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DOWNSCALING

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Projection (extrapolation) of ... Projection (interpolation) of coarse resolution info onto finer scales ... Interpolation in. Space. Time. Across variables ' ... – PowerPoint PPT presentation

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Title: DOWNSCALING


1
DOWNSCALING
  • Bo Cui , Yuejian Zhu, Zoltan Toth
  • Environmental Modeling Center
  • NOAA/NWS/NCEP
  • Ackn.
  • Steve Lord, Geoff DiMego, Ken Mitchell
  • http//wwwt.emc.ncep.noaa.gov/gmb/ens/index.html

2
FORECASTING, BIAS CORRECTION, DOWNSCALING
  • Forecasting
  • Projection (extrapolation) of events in time into
    the future
  • Assessed by measures of statistical resolution
  • Numerical modeling techniques dominate
  • Model drift causes lead-time dependent
    systematic error (forecast bias)
  • Statistical bias correction possible
  • Finite resolution in time, space, variables due
    to limited computational resources
  • Increasing resolution has limited return in
    statistical resolution
  • Downscaling possible
  • Statistical bias correction in numerical modeling
  • Estimate/eliminate lead-time dependent systematic
    error from forecasts
  • Primary choice is improving numerical model
  • Make forecasts statistically look like initial
    (analyzed) fields
  • Improved statistical reliability
  • Feedback to numerical modeling
  • Downscaling
  • Projection (interpolation) of coarse resolution
    info onto finer scales
  • Needed due to computational resource limitations
  • Interpolation in

3
FORECASTING, BIAS CORRECTION, DOWNSCALING - 2
  • Example Global forecast integration out to 16
    days on 1x1 degree grid
  • Forecast part is done
  • Resolution cannot be improved via statistical
    post-processing etc
  • Fidelity (statistical resolution) can be
    improved by either
  • Bias correction of eg 10-day forecast on model
    grid
  • Make 1x1 degree forecast look like 1x1 degree
    analysis
  • Downscaling
  • Make 1x1 degree analysis (or bias-free fcst) look
    like 5x5 km analysis
  • Relationship between bias correction and
    downscaling
  • Common
  • Both intend to improve statistical reliability
  • Difference
  • Lead-time dependent correction
  • Bias correction
  • Enhanced spatial resolution
  • Downscaling
  • Joint/mixed application
  • Often two goals addressed with same algorithm
  • Potential benefits if treated separately

4
DOWNSCALING
  • Goal
  • Establish relationship between coarse and fine
    resolution data
  • Assume difference between low hires analysis is
    systematicreproducible
  • Entire difference is deterministic
  • Hires numerical model could capture difference
  • Performance objectives
  • Systematic error reduced enhanced statistical
    reliability
  • Random errors not increased maintained
    statistical resolution
  • Approaches/methods with various levels of
    sophistication
  • Climatological downscaling
  • Eg, difference in climate mean low hires
    analysis fields
  • Smart Init effect of topography, etc (any
    case dependent adjustments?)
  • Regime dependent
  • Eg, time mean difference in recent low hires
    analysis fields
  • Bo Cui, decaying averaging difference
  • Gridded MOS, Analog approaches, etc
  • Case dependent
  • Physics considered (INFORM) simplified
    numerical models
  • Hybrid ensemble (Jun Du others), dual
    resolution 3/4DVAR or ens-DA

5
CHARACTERISTICS OF RELIABILITY RESOLUTION
  • Reliability
  • Related to form of forecast, not forecast content
  • Fidelity of forecast
  • Reproduce nature when resolution is perfect,
    forecast looks like nature
  • Not related to time sequence of forecast/observed
    systems
  • How to improve?
  • Make model more realistic
  • Also expected to improve resolution
  • Statistical bias correction Can be statistically
    imposed at one time level
  • If both natural forecast systems are stationary
    in time
  • If there is a large enough set of
    observed-forecast pairs
  • Link with verification
  • Replace forecast with corresponding fdo
  • Resolution
  • Related to inherent predictive value of forecast
    system
  • Not related to form of forecasts
  • Statistical consistency at one time level
    (reliability) is irrelevant
  • How to improve?

6
STATISTICAL RELIABILITY TEMPORAL AGGREGATE
STATISTICAL CONSISTENCY OF FORECASTS WITH
OBSERVATIONS
  • BACKGROUND
  • Consider particular forecast class Fa
  • Consider frequency distribution of observations
    that follow forecasts Fa - fdoa
  • DEFINITION
  • If forecast Fa has the exact same form as fdoa,
    for all forecast classes,
  • the forecast system is statistically consistent
    with observations gt
  • The forecast system is perfectly reliable
  • MEASURES OF RELIABILITY
  • Based on different ways of comparing Fa and fdoa

7
STATISTICAL RESOLUTION TEMPORAL EVOLUTION
ABILITY TO DISTINGUISH, AHEAD OF TIME, AMONG
DIFFERENT OUTCOMES
  • BACKGROUND
  • Assume observed events are classified into finite
    number of classes, like Oa
  • DEFINITION
  • If all observed classes (Oa, Ob,) are preceded
    by
  • Distinctly different forecasts (Fa, Fb,)
  • The forecast system resolves the problem gt
  • The forecast system has perfect resolution
  • MEASURES OF RESOLUTION
  • Based on degree of separation of fdos that
    follow various forecast classes
  • Measured by difference between fdos climate
    distribution
  • Measures differ by how differences between
    distributions are quantified

FORECASTS
OBSERVATIONS
EXAMPLES
8
FORECAST SYSTEM ATTRIBUTES
  • Abstract concept (like length)
  • Reliability and Resolution
  • Both can be measured through different statistics
  • Statistical property
  • Interpreted for large set of forecasts
  • Describe behavior of forecast system, not a
    single forecast
  • For their definition, assume that
  • Forecasts
  • Can be of any format
  • Single value, ensemble, categorical,
    probabilistic, etc
  • Take a finite number of different classes Fa
  • Observations
  • Can also be grouped into finite number of
    classes like Oa

9
CHARACTERISTICS OF FORECAST SYSTEM ATTRIBUTES
  • RELIABILITY AND RESOLUTION ARE
  • General forecast attributes
  • Valid for any forecast format (single,
    categorical, probabilistic, etc)
  • Independent attributes
  • For example
  • Climate pdf forecast is perfectly reliable, yet
    has no resolution
  • Reversed rain / no-rain forecast can have perfect
    resolution and no reliability
  • To separate them, they must be measured according
    to general definition
  • If measured according to traditional definition
  • Reliability resolution can be mixed
  • Function of forecast quality
  • There is no other relevant forecast attribute
  • Perfect reliability and perfect resolution
    perfect forecast system
  • Deterministic forecast system that is always
    correct
  • Both needed for utility of forecast systems
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