Huug van den Dool and Suranjana Saha Prediction Skill and Predictability in CFS - PowerPoint PPT Presentation

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Title: Huug van den Dool and Suranjana Saha Prediction Skill and Predictability in CFS


1
Huug van den Dool and Suranjana Saha
Prediction Skill and Predictability in CFS
2
Definitions Prediction Skill and
PredictabilityOpinion Literature fuzzies up
predictability vs prediction skill
3
Definition 1 Evaluation of skill of real time
prediction the old-fashioned way. Problems a)
Sample size! , b) Wait a long time(and funding
agents are impatient)
4
Definition 1 Evaluation of skill of real time
prediction the old-fashioned way. Definition
2 Evaluation of skill of hindcasts hard, not
impossible.Problems a) Sample size, b)
honesty of hindcasts
5
Definition 1 Evaluation of skill of real time
prediction the old-fashioned way. Definition
2 Evaluation of skill of hindcasts hard, not
impossible.Definition 3 Predictability of the
1st kind ( sensitivity due to uncertainty in
initial conditions)
6
Definition 1 Evaluation of skill of real time
prediction the old-fashioned way. Sample
size!Definition 2 Evaluation of skill of
hindcasts hard, not impossibleDefinition 3
Predictability of the 1st kind ( sensitivity due
to uncertainty in initial conditions)Definition
4 Predictability of the 2nd kind due to
variations in external boundary conditions (AMIP
Potential Predictability Reproducibility
Maddens approach)
7
Predictability (theoretical/intrinsic) is a
ceiling for actual prediction skill.Any other
kinds of predictability?
8
CFS forecastX (space, lead, member ,year)
  • Space is 2.5oX2.5o (Z500) or 1oX2o (SST/mask), or
    1.875 by Gaussian (Soilw, T2m, Precip)
  • Basic data used is monthly mean
  • Lead 0, 8 in units of months member 1, 15
  • Year 1981 2003 (increases annually)
  • Example Initial Month is August ( lead 0)
  • Note IC is Jul 11/21/Aug 1 for SST, and Jul
    09-13/ 19-23 / Jul 30-Aug3 for atmosphere and
    soil.
  • Member 16 is ensemble average
  • Member 17 is matching observed field
  • X ( Z500, SST, Soilw, T2m, Precip)

9
ASPECTS
  • Prediction skill (member i vs member 17)
  • Predictability (member i vs member j)
  • Monthly mean
  • Seasonal mean
  • Ensemble average
  • Predictability of 1st kind only.

10
Two types of climatology plus complications
  • Xclim_mdl (space, lead) is average over years and
    (14 or 15) members, depending.
  • Xclim_verif (space, lead) is ave over (same)
    years for either member 17, or member i, i15.
  • Anomaly X minus Xclim, whichever is relevant
  • Systematic error (SE) is automatically corrected
    by the above
  • CV of the SE correction (exclude from Xclim the
    member and the year to be verified). Not trivial.

11
Prediction Skill Monthly
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Conclusions (monthly data)
  • CFS data is a goldmine.
  • CFS has enough (?) data for forecast evaluation
    (and diagnostics)
  • Member i vs member j unifies predictability of
    1st and 2nd kind in CFS output
  • CFS has some prediction skill. In order of skill
    SST, tropical variables, soilw,T2m, Precip
  • CFS has some more predictability (as defined),
    but ceiling is low in mid-latitudes.
  • Seasonality (no surprise)

30
To do
  • Identify interdecadal skill source (if any)
  • Identify soil moisture skill source (are models
    still too strong on local effects? How about
    non-local effects)
  • Daily data for the finer temporal scales in
    skill/predictability.
  • Why do models like CFS have predictability in so
    few d.o.f. (and is that really all there is)
  • Further ideas about new predictability notions

31
A case for the importance of knowing the
effective number of degrees of freedom (edof) in
which we have forecast skill.Considerations-)
physical models have one clear strength they can
execute the non-linear terms-) a model needs at
least 3 degrees of freedom to be non-linear
(Lorenz, 1960)-) a non-linear model with
nominally a zillion degrees of freedom, but skill
in only lt 3 dof is functionally linear in terms
of the skill of its forecasts - and, to its
detriment, the non-linear terms add random
numbers to the tendencies of the modes with
predictability. gt Therefore Physical models
need to have skill in, effectively, gt 3 dof
before they can be expected to take advantage of
non-linearity. (In a forecast setting). (
Note not any 3 degrees of freedom will do.)
32
Lingering memory CaiVan den Dool(2005) Schemm
et al calibration data set, (CFS daily data set
will be used also).
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