2021
DOI: 10.1002/joc.6973
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Interdecadal modulation of interannual ENSO‐Indian summer monsoon rainfall teleconnections in observations and CMIP6 models: Regional patterns

Abstract: This study examined the Inter‐decadal modulations of interannual El Niño‐Southern Oscillation (ENSO)‐Indian Summer Monsoon (ISM) rainfall regional teleconnection patterns in the observations and Coupled Model Intercomparison Project Phase 6 (CMIP6) models. Observations show strong epochal changes of the relationship between ENSO and all‐India summer rainfall (AISR) with weak teleconnections in epoch‐1 (centred around 1915) and epoch‐4 (recent epoch) and strong teleconnections in epoch‐2 (centred around 1940) a… Show more

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Cited by 27 publications
(38 citation statements)
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“…Recently, [9] observed that historically r τ fluctuated less in some parts of the Indian monsoon region and more in others (as seen in Fig. S1 (c,d)), alluding thereafter to "epochs" of weaker and stronger "ENSO-ISM teleconnection".…”
Section: Introductionmentioning
confidence: 88%
See 1 more Smart Citation
“…Recently, [9] observed that historically r τ fluctuated less in some parts of the Indian monsoon region and more in others (as seen in Fig. S1 (c,d)), alluding thereafter to "epochs" of weaker and stronger "ENSO-ISM teleconnection".…”
Section: Introductionmentioning
confidence: 88%
“…Most of the decadal variability of running window correlations, r τ , should therefore be due to "undersampling"; whereby a characteristic time scale of variability is an artifact of the analysis technique determined by the applied time window length, τ , being the sample size. Because of this undersampling of the true climatological correlation [6,7,8], r, we will refer to r τ as the apparent teleconnection strength.Recently, [9] observed that historically r τ fluctuated less in some parts of the Indian monsoon region and more in others (as seen in Fig. S1 (c,d)), alluding thereafter to "epochs" of weaker and stronger "ENSO-ISM teleconnection".…”
mentioning
confidence: 88%
“…Observation suggested that the regional Hadley circulation, via NAO in the northern hemisphere and IOD in the southern hemisphere, had roles in the change in ISM behavior (Roy and Collins, 2015). More recently, importance of western north Pacific low-level circulation influence on modulating ENSO-ISM teleconnections is highlighted (Mahendra et al, 2020;Ramu et al, 2020). Such features though well captured in the observation but shown missing in models (Roy and Kripalani, 2019b).…”
Section: Mechanisms: Role Of Natural Factorsmentioning
confidence: 99%
“…Separating models based on High Top or Low Top did not make much difference. Even many CMIP6 models are unable to represent the regional summer rainfall patterns over India associated with ENSO (Mahendra et al 2020).…”
Section: Ism-enso Teleconnectionmentioning
confidence: 99%
“…Studying these teleconnections could help in forecasting episodes of extreme precipitation or droughts. The Indian summer monsoon (from June to September) contributing to almost 75% of the country's annual rainfall, shows a considerable link with the El Niño‐Southern Oscillation (ENSO; Mahendra et al ., 2020). The warming of the central and eastern tropical Pacific ocean known as the El Niño phase of ENSO is associated with deficit monsoon rainfall, and the cooling phase (La Niña) brings excess rain (Roy et al ., 2019).…”
Section: Introductionmentioning
confidence: 99%