Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation

Studies conducted by the UK Met Office reported significant skill in predicting the winter North Atlantic Oscillation (NAO) index with their seasonal prediction system. At the same time, a very low signal‐to‐noise ratio was observed, as measured using the “ratio of predictable components” (RPC) metr...

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Main Authors: Strommen, K, Palmer, T
Format: Journal article
Published: Royal Meteorological Society 2018
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author Strommen, K
Palmer, T
author_facet Strommen, K
Palmer, T
author_sort Strommen, K
collection OXFORD
description Studies conducted by the UK Met Office reported significant skill in predicting the winter North Atlantic Oscillation (NAO) index with their seasonal prediction system. At the same time, a very low signal‐to‐noise ratio was observed, as measured using the “ratio of predictable components” (RPC) metric. We analyse both the skill and signal‐to‐noise ratio using a new statistical toy model, which assumes NAO predictability is driven by regime dynamics. It is shown that if the system is approximately bimodal in nature, with the model consistently underestimating the level of regime persistence each season, then both the high skill and high RPC value of the Met Office hindcasts can easily be reproduced. Underestimation of regime persistence could be attributable to any number of sources of model error, including imperfect regime structure or errors in the propagation of teleconnections. In particular, a high RPC value for a seasonal mean prediction may be expected even if the model's internal level of noise is realistic.
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spelling oxford-uuid:0033d709-5147-4d95-a330-7420d39887ec2022-03-26T08:28:18ZSignal and noise in regime systems: A hypothesis on the predictability of the North Atlantic OscillationJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:0033d709-5147-4d95-a330-7420d39887ecSymplectic Elements at OxfordRoyal Meteorological Society2018Strommen, KPalmer, TStudies conducted by the UK Met Office reported significant skill in predicting the winter North Atlantic Oscillation (NAO) index with their seasonal prediction system. At the same time, a very low signal‐to‐noise ratio was observed, as measured using the “ratio of predictable components” (RPC) metric. We analyse both the skill and signal‐to‐noise ratio using a new statistical toy model, which assumes NAO predictability is driven by regime dynamics. It is shown that if the system is approximately bimodal in nature, with the model consistently underestimating the level of regime persistence each season, then both the high skill and high RPC value of the Met Office hindcasts can easily be reproduced. Underestimation of regime persistence could be attributable to any number of sources of model error, including imperfect regime structure or errors in the propagation of teleconnections. In particular, a high RPC value for a seasonal mean prediction may be expected even if the model's internal level of noise is realistic.
spellingShingle Strommen, K
Palmer, T
Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
title Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
title_full Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
title_fullStr Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
title_full_unstemmed Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
title_short Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
title_sort signal and noise in regime systems a hypothesis on the predictability of the north atlantic oscillation
work_keys_str_mv AT strommenk signalandnoiseinregimesystemsahypothesisonthepredictabilityofthenorthatlanticoscillation
AT palmert signalandnoiseinregimesystemsahypothesisonthepredictabilityofthenorthatlanticoscillation