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Internal climate memory in observations and models
Attribution of cause of climate change is hindered by our ability to separate internal low‐frequency variability from the forced response in the climate system. We characterize the spatiotemporal characteristics of internal variability by comparing ensemble averages of in‐band fractional variances i...
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Published in: | Geophysical research letters 2015-02, Vol.42 (4), p.1232-1242 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Attribution of cause of climate change is hindered by our ability to separate internal low‐frequency variability from the forced response in the climate system. We characterize the spatiotemporal characteristics of internal variability by comparing ensemble averages of in‐band fractional variances in Coupled Model Intercomparison Project Phase 5 (CMIP5) preindustrial control simulations to estimates from observations and reanalyses. For sea surface temperature and sea level height anomalies both models and observations show that variability on time scales less than 5 years is predominantly in the tropics and has the spatial signature of El Niño–Southern Oscillation. On progressively longer time scales the variance moves to the extratropics and from middle to higher latitudes while displaying spatially coherent features. The CMIP5 models show good agreement in the spatial and temporal apportioning of in‐band variance when the variances are normalized.
Key Points
Beyond 5 years little variance evident in the tropics
Southern Hemisphere oceans variance maxima are in subtropical baroclinic zones
Memory on longer time scales is related to identifiable dynamical processes |
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ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1002/2014GL062765 |