Journal article
Signal and noise in regime systems: A hypothesis on the predictability of the North Atlantic Oscillation
- Abstract:
- 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.
- Publication status:
- Published
- Peer review status:
- Peer reviewed
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- Files:
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(Preview, Accepted manuscript, pdf, 7.3MB, Terms of use)
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- Publisher copy:
- 10.1002/qj.3414
Authors
+ European Research Council
More from this funder
- Funding agency for:
- Strommen, K
- Palmer, T
- Grant:
- Seventh Framework Programme: 641727
- 291406
- Publisher:
- Royal Meteorological Society
- Journal:
- Quarterly Journal of the Royal Meteorological Society More from this journal
- Volume:
- 145
- Issue:
- 718
- Pages:
- 147-163
- Publication date:
- 2018-10-10
- Acceptance date:
- 2018-09-28
- DOI:
- EISSN:
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1477-870X
- ISSN:
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0035-9009
- Keywords:
- Pubs id:
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pubs:952811
- UUID:
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uuid:0033d709-5147-4d95-a330-7420d39887ec
- Local pid:
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pubs:952811
- Source identifiers:
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952811
- Deposit date:
-
2018-12-17
Terms of use
- Copyright holder:
- Royal Meteorological Society
- Copyright date:
- 2018
- Notes:
- © 2018 Royal Meteorological Society. This is the accepted manuscript version of the article. The final version is available online from the Royal Meteorological Society at: https://doi.org/10.1002/qj.3414
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