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

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 a...

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Autores principales: Azad, Sarita, Rajeevan, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4738276/
https://www.ncbi.nlm.nih.gov/pubmed/26837459
http://dx.doi.org/10.1038/srep20145
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author Azad, Sarita
Rajeevan, M.
author_facet Azad, Sarita
Rajeevan, M.
author_sort Azad, Sarita
collection PubMed
description 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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spelling pubmed-47382762016-02-09 Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming Azad, Sarita Rajeevan, M. Sci Rep Article 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. Nature Publishing Group 2016-02-03 /pmc/articles/PMC4738276/ /pubmed/26837459 http://dx.doi.org/10.1038/srep20145 Text en Copyright © 2016, Macmillan Publishers Limited http://creativecommons.org/licenses/by/4.0/ This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/
spellingShingle Article
Azad, Sarita
Rajeevan, M.
Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming
title Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming
title_full Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming
title_fullStr Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming
title_full_unstemmed Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming
title_short Possible shift in the ENSO-Indian monsoon rainfall relationship under future global warming
title_sort possible shift in the enso-indian monsoon rainfall relationship under future global warming
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4738276/
https://www.ncbi.nlm.nih.gov/pubmed/26837459
http://dx.doi.org/10.1038/srep20145
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