European windstorms: seasonal prediction and a signal to noise paradox - Prof. Adam Scaife
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European windstorms: seasonal prediction and a signal to noise paradox Prof. Adam Scaife Met Office Hadley Centre College of Engineering, Mathematics and Physical Sciences, Exeter University metoffice.gov.uk © Crown copyright
The NAO and why it is important to you Walz et al, 2018 Mailier et al, 2018 The NAO is a key driver of year to year variations in European windstorms This large scale interannual variability leads to apparent clustering of storms
Computer Models of Weather and Climate 5 fundamental equations + ideal gas law Represented on a 3D grid of points Small scale processes in ‘S’ The problem is well defined but these equations have an unfortunate property… Scaife et al, Physics World, 2007
‘One flap of a seagull’s wings may forever change the course of the weather’ Ed Lorenz (1917-2008) - Small changes now can grow into storms or dead calm a few months later - Does this scupper long range forecasting? - Can we use our computer models to investigate the possibilities?
Predictability of winter weather from early November Winter seasonal predictions Skilful predictions of the North Atlantic Oscillation Retrospective forecasts in red Real time forecasts in blue Real world observations in black So where does this come from? Correlation = 62% Scaife et al, GRL, 2014
The importance of tropical rainfall High skill in winter rainfall forecasts Tropical rainfall explains NAO forecast Tropical rainfall explains real NAO Scaife et al., IJOC, 2018 Scaife et al., QJRMS, 2017 Predicted signals in the NAO come largely from tropics Rainfall may even give a better prediction than the predicted NAO! So how good are models at predicting tropical rainfall?
Seasonal forecasts do a decent job for rainfall (despite what people say about computer models) WINTER AVERAGE YEAR TO YEAR VARIATIONS REAL WORLD MODEL Scaife et al., IJOC, 2018
Prediction skill is high in the Atlantic Ocean Scaife et al., IJOC, 2018
Prediction skill is reasonable in the Indian Ocean (but varies across models) Scaife et al., IJOC, 2018
ENSO explains ranking of interannual variability and ranking of skill Top row shows variability Bottom row shows effect of ENSO Note ranking: TEP > TWP > TAT > TIO Scaife et al., IJOC, 2018
From tropical rainfall to the extratropics Rossby Wave Sources Teleconnections as Rossby waves A few common source regions Poleward and eastward propagation of waves Fluctuate with forcing from tropical rainfall Introduces som symmetry about the equator Scaife et al, QJRMS, 2017
Tropical rainfall predictions allow good predictions of the NAO Observed rainfall => Observed NAO Modelled rainfall => Observed NAO Single models can beat a multi-model Rainfall gives better prediction than forecast NAO Scaife et al., IJOC, 2018
A fly in the ointment: The signal to noise paradox metoffice.gov.uk © Crown copyright
Revisit the predictability of the NAO Winter NAO seasonal predictions Model predicting real Skilful predictions of the NAO world But signals are small Winter NAO predictions Model Skill rises slowly with ensemble size predicting itself Model can predict the real world but not itself! © Crown Scaife et copyright al 2014, Met Office Eade et al 2014, Siegert et al 2015, Dunstone et al 2016, Scaife and Smith 2018
A simple interpretation of what’s going on Real world Model 24 hPa2 Unpredictable 58 hPa2 64 hPa2 64 hPa2 40 hPa2 Predictable 6 hPa2 Forecasts appear to have about the right amount of variability BUT The proportion of variability that is predictable appears to be less in models
Another use of ensemble forecasts: UNprecedented Simulated Extremes using ENsembles metoffice.gov.uk © Crown copyright
January 2014: just a freak? What chance of recurrence? www.theguardian.co.uk January 2014 saw the greatest monthly rainfall total on record Could it have been even worse? metoffice.gov.uk © Crown copyright
UNprecedented Simulated Extremes using ENsembles SE England Rainfall Record SE England Rainfall Simulations Observations Model Observations are inherently uncertain due to atmospheric chaos Dynamical models now getting good enough in some cases to be indistinguishable from observations => Availability of many more samples & unprecedented events metoffice.gov.uk Thompson et©al., Crown Nat. copyright Comm., 2017
Unprecedented weather conditions… Weather patterns for extreme rainfall in observations Our physically based computer simulations have realistic but different patterns Both the NAO and EAP patterns are visible in these extreme cases metoffice.gov.uk Thompson et©al., Crown Nat. copyright Comm., 2017
Global applications: heatwaves in SE China We can use this method to estimate extremes in other regions We can also track down remote global influences Thompson et al., Clim. Dyn., 2018
Summary Skilful seasonal prediction of the winter NAO and hence European windstorm activity is now possible and is driven largely from the tropics It’s mainly the NAO that is predictable (rather than other important patterns) Predicted signals are inexplicably small Not just a simple matter of errors in spread Models are unpredictable but they can predict the real world => ‘Signal to Noise Paradox’ Irrespective of any predictability, these ensemble simulations can also be used to investigate the chances of extreme and even unprecedented events as well as their meteorology
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