© crown copyright met office long-range forecasting emily wallace nov 2012
TRANSCRIPT
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© Crown copyright Met Office
Long-range forecasting
Emily Wallace Nov 2012
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© Crown copyright Met Office
Content
• How is long-range forecasting possible?
• predictability vs chaos, drivers of predictability, what is predictable?
• Dynamical seasonal prediction systems
• Initialisation, coupled modelling, assessing uncertainty
• Hindcasts
• Bias correction, model climatology, skill assessment
• Products
• Standard products, bespoke products
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How is it possible?
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Predictability and chaos
‘chaos’
dry wetThe distribution is analogous to the climatology of a meteorological variable (here, rainfall).
The ball drops can be seen as values corresponding to individual years.
• The precise bin in which a ball falls cannot be predicted (‘chaos’).
• If many drops are made, the ‘distribution’ of balls in the bins can be described.
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Predictability and chaos
wetdry
‘chaos’
large-scale influences
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Individual ball drops are analogous to individual forecasts, all with similar starting points.
The prediction consists in quantifying the difference between the two distributions (climatology and forecast).
Example of large-scale influence:ocean temperatures
• The precise bin in which a ball falls still cannot be predicted (‘chaos’).
• The tilt of the table changes the shape of the distribution (‘predictability’).
• If many drops are made, the new distribution of balls in the bins can be described.
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time
pred
icta
bilit
y
ICs
SSTs, surface, etc
external forcings
days months years
Sources of predictability: Initial conditionsBoundary conditions (SST, soil moisture, etc); External forcing (emissions, etc)
Seasonal: probabilistic forecast
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Example of forcing: sea surface temperature anomalies
The forcing pattern is large scale and slow-varying in time.The impact is also large scale.
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Teleconnections: typical El Niño impacts
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Teleconnections: typical La Niña impacts
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• ‘climate’ (seasonal averages), not ‘weather’ (conditions on specific days)
• large-area averages, not localised events
• range of outcomes, with probabilities attached to them (risk)
What is predictable at long range?
How are long-range predictions done?
• statistical methods – using empirical relationships derived from historical records
• dynamical methods – using dynamical (climate) models
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Statistical models – using empirical relationships derived from historical records
Statistical models are…
• Cheap – equations are far less complex than dynamical models
But…
• Require a long, good quality, observational dataset to train the model on
• Will produce poor predictions if the assumptions change
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Seasonal forecasting with dynamical models
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A seasonal forecasting system requires:
• definition of starting point (initial conditions; data assimilation)
• model of the climate system
• description of uncertainties (ensembles)
Dynamical methods: seasonal forecasting systems
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For seasonal forecasting, assimilation of ocean state is important
Tropical Atmosphere Ocean array (TAO)
ARGO floats
SST
Subsurface ocean
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Climate simulation Vs. seasonal prediction
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Climate model
Observed state of ocean/atmosinitialisation time
Synchronised to real world
Forecast from initialisation time
Climate model
Climate simulationArbitrary or climatology start
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A seasonal forecasting system requires:
• definition of starting point (initial conditions; data assimilation)
• model of the climate system
• description of uncertainties (ensembles)
Dynamical methods: seasonal forecasting systems
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Coupled and uncoupled seasonal forecast systems http://www.wmolc.org “Data ->system configuration”
• Coupled (1-tier) systems
• Model: Includes interactive 3D ocean model
• Initial conditions: atmosphere + 3D ocean
• GPCs: Exeter, ECMWF, Washington, Toulouse, Melbourne, Montreal, Tokyo, Beijing
• Forecast range: typically 6 months +
• Uncoupled (2-tier) systems
• Model: atmosphere only + prescribed SST. Atmosphere ‘forced’ with predicted (or persisted) SST anomalies. No 2-way atmosphere/ocean interaction
• Initial conditions: atmosphere (usually) + SST
• GPCs: Moscow, Seoul, CPTEC, Pretoria
• Forecast range: typically 3-5 months
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A seasonal forecasting system requires:
• definition of starting point (initial conditions; data assimilation)
• model of the climate system
• description of uncertainties (ensembles)
Dynamical methods: seasonal forecasting systems
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Uncertainty type 1: initial condition uncertainty
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Climate model
Data assimilation: ocean/atmos
• Run model forecasts from many slightly different initial conditions• Forecasts may evolve differently • Collectively, the ensemble estimates the range of uncertainty stemming from sensitivity to initial conditions
forecastEnsemble prediction
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Addressing initial condition uncertainties
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Uncertainty in initial atmospheric
state Uncertainty in future atmospheric
state
Ensemble forecast explores part of the future uncertainty (from initial
condition) uncertainty
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Uncertainty type 2: uncertainty in model formulation• When climate models are developed choices must be
made on schemes to represent physical processes
• e.g. Convection scheme, radiation scheme...
• Forecasts from the same basic model and same initial state may give different forecasts when different physics schemes are used.
• Choice of physics scheme is often centre dependent
• Thus more uncertainty!
• Model formulation uncertainties are addressed by:
• Stochastically perturbing model variables (and/or tuneable physics parameters) as the model runs
• Combining ensembles from different modelling centres. Typically each centre will have made different choices in model formulation. Thus multi-model: e.g. LC-LRFMME, EUROSIP, APCC
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Addressing model formulation uncertainties
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Uncertainty in initial atmospheric
state Uncertainty in future atmospheric
state
Ensemble forecast from model 1 explores part of the future uncertainty (from initial
condition) uncertainty
Ensemble forecast from model 2 (i.e. perturbed physics), run from same set of initial states, typically explores additional future uncertainties (from model
formulation uncertainty)
Including representation of model formulation uncertainties gives better sampling of the true uncertainty.
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Example ensemble predictionsMet Office GloSea4 system
• Initial condition uncertainty (lagged analysis)
• 21 different initial ocean/atmos states used (daily lag)
• Model formulation uncertainty
• Stochastic (kinetic energy) perturbations to model wind field as the model runs
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22nd Feb‘11
23rd
Mar’1121st Feb‘11
Forecast
2 perturbed runs from daily start dates ->14 runs to (7 months) each week, after 3 weeks we have a 42 member ensemble
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GloSea4 ensemble prediction of Nino3.4 SST anomaly from March 2010
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Ensemble ‘postage’ stamps
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Ensemble mean: reinforces commonalities, masks uncertainties
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Qualities of the ensemble mean
• Considered the ‘most likely’ single (deterministic) prediction.
• Usually lies near centre of the ensemble distribution
• Picks out the dominant signal:
• Commonalities across the members ‘reinforce’
• Differences across members tend to cancel
Important ‘but’…..
• Quantitative information on uncertainty is removed by the averaging process
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Seasonal prediction systems
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Climate model
Initialisation:Current state of ocean/atmos
forecast
Ensemble generation
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Hindcasts: Correcting model climatology and assessing model quality
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Hindcasts: for bias correction and skill assessments
• To adjust for biases in the seasonal forecast we generate a set of retrospective forecasts (hindcasts) that describe the ‘climatology’ of the model
• Model climatologies are defined over all retrospective years and all members
• For GloSea4: 14 hindcast years, 12 members = 168 realisations of each season.
• Note: most systems have more ensemble members in the real-time forecast than in the hindcast set.
• Hindcasts are also the basis of assessing forecast performance
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Model bias
• In this example:
• 14 years (1989-2002)
• 8 members per year
Calibrated forecast
obs
Hindcastmean
Forecastmembers
At long range, predict anomalies
black line: observed climatologyPale red lines: hindcast membersblue line: model climatology
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MAM Temperatures in SE Asia
March-April-May
Temperature Anomalies relative to 1961-1990
Black Line:
CRUTEM3
Red Lines:
8 GCM simulations• CNRM-CM5
• CanEMS2
• GISS-ES-R
• HadGEM2-ES
• NorESM1-M
• bcc-csm1-1
• inmcm4
• ipsl-csma
The model simulations were extended to 2010 following RCP8.5
Courtesy of Nikos Christidis
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• PROBLEM:
• What does “climate” mean under climate change?
Calculating anomalies: the importance of the reference period
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Ensemble-mean forecast for the average temperature anomaly over MAM 2011
1996-2009
1981-2010
1971-2000
Reference period
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Generating probabilistic forecasts
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Probabilistic forecasts and bias correction e.g. precipitation forecast
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wet
dry
Observed climatology,
Lower tercile (obs)
Upper tercile (obs)
Model climatology, e.g. wet bias
Upper tercile (model)
Lower tercile (model)
Ensemble member
Member is counted as a prediction of the average (obs) tercile category
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Generating probability forecasts from the ensemble
• An estimate of the forecast probability of an event is the proportion of the ensemble members that predict the event
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Category No. Members that predict category
Fraction of total ensemble members
Forecast probability
above 5 5/9 55%
average 3 3/9 33%
below 1 1/9 11%
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Seasonal prediction systems
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Climate model
Initialisation:Current state of ocean/atmos
forecast
Ensemble generation
Retrospective forecasts
(hindcasts)Skill
assessment(verification)
Forecast bias correction
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Hindcasts: Assessing skill
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Skill of seasonal forecasting systems
• Skill is assessed on the hindcast (covering a number of past years)
• Can (and should) be done in several ways:
• Statistical assessment of skill
• Process based assessment
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What is in Malaysia for me?What’s in Malaysia for me?
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Statistical skill of forecast products, estimated from hindcasts:http://www.metoffice.gov.uk/research/climate/seasonal-to-decadal/gpc-outlooks/glob-seas-prob-skillROC curves Reliability
diagram
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• Forecasts are generated monthly using data from GloSea4 and ECMWF
• Skill (linear correlation) of 6-month forecasts from March to September is detailed below
Skill (linear correlation)
Mar Apr May Jun Jul Aug Sep
TS 0.26 0.49 0.59 0.33 0.55 0.50 0.42
ACE 0.14 0.25 0.74 0.61 0.56 0.46 0.17
Perfect forecasts would have a skill of 1.0
Deterministic skill assessmentSkill of tropical storm seasonal forecast 1987–2009
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Skill of seasonal forecasting systems
• Skill is assessed on the hindcast (covering a number of past years)
• Can (and should) be done in several ways:
• Statistical assessment of skill
• Process based assessment
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Time
Lat
itud
e
Colours: 5-day average rainfall in mm/day, 10°W-10°E
Red line: Timing of monsoon onset , early July
Time
Lat
itud
e
Mean observed rainfall (TRMM1998-2010) GloSea4 mean rainfall (1996-2009), 25 April start dates
•Good agreement between observed and GloSea4 temporal evolution of monsoon and onset timing
•Some skill in predicting late/early onset (ROC score ~0.6)
Seasonal forecasts with GloSea4 of timing of monsoon onset over Sahel
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ENSO teleconnections: precipitation
JJA
DJF
Forecast (E-L) Observed (E-L)
Skilful reproductions in the tropics – even for rainfall
Red = El Nino is drier Blue = El Nino is wetter
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Examples of simple forecast products:http://www.metoffice.gov.uk/research/climate/seasonal-to-decadal/gpc-outlooks
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‘Raw’ products
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Examples of bespoke forecast products and information
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GloSea4 Forecast probabilities for 2011 Short Rains (Sep-Nov)
Early onset: Late onset:
Courtesy of Michael Vellinga
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Observations for 2011
Plots courtesy of Lizzie Good Courtesy of Michael Vellinga
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Forecast products
Deterministic forecasts
• Provides a best estimate and forecast range (±1 stdev interval) for:
• Numbers of named storms
• ACE index
• During the following 6 months
Probabilistic forecasts
• Probability distributions
• Exceedance of thresholds (to aid assessment of risk)
• Help to quantify and communicate the inherent uncertainties in the forecast.
Public forecast
Tailored products
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Summary
How is long-range forecasting possible?
• Large scale forcing that evolve slowly can make climate predictable
Dynamical seasonal prediction systems
• Must include: initialisation, a climate model, and a way to assess uncertainty
Hindcasts
• Due to model biases hindcasts are needed for correction of forecasts, They are also used to assess forecast quality, and can lead to model improvements
Products
• We are developing new and exciting bespoke products
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Questions and answers