ePrints@IIScePrints@IISc Home | About | Browse | Latest Additions | Advanced Search | Contact | Help

Multidecadal see-saw of the impact of ENSO on Indian and West African summer monsoon rainfall

Srivastava, Gaurav and Chakraborty, Arindam and Nanjundiah, Ravi S (2019) Multidecadal see-saw of the impact of ENSO on Indian and West African summer monsoon rainfall. In: CLIMATE DYNAMICS, 52 (11). pp. 6633-6649.

[img] PDF
Cli_Dyn_52-11_6633-6649_2019.pdf - Published Version
Restricted to Registered users only

Download (11MB) | Request a copy
Official URL: https://doi.org/10.1007/s00382-018-4535-2

Abstract

The strength of the simultaneous linear relationship between El Nino/Southern Oscillation (ENSO) and Indian summer monsoon (ISM) precipitation show strong variations on a decadal timescale. While some studies attribute this to shift in the state of the climate and consequent teleconnection pattern, some other argue this as natural variability between two random time series. In this study, we show that the relationship between West African Summer Monsoon (WASM) precipitation with ENSO also experiences decadal timescale oscillation. While the ENSO-ISM relationship weakened during the past seven decades, ENSO-WASM relationship strengthened to above the 95% significance level. We explain this multi-decadal see-saw of strong-weak impact of ENSO on ISM and WASM through a common mechanism. ENSO impacts ISM and WASM rainfall by modulating the upper tropospheric temperature of subtropical Africa and South Asia. While the impact of ENSO on this temperature anomaly was strong and concentrated over the northwest of Indian region before the 1980, the anomalies are spatially discontinuous and weak after 1980. Moreover, a westward shift of the center of this anomaly after 1980 help strengthen the ENSO-WASM relationship. We also show a dramatic change in the relationship between Atlantic Nino and ENSO before and after the 1980s. While before 1980 ENSO did not have much impact on Atlantic Nino index-3 (ATL3), after 1980 El Nino (La Nina) is coincidental with negative (positive) ATL3 index. Since a negative (positive) ATL3 reduce (enhance) WASM by increased south-westerly moisture flux, the ENSO-WASM relationship strengthens after 1980. Our study suggests that the decadal variations of ENSO-ISM and ENSO-WASM relationship is physically linked and possibly could not be due to pure noise in the time series.

Item Type: Journal Article
Publication: CLIMATE DYNAMICS
Publisher: SPRINGER
Additional Information: Copyright of this article belongs to SPRINGER
Keywords: El Nino/Southern oscillation; Indian summer monsoon; West African summer monsoon; Decadal variability
Department/Centre: Division of Mechanical Sciences > Divecha Centre for Climate Change
Division of Mechanical Sciences > Centre for Atmospheric & Oceanic Sciences
Date Deposited: 24 Jun 2019 18:35
Last Modified: 24 Jun 2019 18:35
URI: http://eprints.iisc.ac.in/id/eprint/63041

Actions (login required)

View Item View Item