360 likes | 523 Views
COST ES0601 Temperature Network 000001 Michele BRUNETTI (m.brunetti@isac.cnr.it) I stituto di S cienze dell' A tmosfera e del C lima CONSIGLIO NAZIONALE DELLE RICERCHE Via P. Gobetti, 101 – 40129 BOLOGNA. TARRAGONA 9-11 March 2009. CRADDOCK TEST. A. B.
E N D
COST ES0601 Temperature Network 000001 Michele BRUNETTI (m.brunetti@isac.cnr.it) Istituto di Scienze dell'Atmosfera e del Clima CONSIGLIO NAZIONALE DELLE RICERCHE Via P. Gobetti, 101 – 40129 BOLOGNA TARRAGONA 9-11 March 2009
CRADDOCK TEST A B Where is the in homogeneity? In A or B?
CORRECTION To be corrected SHIFT RATIO
SMOOTHING SMOOTHING OF THE CORRECTING FACTORS TO IMPROVE THE SIGNAL-TO-NOISE RATIO CORRECT WITHSMOOTHING CORRECT WITHOUT SMOOTHING ORIGINAL TO AVOID NOT IDENTIFIED OUTLIERS AFFECTING THE ANNUAL CYCLE Auer et al., 2005, Int. J. Clim., 25, 139-166
EXAMPLE Unsteadiness in the first derivation of the Craddock function 1st January 1933: Changes in the observation times
DAILY HOMOGENIZATION Unsteadiness in the first derivation of the Craddock function 1st January 1933: Changes in the observation times
DAILY HOMOGENIZATION The correction coefficients were calculated on monthly bases, then they were fitted with a trigonometric function in order to obtain daily corrections without discontinuities from one month to another.
SERIE GIORNALIERE Only the coherentcurveswereusedtocalculate the meancorrectingfactorseries
TREND (YEAR) ORI
TREND (WINTER) ORI
TREND (SUMMER) ORI
SOME STATISTICS 25 OUTLIERS 34 BREAKS
TREND (YEAR) ORI HOM
TREND (WINTER) ORI HOM
TREND (SUMMER) ORI HOM