Statistical Downscaling of General Circulation Models to Produce Climate Change Scenarios for Halifax, NS - PowerPoint PPT Presentation

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Statistical Downscaling of General Circulation Models to Produce Climate Change Scenarios for Halifax, NS

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Title: Statistical Downscaling of General Circulation Models to Produce Climate Change Scenarios for Halifax, NS


1
Statistical Downscaling of General Circulation
Models to Produce Climate Change Scenarios for
Halifax, NS
  • Lee Titus BSc (physics), Dmet, MSc Candidate
    (physics)
  • Environment Canada
  • Meteorological Service of Canada
  • Climate Change Section
  • In collaboration with Dr. Richard Greatbatch,
    Dr. Jinyu Sheng and Dr. Ian Folkins in the
    Department of Atmospheric Science at Dalhousie
    University

1
2
(No Transcript)
3
Typical grid spacing in a GCM
4
4
From IPCC 2001
5
METHOD
  • Remove seasonal cycle from predictand/predictors.
  • Focus on Winter (DJF)
  • Predictor Selection
  • Principal component analysis (PCA).
  • Multiple linear regression on Tmax and NCEP PCs.
  • Validation
  • Use CGCM3 predictors to hindcast historical
    distribution.
  • Use future CGCM3 predictors to make projections.

6
Seasonal cycle removal
7
Predictor Selection
  • mean sea level Pressure
    Redundancy inspired the removal of
  • 500hpa geopotential height
  • 500hpa zonal windspeed.
  • 500hpa meridional windspeed
    total windspeed
  • 500hpa vorticity
  • 850hpa geopotential height

  • 850hpa zonal windspeed
  • 850hpa meridional windspeed
    wind direction
  • 850hpa vorticity
  • surface zonal windspeed

  • surface meridional windspeed
  • surface vorticity
    divergence
  • 500hpa specific humidity
  • 850hpa specific humidity
  • surface specific humidity
  • surface mean temperature

8
PCA/MLR BASICS
9
PCA
  • mean sea level pressure -0.17
  • 500hpa geopotential height 0.14
  • 500hpa zonal windspeed -0.05
  • 500hpa meridional windspeed 0.48
  • 500hpa vorticity -0.14
    CORRELATION 0.62
  • 850hpa geopotential height -0.01
    40 of the variation in TMAX is
  • 850hpa zonal windspeed -0.08
    explained by temperature advection
  • 850hpa meridional windspeed 0.58
  • 850hpa vorticity 0.10
  • surface zonal windspeed -0.13
  • surface meridional windspeed 0.52
  • surface vorticity
    0.24

10
PCA
850GPH
500GPH
????
MSLP
11
REGRESSION INFO
  • Explained variance (percent) 79
  • Regression error variance 0.07
  • Number of predictors (PC's) 10
  • Gamma squared 0.21

12
VALIDATION
13
NCEP PREDICTION
14
NEXT
  • Once the best historical model from NCEP has been
    madehindcast using CGCM3 predictors.
  • Project the CGCM3 predictors onto the
    eigenvectors created from NCEP.

15
CGCM3 PREDICTION
16
PROJECTIONS
1

17
SUMMARY
  • Predictor Selection/PCA improves regression
  • Reduces autocorrelation of regression errors
    (removal of seasonal cycle).
  • Identify governing physics by season (gives
    confidence in the future).
  • Normal distributions are a much better assumption
    using seasons compared to annual.

18
My Next Steps
  • FDEOFR to get regression coefficients as a
    function of frequency.
  • FDEOFR gives candidate downscaling frequencies
    and helps sort out physics (climate vs. weather)

19
CLIMATE QUOTES
  • The reasonable man tries to adapt to the world
    around him, while the unreasonable tries to
    adapt the world to himself. Therefore all
    progress depends on the unreasonable man
  • --George Bernard Shaw
  • The real problem is not global warming. It is
    in fact the majoritys level of awareness. As if
    we are somehow separate from nature
  • --Lee Titus
  • The laws of Congress and the laws of physics
    have grown increasingly divergent, and the laws
    of physics are not likely to change."--Bill
    McKibben
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