Decadal variation of prediction skill for Indian Ocean dipole over the past century

Indian Ocean dipole (IOD) is one of the dominant modes of interannual variability in the Indian Ocean, which has global climate impacts and thus is one of the key targets of seasonal predictions. In this study, based on a century-long seasonal hindcast experiment from the Coupled Seasonal Forecasts...

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Main Authors: Shuai Hu, Bo Wu, Tianjun Zhou
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Climate
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fclim.2022.1082026/full
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author Shuai Hu
Bo Wu
Tianjun Zhou
Tianjun Zhou
author_facet Shuai Hu
Bo Wu
Tianjun Zhou
Tianjun Zhou
author_sort Shuai Hu
collection DOAJ
description Indian Ocean dipole (IOD) is one of the dominant modes of interannual variability in the Indian Ocean, which has global climate impacts and thus is one of the key targets of seasonal predictions. In this study, based on a century-long seasonal hindcast experiment from the Coupled Seasonal Forecasts of the 20th century (CSF-20C), we show that the prediction skill for IOD exhibits remarkable decadal variations, with low skill in the early-to-mid 20th century but high skill in the second half of the 20th century. The decadal variations of prediction skills for IOD are caused by two factors. The first is associated with the decadal variation of the ENSO-IOD relationship. Although individual members of the predictions can simulate the variation of the ENSO-IOD relationship, with amplitude close to that in the observation, the feature is greatly suppressed in the ensemble mean due to the asynchrony of variation phases among individual members. In the ensemble mean, the IOD evolution shows an unrealistic stable and high correlation with ENSO evolution. This causes the prediction to have much higher skill for those periods during which IOD is accompanied by ENSO in the observation. The second factor is associated with the decadal variation of IOD predictability in the prediction system. In the prediction system, the decadal variation of IOD signal strength closely follows that of ENSO signal strength. Meanwhile, the IOD noise strength shows variations opposite to the IOD signal strength. As a result, the signal-to-noise ratio greatly increases in the second half of the 20th century due to the enhancement of the ENSO signal strength, which represents the increase of IOD predictability in the prediction system.
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spelling doaj.art-bf1b80af687e446d94a147e841f141062023-01-06T14:50:07ZengFrontiers Media S.A.Frontiers in Climate2624-95532023-01-01410.3389/fclim.2022.10820261082026Decadal variation of prediction skill for Indian Ocean dipole over the past centuryShuai Hu0Bo Wu1Tianjun Zhou2Tianjun Zhou3State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, ChinaUniversity of the Chinese Academy of Sciences, Beijing, ChinaIndian Ocean dipole (IOD) is one of the dominant modes of interannual variability in the Indian Ocean, which has global climate impacts and thus is one of the key targets of seasonal predictions. In this study, based on a century-long seasonal hindcast experiment from the Coupled Seasonal Forecasts of the 20th century (CSF-20C), we show that the prediction skill for IOD exhibits remarkable decadal variations, with low skill in the early-to-mid 20th century but high skill in the second half of the 20th century. The decadal variations of prediction skills for IOD are caused by two factors. The first is associated with the decadal variation of the ENSO-IOD relationship. Although individual members of the predictions can simulate the variation of the ENSO-IOD relationship, with amplitude close to that in the observation, the feature is greatly suppressed in the ensemble mean due to the asynchrony of variation phases among individual members. In the ensemble mean, the IOD evolution shows an unrealistic stable and high correlation with ENSO evolution. This causes the prediction to have much higher skill for those periods during which IOD is accompanied by ENSO in the observation. The second factor is associated with the decadal variation of IOD predictability in the prediction system. In the prediction system, the decadal variation of IOD signal strength closely follows that of ENSO signal strength. Meanwhile, the IOD noise strength shows variations opposite to the IOD signal strength. As a result, the signal-to-noise ratio greatly increases in the second half of the 20th century due to the enhancement of the ENSO signal strength, which represents the increase of IOD predictability in the prediction system.https://www.frontiersin.org/articles/10.3389/fclim.2022.1082026/fullIndian Ocean dipole modeseasonal predictionpredictabilitysignal-to-noise ratio (S/N ratio)El Niño–Southern Oscillation (ENSO)
spellingShingle Shuai Hu
Bo Wu
Tianjun Zhou
Tianjun Zhou
Decadal variation of prediction skill for Indian Ocean dipole over the past century
Frontiers in Climate
Indian Ocean dipole mode
seasonal prediction
predictability
signal-to-noise ratio (S/N ratio)
El Niño–Southern Oscillation (ENSO)
title Decadal variation of prediction skill for Indian Ocean dipole over the past century
title_full Decadal variation of prediction skill for Indian Ocean dipole over the past century
title_fullStr Decadal variation of prediction skill for Indian Ocean dipole over the past century
title_full_unstemmed Decadal variation of prediction skill for Indian Ocean dipole over the past century
title_short Decadal variation of prediction skill for Indian Ocean dipole over the past century
title_sort decadal variation of prediction skill for indian ocean dipole over the past century
topic Indian Ocean dipole mode
seasonal prediction
predictability
signal-to-noise ratio (S/N ratio)
El Niño–Southern Oscillation (ENSO)
url https://www.frontiersin.org/articles/10.3389/fclim.2022.1082026/full
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