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PCA-based strategy to represent stations for empirical-statistical downscaling
Rasmus E. Benestad, Kajsa M. Parding, Abdelkader MezghaniICRC-CORDEX B3, Stockholm May 18, 2016
Why principal component analysis (PCA)?
Redundant information
Signal enhancement
Covariance preservation
Computation time
Orthogonality
Norwegian Meteorological Institute
Redundancy: information vs data
Norwegian Meteorological InstituteTellus A 2015, 67, 28326, http://dx.doi.org/10.3402/tellusa.v67.28326
Restructure data with information first
Norwegian Meteorological Institute
Covariance structure
Norwegian Meteorological Institute
Sensitivity to predictor domain
Norwegian Meteorological Institute
Requirements for PCA-based downscaling
No missing dataSuitable distributionNot too spatially spread
Norwegian Meteorological Institute
Test of pcafill
Data matrix with missing data
Complete data matrix
Norwegian Meteorological Institute
Example of PCA-based regression
• Apply multiple regression to single principal components.
• Fast: 4 leading modes rather than ~400 stations• especially for large ensembles
Norwegian Meteorological Institute
Downscaling: diagnostics for leading PCA
Norwegian Meteorological Institute
PCA quick to grid: only a few patterns
LatticeKrigCovariate: z
Norwegian Meteorological Institute
“Warm season” wet-day mean precip μ
Norwegian Meteorological Institute
“Warm season” wet-day frequency fw
Storm tracks
Thank you for your attention!
Tellus A 2015, 67, 28326, http://dx.doi.org/10.3402/tellusa.v67.28326
Benestad, Rasmus; Parding, Kajsa; Isaksen, Ketil, Mezghani, Abdelkader “Climate change and projections for the Barents region: what is expected to change and what will stay the same?", ERL-102170.R2 (accepted)
https://github.com/metno/esd_Rmarkdown/tree/master/CORDEX