Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf

The Indian Ocean Dipole is a leading phenomenon of climate variability in the tropics, which affects the global climate. However, the best lead prediction skill for the Indian Ocean Dipole, until recently, has been limited to ~6 months before the occurrence of the event. Here, we show that multi-yea...

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Main Authors: F. Feba, Karumuri Ashok, Matthew Collins, Satish R. Shetye
Format: Dataset
Language:unknown
Published: 2021
Subjects:
Online Access:https://doi.org/10.3389/fclim.2021.736759.s001
https://figshare.com/articles/dataset/Data_Sheet_1_Emerging_Skill_in_Multi-Year_Prediction_of_the_Indian_Ocean_Dipole_pdf/16684948
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record_format openpolar
spelling ftfrontimediafig:oai:figshare.com:article/16684948 2023-05-15T13:57:52+02:00 Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf F. Feba Karumuri Ashok Matthew Collins Satish R. Shetye 2021-09-27T07:59:46Z https://doi.org/10.3389/fclim.2021.736759.s001 https://figshare.com/articles/dataset/Data_Sheet_1_Emerging_Skill_in_Multi-Year_Prediction_of_the_Indian_Ocean_Dipole_pdf/16684948 unknown doi:10.3389/fclim.2021.736759.s001 https://figshare.com/articles/dataset/Data_Sheet_1_Emerging_Skill_in_Multi-Year_Prediction_of_the_Indian_Ocean_Dipole_pdf/16684948 CC BY 4.0 CC-BY Climate Science Climate Change Processes Climatology (excl. Climate Change Processes) Carbon Sequestration Science Indian Ocean (Dipole) decadal prediction CanCM4 MIROC5 Southern Ocean IOD and Southern Ocean Antarctic Circumpolar Current (ACC) decadal prediction in tropics Dataset 2021 ftfrontimediafig https://doi.org/10.3389/fclim.2021.736759.s001 2021-09-29T23:00:42Z The Indian Ocean Dipole is a leading phenomenon of climate variability in the tropics, which affects the global climate. However, the best lead prediction skill for the Indian Ocean Dipole, until recently, has been limited to ~6 months before the occurrence of the event. Here, we show that multi-year prediction has made considerable advancement such that, for the first time, two general circulation models have significant prediction skills for the Indian Ocean Dipole for at least 2 years after initialization. This skill is present despite ENSO having a lead prediction skill of only 1 year. Our analysis of observed/reanalyzed ocean datasets shows that the source of this multi-year predictability lies in sub-surface signals that propagate from the Southern Ocean into the Indian Ocean. Prediction skill for a prominent climate driver like the Indian Ocean Dipole has wide-ranging benefits for climate science and society. Dataset Antarc* Antarctic Southern Ocean Frontiers: Figshare Antarctic Indian Southern Ocean
institution Open Polar
collection Frontiers: Figshare
op_collection_id ftfrontimediafig
language unknown
topic Climate Science
Climate Change Processes
Climatology (excl. Climate Change Processes)
Carbon Sequestration Science
Indian Ocean (Dipole)
decadal prediction
CanCM4
MIROC5
Southern Ocean
IOD and Southern Ocean
Antarctic Circumpolar Current (ACC)
decadal prediction in tropics
spellingShingle Climate Science
Climate Change Processes
Climatology (excl. Climate Change Processes)
Carbon Sequestration Science
Indian Ocean (Dipole)
decadal prediction
CanCM4
MIROC5
Southern Ocean
IOD and Southern Ocean
Antarctic Circumpolar Current (ACC)
decadal prediction in tropics
F. Feba
Karumuri Ashok
Matthew Collins
Satish R. Shetye
Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf
topic_facet Climate Science
Climate Change Processes
Climatology (excl. Climate Change Processes)
Carbon Sequestration Science
Indian Ocean (Dipole)
decadal prediction
CanCM4
MIROC5
Southern Ocean
IOD and Southern Ocean
Antarctic Circumpolar Current (ACC)
decadal prediction in tropics
description The Indian Ocean Dipole is a leading phenomenon of climate variability in the tropics, which affects the global climate. However, the best lead prediction skill for the Indian Ocean Dipole, until recently, has been limited to ~6 months before the occurrence of the event. Here, we show that multi-year prediction has made considerable advancement such that, for the first time, two general circulation models have significant prediction skills for the Indian Ocean Dipole for at least 2 years after initialization. This skill is present despite ENSO having a lead prediction skill of only 1 year. Our analysis of observed/reanalyzed ocean datasets shows that the source of this multi-year predictability lies in sub-surface signals that propagate from the Southern Ocean into the Indian Ocean. Prediction skill for a prominent climate driver like the Indian Ocean Dipole has wide-ranging benefits for climate science and society.
format Dataset
author F. Feba
Karumuri Ashok
Matthew Collins
Satish R. Shetye
author_facet F. Feba
Karumuri Ashok
Matthew Collins
Satish R. Shetye
author_sort F. Feba
title Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf
title_short Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf
title_full Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf
title_fullStr Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf
title_full_unstemmed Data_Sheet_1_Emerging Skill in Multi-Year Prediction of the Indian Ocean Dipole.pdf
title_sort data_sheet_1_emerging skill in multi-year prediction of the indian ocean dipole.pdf
publishDate 2021
url https://doi.org/10.3389/fclim.2021.736759.s001
https://figshare.com/articles/dataset/Data_Sheet_1_Emerging_Skill_in_Multi-Year_Prediction_of_the_Indian_Ocean_Dipole_pdf/16684948
geographic Antarctic
Indian
Southern Ocean
geographic_facet Antarctic
Indian
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation doi:10.3389/fclim.2021.736759.s001
https://figshare.com/articles/dataset/Data_Sheet_1_Emerging_Skill_in_Multi-Year_Prediction_of_the_Indian_Ocean_Dipole_pdf/16684948
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.3389/fclim.2021.736759.s001
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