Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000

Summary: El Niño–Southern Oscillation (ENSO) was identified as the dominant predictor for the Indian summer monsoon rainfall (ISMR) in the early 1900s. An apparent weakening of the ENSO–ISMR relationship has been observed since the 1970s. Here, we found a clear restoration of the ENSO–ISMR relations...

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Published in:The Innovation
Main Authors: Xianke Yang, Ping Huang
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2021
Subjects:
Online Access:https://doi.org/10.1016/j.xinn.2021.100102
https://doaj.org/article/aae3f2b7d1ae486c8f7223039dbfa6f6
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spelling ftdoajarticles:oai:doaj.org/article:aae3f2b7d1ae486c8f7223039dbfa6f6 2023-05-15T17:34:01+02:00 Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000 Xianke Yang Ping Huang 2021-05-01T00:00:00Z https://doi.org/10.1016/j.xinn.2021.100102 https://doaj.org/article/aae3f2b7d1ae486c8f7223039dbfa6f6 EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S2666675821000278 https://doaj.org/toc/2666-6758 2666-6758 doi:10.1016/j.xinn.2021.100102 https://doaj.org/article/aae3f2b7d1ae486c8f7223039dbfa6f6 The Innovation, Vol 2, Iss 2, Pp 100102- (2021) ENSO–ISMR relationship interdecadal transition tropical Atlantic SSTAs emerging ENSOs continuing ENSOs Science (General) Q1-390 article 2021 ftdoajarticles https://doi.org/10.1016/j.xinn.2021.100102 2022-12-31T06:41:59Z Summary: El Niño–Southern Oscillation (ENSO) was identified as the dominant predictor for the Indian summer monsoon rainfall (ISMR) in the early 1900s. An apparent weakening of the ENSO–ISMR relationship has been observed since the 1970s. Here, we found a clear restoration of the ENSO–ISMR relationship since 1999/2000. This restoring relationship is closely linked to the interdecadal transition of ENSO evolution and the associated sea surface temperature anomalies (SSTAs) over the tropical Atlantic. During 1979–1997, summer ENSO events mainly continued from the previous winter, which can drive apparent Atlantic Niña SSTAs to offset ENSO's impact on ISMR and weaken the ENSO–ISMR relationship. In contrast, when ENSO events newly emerge from late spring, as they have done more recently during 2000–2018, the associated tropical Atlantic SSTAs are weak and shift to the tropical North Atlantic, which can offset the contribution of Atlantic Niña and reinforce the ENSO–ISMR relationship. We identified that the diversity of ENSO's evolution, continuing from the previous winter or emerging from late spring, is the dominant factor perturbing the ENSO–ISMR relationship in recent epochs, with tropical Atlantic SSTAs as the crucial bridge. This finding should be considered in our efforts to improve ISMR prediction. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Indian The Innovation 2 2 100102
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ENSO–ISMR relationship
interdecadal transition
tropical Atlantic SSTAs
emerging ENSOs
continuing ENSOs
Science (General)
Q1-390
spellingShingle ENSO–ISMR relationship
interdecadal transition
tropical Atlantic SSTAs
emerging ENSOs
continuing ENSOs
Science (General)
Q1-390
Xianke Yang
Ping Huang
Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000
topic_facet ENSO–ISMR relationship
interdecadal transition
tropical Atlantic SSTAs
emerging ENSOs
continuing ENSOs
Science (General)
Q1-390
description Summary: El Niño–Southern Oscillation (ENSO) was identified as the dominant predictor for the Indian summer monsoon rainfall (ISMR) in the early 1900s. An apparent weakening of the ENSO–ISMR relationship has been observed since the 1970s. Here, we found a clear restoration of the ENSO–ISMR relationship since 1999/2000. This restoring relationship is closely linked to the interdecadal transition of ENSO evolution and the associated sea surface temperature anomalies (SSTAs) over the tropical Atlantic. During 1979–1997, summer ENSO events mainly continued from the previous winter, which can drive apparent Atlantic Niña SSTAs to offset ENSO's impact on ISMR and weaken the ENSO–ISMR relationship. In contrast, when ENSO events newly emerge from late spring, as they have done more recently during 2000–2018, the associated tropical Atlantic SSTAs are weak and shift to the tropical North Atlantic, which can offset the contribution of Atlantic Niña and reinforce the ENSO–ISMR relationship. We identified that the diversity of ENSO's evolution, continuing from the previous winter or emerging from late spring, is the dominant factor perturbing the ENSO–ISMR relationship in recent epochs, with tropical Atlantic SSTAs as the crucial bridge. This finding should be considered in our efforts to improve ISMR prediction.
format Article in Journal/Newspaper
author Xianke Yang
Ping Huang
author_facet Xianke Yang
Ping Huang
author_sort Xianke Yang
title Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000
title_short Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000
title_full Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000
title_fullStr Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000
title_full_unstemmed Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000
title_sort restored relationship between enso and indian summer monsoon rainfall around 1999/2000
publisher Elsevier
publishDate 2021
url https://doi.org/10.1016/j.xinn.2021.100102
https://doaj.org/article/aae3f2b7d1ae486c8f7223039dbfa6f6
geographic Indian
geographic_facet Indian
genre North Atlantic
genre_facet North Atlantic
op_source The Innovation, Vol 2, Iss 2, Pp 100102- (2021)
op_relation http://www.sciencedirect.com/science/article/pii/S2666675821000278
https://doaj.org/toc/2666-6758
2666-6758
doi:10.1016/j.xinn.2021.100102
https://doaj.org/article/aae3f2b7d1ae486c8f7223039dbfa6f6
op_doi https://doi.org/10.1016/j.xinn.2021.100102
container_title The Innovation
container_volume 2
container_issue 2
container_start_page 100102
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