Optimisation of an idealised ocean model, stochastic parameterisation of sub-grid eddies

Ocean Modelling Elsevier 88 (2015) 38-53

Authors:

Fenwick C Cooper, Laure Zanna

Impact of hindcast length on estimates of seasonal climate predictability

Geophysical Research Letters 42:5 (2015) 1554-1559

Authors:

W Shi, N Schaller, D Macleod, TN Palmer, A Weisheimer

Abstract:

It has recently been argued that single-model seasonal forecast ensembles are overdispersive, implying that the real world is more predictable than indicated by estimates of so-called perfect model predictability, particularly over the North Atlantic. However, such estimates are based on relatively short forecast data sets comprising just 20 years of seasonal predictions. Here we study longer 40 year seasonal forecast data sets from multimodel seasonal forecast ensemble projects and show that sampling uncertainty due to the length of the hindcast periods is large. The skill of forecasting the North Atlantic Oscillation during winter varies within the 40 year data sets with high levels of skill found for some subperiods. It is demonstrated that while 20 year estimates of seasonal reliability can show evidence of overdispersive behavior, the 40 year estimates are more stable and show no evidence of overdispersion. Instead, the predominant feature on these longer time scales is underdispersion, particularly in the tropics.

Impact of hindcast length on estimates of seasonal climate predictability.

Geophysical research letters 42:5 (2015) 1554-1559

Authors:

W Shi, N Schaller, D MacLeod, TN Palmer, A Weisheimer

Abstract:

It has recently been argued that single-model seasonal forecast ensembles are overdispersive, implying that the real world is more predictable than indicated by estimates of so-called perfect model predictability, particularly over the North Atlantic. However, such estimates are based on relatively short forecast data sets comprising just 20 years of seasonal predictions. Here we study longer 40 year seasonal forecast data sets from multimodel seasonal forecast ensemble projects and show that sampling uncertainty due to the length of the hindcast periods is large. The skill of forecasting the North Atlantic Oscillation during winter varies within the 40 year data sets with high levels of skill found for some subperiods. It is demonstrated that while 20 year estimates of seasonal reliability can show evidence of overdispersive behavior, the 40 year estimates are more stable and show no evidence of overdispersion. Instead, the predominant feature on these longer time scales is underdispersion, particularly in the tropics.

Key points

Predictions can appear overdispersive due to hindcast length sampling errorLonger hindcasts are more robust and underdispersive, especially in the tropicsTwenty hindcasts are an inadequate sample size to assess seasonal forecast skill.

Bell's Conspiracy, Schrödinger's Black Cat and Global Invariant Sets

ArXiv 1502.06972 (2015)

Invariant Set Theory and the Symbolism of Quantum Measurement

ArXiv 1502.06968 (2015)