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. 2016 Feb 3:6:20145.
doi: 10.1038/srep20145.

Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming

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Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming

Sarita Azad et al. Sci Rep. .

Abstract

EI Nino-Southern Oscillation (ENSO) and Indian monsoon rainfall are known to have an inverse relationship, which we have observed in the rainfall spectrum exhibiting a spectral dip in 3-5 y period band. It is well documented that El Nino events are known to be associated with deficit rainfall. Our analysis reveals that this spectral dip (3-5 y) is likely to shift to shorter periods (2.5-3 y) in future, suggesting a possible shift in the relationship between ENSO and monsoon rainfall. Spectral analysis of future climate projections by 20 Coupled Model Intercomparison project 5 (CMIP5) models are employed in order to corroborate our findings. Change in spectral dip speculates early occurrence of drought events in future due to multiple factors of global warming.

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Figures

Figure 1
Figure 1. PSD of seven sub-divisional rainfall of SHR7 region and ISMR (inset) demonstrating spectral dip in the 3–5 y period band.
India’s map is created using shape file which is available at survey of India website www.surveyofindia.gov.in.
Figure 2
Figure 2. Inverse relation between ENSO-SHR7 rainfall in observed spectra during the time period 1871–2005.
Figure 3
Figure 3. PSD of SHR7 rainfall from 20 CMIP5 models (red) against observations (blue).
The eight models whose spectra match well with the observed are marked in circle.
Figure 4
Figure 4. PSD of projected SHR7 rainfall from 20 CMIP5 models.
The five models which show shift in the spectral dip are marked in circle.
Figure 5
Figure 5. PSD of (a) observed; (b) model IPSL-CM5A; and (c) comparison of SHR7 rainfall and ISMR projected.
Figure 6
Figure 6. Projected changes in Nino 3 SST by model GFDL-CM3.

References

    1. Walker G. T. & Bliss E. W. World weather V, Mem. R. Meteorol. Soc. 4, 53–84 (1932).
    1. Rajeevan M. & McPhaden M. J. Tropical Pacific upper ocean heat content variations and Indian summer monsoon rainfall. Geophys. Res. Lett. 31, L18203, 10.1029/2004GL020631 (2004). - DOI
    1. Sikka D. R. Some aspects of the large scale fluctuations of summer monsoon rainfall over India in relation to fluctuations in the planetary and regional scale circulation parameters. Proc. Indian Acad. Sci. Earth Planet Sci. 89, 179–195 (1980).
    1. Kripalani R. H. & Kulkarni A. Climatic impact of El NiAo/La Niiia on the Indian monsoon: A new perspective, Weather 52(2), 39–46 (1997).
    1. Bhattacharyya S. & Narasimha R. Regional differentiation in multidecadal connections between Indian monsoon rainfall and solar activity. J. Geophys. Res. 112, 10.1029/2006JD008353,D24103 (2007). - DOI

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