A, Oza H, Padhya V, Pandey A, Deshpande RD (2023) Multidecadal summer monsoon rainfall trend reversals in South Peninsular India: A new approach to examining long-term rainfall dataset . Journal of Hydrology 624:129975. ://doi.org/10.1016/j.jhydrol.2023.129975
-
[6]
The CMS experiment at the CERN LHC
Chansaengkrachang K, Luadsong A, Aschariyaphotha N (2018) Vertically integrated moisture flux convergence over Southeast Asia and its relation to rainfall over Thailand . Pertanika Journal of Science & Technology 26(1):235--246. ://rbkm.kmutt.ac.th/xmlui//handle/123456789/1665
-
[7]
Science of The Total Environment 661:10--17
Chen CC, Wang YR, Guo YLL, Wang YC, Lu MM (2019) Short-term prediction of extremely hot days in summer due to climate change and ENSO and related attributable mortality . Science of The Total Environment 661:10--17. ://doi.org/10.1016/j.scitotenv.2019.01.168
-
[8]
Journal of Climate 33(6):2025--2050
Chen J, Dai A, Zhang Y, Rasmussen KL (2020) Changes in convective available potential energy and convective inhibition under global warming . Journal of Climate 33(6):2025--2050. ://doi.org/10.1175/JCLI-D-19-0461.1
-
[9]
Journal of Geophysical Research: Atmospheres 114(D10)
Dash SK, Kulkarni MA, Mohanty UC, Prasad K (2009) Changes in the characteristics of rain events in India . Journal of Geophysical Research: Atmospheres 114(D10). ://doi.org/10.1029/2008JD010572
-
[10]
Dash Y, Mishra SK, Panigrahi BK (2019) Predictability assessment of northeast monsoon rainfall in India using sea surface temperature anomaly through statistical and machine learning techniques . Environmetrics 30(4):e2533. ://doi.org/10.1002/env.2533
-
[11]
Hydrological Sciences Journal 67(9):1384--1396
Datta P, Das S (2022) Assessing the consistency of trends in Indian summer monsoon rainfall . Hydrological Sciences Journal 67(9):1384--1396. ://doi.org/10.1080/02626667.2022.2081507
-
[12]
De Deckker P (2016) The Indo-Pacific Warm Pool: Critical to world oceanography and world climate . Geoscience Letters 3(1):20. ://doi.org/10.1186/s40562-016-0054-3
-
[13]
Environmental Research Communications 7(2):021008
Dev R, Muraleedharan KR, Gireeshkumar TR, Shivaprasad S, Baliarsingh SK, Jayaprakash A, Nair TB (2025) Unravelling the mechanism of transient coastal upwelling in the southeastern Arabian Sea triggered by Cyclone Michaung . Environmental Research Communications 7(2):021008. ://doi.org/10.1088/2515-7620/ada96b
-
[14]
Dhar ON, Rakhecha PR (1983) Foreshadowing northeast monsoon rainfall over Tamil Nadu, India . Mon Wea Rev 111:109--112. https://doi.org/10.1175/1520-0493(1983)111
-
[15]
The European Physical Journal Special Topics 174(1):157--179
Donges JF, Zou Y, Marwan N, Kurths J (2009) Complex networks in climate dynamics: Comparing linear and nonlinear network construction methods . The European Physical Journal Special Topics 174(1):157--179. ://doi.org/10.1140/epjst/e2009-01098-2
-
[16]
Fan J, Meng J, Ludescher J, Chen X, Ashkenazy Y, Kurths J, Havlin S, Schellnhuber HJ (2021) Statistical physics approaches to the complex Earth system . Physics Reports 896:1--84. ://doi.org/10.1016/j.physrep.2020.09.005
-
[17]
Journal of Climate 35(3):1009--1020
Fan J, Meng J, Ludescher J, Li Z, Surovyatkina E, Chen X, Kurths J, Schellnhuber HJ (2022) Network-based approach and climate change benefits for forecasting the amount of Indian monsoon rainfall . Journal of Climate 35(3):1009--1020. ://doi.org/10.1175/JCLI-D-21-0063.1
-
[18]
Annual Review of Earth and Planetary Sciences 31(1):429--467
Gadgil S (2003) The Indian monsoon and its variability . Annual Review of Earth and Planetary Sciences 31(1):429--467. ://doi.org/10.1146/annurev.earth.31.100901.141251
-
[19]
Gadgil S, Rupa Kumar K (2006) The Asian monsoon—Agriculture and Economy . In: The Asian monsoon. Springer, p 651--683, ://doi.org/10.1007/3-540-37722-0_18
-
[20]
://www.jstor.org/stable/24110705
Gadgil S, Rajeevan M, Nanjundiah R (2005) Monsoon prediction--Why yet another failure? Current Science 88(9):1389--1400. ://www.jstor.org/stable/24110705
-
[21]
Hydrology and Earth System Sciences 26(16):4431--4446
Ghausi SA, Ghosh S, Kleidon A (2022) Breakdown in precipitation--temperature scaling over India predominantly explained by cloud-driven cooling . Hydrology and Earth System Sciences 26(16):4431--4446. ://doi.org/10.5194/hess-26-4431-2022
-
[22]
Goswami BN, Venugopal V, Sengupta D, Madhusoodanan MS, Xavier PK (2006) Increasing trend of extreme rain events over India in a warming environment . Science 314(5804):1442--1445. ://doi.org/10.1126/science.1132027
-
[23]
Hersbach H, Bell B, Berrisford P, Hirahara S, Hor \'a nyi A, Mu \ n oz-Sabater J, Nicolas J, Peubey C, Radu R, Schepers D, et al (2020) The ERA5 global reanalysis . Quarterly Journal of the Royal Meteorological Society 146(730):1999--2049. ://doi.org/10.1002/qj.3803
-
[24]
Journal of Climate 27(1):57--75
Hirahara S, Ishii M, Fukuda Y (2014) Centennial-scale sea surface temperature analysis and its uncertainty . Journal of Climate 27(1):57--75. ://doi.org/10.1175/JCLI-D-12-00837.1
-
[25]
Hoerl RW (2020) Ridge regression: A Historical context . Technometrics 62(4):420--425. ://doi.org/10.1080/00401706.2020.1742207
-
[26]
Meteorology and Atmospheric Physics 133(1):1--14
Hrudya PH, Varikoden H, Vishnu R (2021) A review on the Indian summer monsoon rainfall, variability and its association with ENSO and IOD . Meteorology and Atmospheric Physics 133(1):1--14. ://doi.org/10.1007/s00703-020-00734-5
-
[27]
Journal of the Geological Society of India 98(6):865--866
Kartheeshwari MR, Elango L (2022) 2021 Chennai floods—An Overview . Journal of the Geological Society of India 98(6):865--866. ://doi.org/10.1007/s12594-022-2079-x
-
[28]
Kothawale DR, Rajeevan M (2017) Monthly, Seasonal and Annual Rainfall Time Series for All India, Homogeneous Regions and Meteorological Subdivisions: 1871--2016 . Tech. Rep. RR-138, Indian Institute of Tropical Meteorology (IITM), ://www.tropmet.res.in/ lip/Publication/RR-pdf/RR-138.pdf, accessed 24 April 2026
2017
-
[29]
Krishnamurthy V, Shukla J (2000) Intraseasonal and interannual variability of rainfall over India . Journal of Climate 13(24):4366--4377. https://doi.org/10.1175/1520-0442(2000)013
-
[30]
Springer Nature, ://doi.org/10.1007/978-981-15-4327-2
Krishnan R, Sanjay J, Gnanaseelan C, Mujumdar M, Kulkarni A, Chakraborty S (2020) Assessment of climate change over the Indian region: A report of the ministry of earth sciences (MOES), government of India . Springer Nature, ://doi.org/10.1007/978-981-15-4327-2
-
[31]
Meteorological Applications 11(3):189--199
Kumar OB, Naidu CV, Rao SRL, Rao BRS (2004) Prediction of southern Indian winter monsoon rainfall from September local upper-air temperatures . Meteorological Applications 11(3):189--199. ://doi.org/10.1017/S1350482704001306
-
[32]
Human brain mapping 8(4):194--208
Lachaux JP, Rodriguez E, Martinerie J, Varela FJ (1999) Measuring phase synchrony in brain signals . Human brain mapping 8(4):194--208. https://doi.org/10.1002/(SICI)1097-0193(1999)8:4
-
[33]
Pure and Applied Geophysics 178(8):3207--3228
Lakshmi S, Nivethaa EAK, Ibrahim SNA, Ramachandran A, Palanivelu K (2021) Prediction of future extremes during the Northeast Monsoon in the coastal districts of Tamil Nadu State in India Based on ENSO . Pure and Applied Geophysics 178(8):3207--3228. ://doi.org/10.1007/s00024-021-02768-1
-
[34]
Geoscience Frontiers 6(6):817--823
Loo YY, Billa L, Singh A (2015) Effect of climate change on seasonal monsoon in Asia and its impact on the variability of monsoon rainfall in Southeast Asia . Geoscience Frontiers 6(6):817--823. ://doi.org/10.1016/j.gsf.2014.02.009
-
[35]
WIREs Computational Statistics1(1), 93– 100 (2009) https://doi.org/10.1002/wics.14
McDonald GC (2009) Ridge regression . Wiley Interdisciplinary Reviews: Computational Statistics 1(1):93--100. ://doi.org/10.1002/wics.14
-
[36]
Climate Dynamics 51(5):1609--1622
Misra V, Bhardwaj A, Mishra A (2018) Local onset and demise of the Indian summer monsoon . Climate Dynamics 51(5):1609--1622. ://doi.org/10.1007/s00382-017-3924-2
-
[37]
Pure and Applied Geophysics 170(11):1945--1967
Nair A, Acharya N, Singh A, Mohanty UC, Panda TC (2013) On the predictability of northeast monsoon rainfall over south peninsular India in general circulation models . Pure and Applied Geophysics 170(11):1945--1967. ://doi.org/10.1007/s00024-012-0633-y
-
[38]
Current Climate Change Reports 1(2):49--59
O’Gorman PA (2015) Precipitation extremes under climate change . Current Climate Change Reports 1(2):49--59. ://doi.org/10.1007/s40641-015-0009-3
-
[39]
Pai DS, Rajeevan M, Sreejith OP, Mukhopadhyay B, Satbha NS (2014) Development of a new high spatial resolution (0.25 0.25) long period (1901-2010) daily gridded rainfall data set over India and its comparison with existing data sets over the region . Mausam 65(1):1--18. ://doi.org/10.54302/mausam.v65i1.851
-
[40]
Pai DS, Arti B, Sunitha D, Madhuri M, Badwaik MR, Kundale AP, Sulochana G, Mohapatra M, Rajeevan M (2020) Normal dates of onset/progress and withdrawal of southwest monsoon over India . Mausam 71(4):553--570. ://doi.org/10.54302/mausam.v71i4.33
-
[41]
Climate Dynamics 53(1):371--387
Park JH, Li T, Yeh SW, Kim H (2019) Effect of recent Atlantic warming in strengthening Atlantic--Pacific teleconnection on interannual timescale via enhanced connection with the Pacific meridional mode . Climate Dynamics 53(1):371--387. ://doi.org/10.1007/s00382-018-4591-7
-
[42]
Proceedings of the Indian Academy of Sciences-Earth and Planetary Sciences 93(4):371--385
Parthasarathy B (1984) Interannual and long-term variability of Indian summer monsoon rainfall . Proceedings of the Indian Academy of Sciences-Earth and Planetary Sciences 93(4):371--385. ://doi.org/10.1007/BF02843255
-
[43]
arXiv preprint arXiv:250315148 ://doi.org/10.48550/arXiv.2503.15148
Patil Y, Chopra G, Tandon S, Goswami BN, Sujith RI (2025) Climatic Phase Transitions Unravel the Onset and Withdrawal of Indian Monsoon . arXiv preprint arXiv:250315148 ://doi.org/10.48550/arXiv.2503.15148
-
[44]
Physical Review Letters 64(8):821
Pecora LM, Carroll TL (1990) Synchronization in chaotic systems . Physical Review Letters 64(8):821. ://doi.org/10.1103/PhysRevLett.64.821
-
[45]
Theoretical and Applied Climatology 112(1):185--191
Prakash S, C M, Sathiyamoorthy V, Gairola RM (2013) Increasing trend of northeast monsoon rainfall over the equatorial Indian Ocean and peninsular India . Theoretical and Applied Climatology 112(1):185--191. ://doi.org/10.1007/s00704-012-0719-6
-
[46]
Groundwater for Sustainable Development 23:101007
Raja SKA, Panday DP, Kumar M (2023) Decoding the enigma of 100-year record-breaking rainfall over Tamil Nadu using wavelet analysis . Groundwater for Sustainable Development 23:101007. ://doi.org/10.1016/j.gsd.2023.101007
-
[47]
Physics and Chemistry of the Earth, Parts A/B/C 135:103642
Rajasekaran SKD, Radhakrishan S, Veeramalai G, Huang X, Ayyamperumal R (2024) Quantifying regional rainfall dynamics in southern India: Unravelling monsoon characteristics and intense precipitation using satellite and observed data records . Physics and Chemistry of the Earth, Parts A/B/C 135:103642. ://doi.org/10.1016/j.pce.2024.103642
-
[48]
Climate Dynamics 28(7):813--828
Rajeevan M, Pai DS, Anil Kumar R, Lal B (2007) New statistical models for long-range forecasting of southwest monsoon rainfall over India . Climate Dynamics 28(7):813--828. ://doi.org/10.1007/s00382-006-0197-6
-
[49]
Geophysical Research Letters 35(18)
Rajeevan M, Bhate J, Jaswal AK (2008) Analysis of variability and trends of extreme rainfall events over India using 104 years of gridded daily rainfall data . Geophysical Research Letters 35(18). ://doi.org/10.1029/2008GL035143
-
[50]
Meteorological Applications 19(2):226--236
Rajeevan M, Unnikrishnan CK, Bhate J, Niranjan Kumar K, Sreekala PP (2012) Northeast monsoon over India: Variability and Prediction . Meteorological Applications 19(2):226--236. ://doi.org/10.1002/met.1322
-
[51]
Rajkumar R, Shaijumon CS, Gopakumar B, Gopalakrishnan D (2020) Extreme rainfall and drought events in Tamil Nadu, India . Climate Research 80:175--188. ://doi.org/10.3354/cr01600
-
[52]
Communications Earth & Environment 6(1):417
Ran G, Meng J, Fan J (2025) Tropical monsoon rainfall can be predicted with lead times up to 10 months . Communications Earth & Environment 6(1):417. ://doi.org/10.1038/s43247-025-02391-1
-
[53]
Rao GN (1999) Variations of the SO relationship with summer and winter monsoon rainfall over India: 1872--1993 . Journal of Climate 12(12):3486--3495. https://doi.org/10.1175/1520-0442(1999)012
-
[54]
Rao PRK, Jagannathan P (1953) A study of the northeast monsoon rainfall of Tamilnadu . Mausam 4(1):22--44. ://doi.org/10.54302/mausam.v4i1.4775
-
[55]
Atmospheric Research 93(1-3):534--545
Riemann-Campe K, Fraedrich K, Lunkeit F (2009) Global climatology of convective available potential energy (CAPE) and convective inhibition (CIN) in ERA-40 reanalysis . Atmospheric Research 93(1-3):534--545. ://doi.org/10.1016/j.atmosres.2008.09.037
-
[56]
Physical Review Letters 76(11):1804
Rosenblum MG, Pikovsky AS, Kurths J (1996) Phase synchronization of chaotic oscillators . Physical Review Letters 76(11):1804. ://doi.org/10.1103/PhysRevLett.76.1804
-
[57]
Physical Review Letters 78(22):4193
Rosenblum MG, Pikovsky AS, Kurths J (1997) From phase to lag synchronization in coupled chaotic oscillators . Physical Review Letters 78(22):4193. ://doi.org/10.1103/PhysRevLett.78.4193
-
[58]
Nature Communications 8(1):1--11
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 . Nature Communications 8(1):1--11. ://doi.org/10.1038/s41467-017-00744-9
-
[59]
Journal of Advances in Modeling Earth Systems 8(1):96--120
Saha SK, Pokhrel S, Salunke K, Dhakate A, Chaudhari HS, Rahaman H, Sujith K, Hazra A, Sikka DR (2016) Potential predictability of Indian summer monsoon rainfall in NCEP CFSv2 . Journal of Advances in Modeling Earth Systems 8(1):96--120. ://doi.org/10.1002/2015MS000542
-
[60]
Climate Dynamics 61(1):831--848
Sengupta A, Vissa NK, Roy I (2023) Seasonal variations in the dynamic and thermodynamic response of precipitation extremes in the Indian subcontinent . Climate Dynamics 61(1):831--848. ://doi.org/10.1007/s00382-022-06613-6
-
[61]
Scientific Reports 13(1):22757
Shahi NK, Rai S (2023) An increase in widespread extreme precipitation events during the northeast monsoon season over south peninsular India . Scientific Reports 13(1):22757. ://doi.org/10.1038/s41598-023-50324-9
-
[62]
Sharma D, Das S, Saha SK, Goswami BN (2022) Mechanism for high “potential skill” of Indian summer monsoon rainfall prediction up to two years in advance . Quarterly Journal of the Royal Meteorological Society 148(749):3591--3603. ://doi.org/10.1002/qj.4375
-
[63]
International Journal of Climatology 43(11):5248--5268
Sharma D, Das S, Goswami BN (2023) Variability and predictability of the Northeast India summer monsoon rainfall . International Journal of Climatology 43(11):5248--5268. ://doi.org/10.1002/joc.8144
-
[64]
Quarterly Journal of the Royal Meteorological Society 152(774):e70023
Sharma D, Das S, Chakraborty D, Mitra A, Goswami BN (2026) Improving Indian summer monsoon rainfall prediction using deep learning up to two years in advance . Quarterly Journal of the Royal Meteorological Society 152(774):e70023. ://doi.org/10.1002/qj.70023
-
[65]
Theoretical and Applied Climatology 108:73--83
Sreekala PP, Rao SVB, Rajeevan M (2012) Northeast monsoon rainfall variability over south peninsular India and its teleconnections . Theoretical and Applied Climatology 108:73--83. ://doi.org/10.1007/s00704-011-0513-x
-
[66]
Climate Dynamics 51:3865--3882
Sreekala PP, Rao SVB, Rajeevan K, Arunachalam MS (2018) Combined effect of MJO, ENSO and IOD on the intraseasonal variability of northeast monsoon rainfall over south peninsular India . Climate Dynamics 51:3865--3882. ://doi.org/10.1007/s00382-018-4117-3
-
[67]
Reviews of Geophysics 56(1):79--107
Sun Q, Miao C, Duan Q, Ashouri H, Sorooshian S, Hsu KL (2018) A review of global precipitation data sets: Data sources, estimation, and intercomparisons . Reviews of Geophysics 56(1):79--107. ://doi.org/10.1002/2017RG000574
-
[68]
Hydrology and Earth System Sciences 25(6):3331--3350
Tarek M, Brissette F, Arsenault R (2021) Uncertainty of gridded precipitation and temperature reference datasets in climate change impact studies . Hydrology and Earth System Sciences 25(6):3331--3350. ://doi.org/10.5194/hess-25-3331-2021
-
[69]
Theoretical and Applied Climatology 151(1):859--870
Tiwari R, Mishra AK, Rai S, Pandey LK (2023) Evaluation and projection of northeast monsoon precipitation over India under higher warming scenario: a multimodel assessment of CMIP6 . Theoretical and Applied Climatology 151(1):859--870. ://doi.org/10.1007/s00704-022-04299-8
-
[70]
Climatic Change 42(1):327--339
Trenberth KE (1999) Conceptual framework for changes of extremes of the hydrological cycle with climate change . Climatic Change 42(1):327--339. ://doi.org/10.1023/A:1005488920935
-
[71]
Climate Research 47(1-2):123--138
Trenberth KE (2011) Changes in precipitation with climate change . Climate Research 47(1-2):123--138. ://doi.org/10.3354/cr00953
-
[72]
Bulletin of the American Meteorological Society 84(9):1205--1218
Trenberth KE, Dai A, Rasmussen RM, Parsons DB (2003) The Changing Character of Precipitation . Bulletin of the American Meteorological Society 84(9):1205--1218. ://doi.org/10.1175/BAMS-84-9-1205
-
[73]
Theoretical and Applied Climatology 127(3):993--1010
Varadan RJ, Kumar P, Jha GK, Pal S, Singh R (2017) An exploratory study on occurrence and impact of climate change on agriculture in Tamil Nadu, India . Theoretical and Applied Climatology 127(3):993--1010. ://doi.org/10.1007/s00704-015-1682-9
-
[74]
Nature Communications 6(1):7154
Wang B, Xiang B, Li J, Webster PJ, Rajeevan MN, Liu J, Ha KJ (2015) Rethinking Indian monsoon rainfall prediction in the context of recent global warming . Nature Communications 6(1):7154. ://doi.org/10.1038/ncomms8154
-
[75]
Journal of Climate 21(21):5545--5565
Wang H, Mehta VM (2008) Decadal variability of the Indo-Pacific warm pool and its association with atmospheric and oceanic variability in the NCEP--NCAR and SODA reanalyses . Journal of Climate 21(21):5545--5565. ://doi.org/10.1175/2008JCLI2049.1
-
[76]
Yadav RK (2012) Why is ENSO influencing Indian northeast monsoon in the recent decades? International Journal of Climatology 32(14). ://doi.org/10.1002/joc.2430
-
[77]
Bulletin of the American Meteorological Society 93(9):1401--1415
Yatagai A, Kamiguchi K, Arakawa O, Hamada A, Yasutomi N, Kitoh A (2012) APHRODITE: Constructing a long-term daily gridded precipitation dataset for Asia based on a dense network of rain gauges . Bulletin of the American Meteorological Society 93(9):1401--1415. ://doi.org/10.1175/BAMS-D-11-00122.1
-
[78]
Journal of Climate 19(8):1567--1575
Zubair L, Ropelewski CF (2006) The strengthening relationship between ENSO and northeast monsoon rainfall over Sri Lanka and southern India . Journal of Climate 19(8):1567--1575. ://doi.org/10.1175/JCLI3670.1
-
[79]
Geophysical Research Letters 30(18)
Goswami BN, Xavier PK (2003) Potential predictability and extended range prediction of Indian summer monsoon breaks . Geophysical Research Letters 30(18). ://doi.org/10.1029/2003GL017810
-
[80]
Theoretical and Applied Climatology 49(4):217--224
Parthasarathy B, Munot AA, Kothawale DR (1994) All-India monthly and seasonal rainfall series: 1871--1993 . Theoretical and Applied Climatology 49(4):217--224. ://doi.org/10.1007/BF00867461
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