May 2005CTEQ Summer School1 Uncertainties of Parton Distribution Functions Dan Stump Michigan State University.

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Presentation transcript:

May 2005CTEQ Summer School1 Uncertainties of Parton Distribution Functions Dan Stump Michigan State University

May 2005CTEQ Summer School2 Outline 1/ Introduction 2/ Compatibility of Data 3/ Uncertainty Analysis 4/ Examples of PDF uncertainty 5/ Outlook

May 2005CTEQ Summer School3 The systematic study of uncertainties of PDF’s developed slowly. Pioneers… J. Collins and D. Soper, CTEQ Note 94/01, hep-ph/ C. Pascaud and F. Zomer, LAL M. Botje, Eur. Phys. J. C 14, 285 (2000). Today many groups and individuals are involved in this research.

May 2005CTEQ Summer School4 CTEQ group at Michigan State (J. Pumplin, D. Stump, WK. Tung, HL. Lai, P. Nadolsky, J. Huston, R. Brock) and others (J. Collins, S. Kuhlmann, F. Olness, J. Owens) MRST group (A. Martin, R. Roberts, J. Stirling, R. Thorne) Fermilab group (W. Giele, S. Keller, D. Kosower) S. I. Alekhin V. Barone, C. Pascaud, F. Zomer; add B. Portheault HERA collaborations ZEUS – S. Chekanov et al; A. Cooper-Sarkar H1 – C. Adloff et al Current research on PDF uncertainties

May 2005CTEQ Summer School5 The program of Global Analysis is not a routine statistical analysis, because of systematic differences between experiments. We must sometimes use physics judgment in this complex real-world problem.

May 2005CTEQ Summer School6 Compatibility The two data sets are consistent within the systematic errors, but there is a systematic difference. The combined value is a compromise, with uncertainty from the systematic errors. Two experimental collaborations measure the same quantity  : Collaboration A Collaboration B

May 2005CTEQ Summer School7 2/ A Study of Compatibility

May 2005CTEQ Summer School8 The PDF’s are not exactly CTEQ6 but very close – a no-name generic set of PDF’s for illustration purposes. Table of Data Sets 1 BCDMS F2p BCDMS F2d H1 (a) H1 (b) H1 (c ) ZEUS CDHSW F NMC F2p NMC d/p CCFR F E E866 pp E866 d/p D0 jet CDF jet CDHSW F CCFR F CDF W Lasy N  2  2 /N N tot = 2291  2 global = 2368.

May 2005CTEQ Summer School9 So, we have accounted for … Statistical errors Overall normalization uncertainty (by fitting {f N,e }) Other systematic errors (analytically) We may make further refinements of the fit with weighting factors Default : w e and w N,e = 1 The spirit of global analysis is compromise – the PDF’s should fit all data sets satisfactorily. If the default leaves some experiments unsatisfied, we may be willing to reduce the quality of fit to some experiments in order to fit better another experiment. (However, we use this trick sparingly!)

May 2005CTEQ Summer School10 Example 1. The effect of giving the CCFR F2 data set a heavy weight. By applying weighting factors in the fitting function, we can test the “compatibility” of disparate data sets. 3H1 (a)8.3 7CDHSW F26.3 8NMC F2p CCFR F2  E866 pp5.5 14D0 jet23.5  2  2 (CCFR) =  19.7  2 (other) = Giving a single data set a large weight is tantamount to determining the PDF’s from that data set alone. The result is a significant improvement for that data set but which does not fit the others.

May 2005CTEQ Summer School11 2BCDMS F2d  H1 (a)  H1 (b)  4.3 6ZEUS27.5 7CDHSW F NMC F2p8.0 10CCFR F D0 jet CDHSW F CCFR F35.9 Example 2. Giving heavy weight to H1 and BCDMS  2  2 ( H & B ) =  38.7  2 ( other ) =

May 2005CTEQ Summer School12 Lessons from these reweighting studies  Global analysis requires compromises – the PDF model that gives the best fit to one set of data does not give the best fit to others. This is not surprising because there are systematic differences between the experiments.  The scale of acceptable changes of  2 must be large. Adding a new data set and refitting may increase the  2 ‘s of other data sets by amounts >> 1.

May 2005CTEQ Summer School13 Clever ways to test the compatibility of disparate data sets  Plot  2 versus  2 J Collins and J Pumplin (hep-ph/ )  The Bootstrap Method Efron and Tibshirani, Introduction to the Bootstrap (Chapman&Hall) Chernick, Bootstrap Methods (Wiley)

May 2005CTEQ Summer School14 3/ Uncertainty Analysis

May 2005CTEQ Summer School15 We continue to use  2 global as figure of merit. Explore the variation of  2 global in the neighborhood of the minimum. The Hessian method (  = … d) a1a1 a2a2 the standard fit, minimum  2 nearby points are also acceptable

May 2005CTEQ Summer School16 Classical error formula for a variable X(a) Obtain better convergence using eigenvectors of H  S  (+) and S  (  ) denote PDF sets displaced from the standard set, along the  directions of the  th eigenvector, by distance T =  (  2) in parameter space. Better: Use asymmetric bounds “Master Formula” for the Hessian Method

May 2005CTEQ Summer School17 The 40 eigenvector basis sets – a complete set of alternate PDFs, tolerably near the minimum of  2. S  (+) and S  (  ) denote PDF sets displaced from the standard set, along the  directions of the  th eigenvector, by distance T =  (  2) in parameter space. a1a1 a2a2 ( available in the LHAPDF format : 2d alternate sets )

May 2005CTEQ Summer School18 Minimization of F [ w.r.t {a  } ] gives the best fit for the value X(a min,  ) of the variable X. Hence we trace out a curve of  2 globa l versus X. The Lagrange Multiplier Method … for analyzing the uncertainty of PDF- dependent predictions. The fitting function for constrained fits  : Lagrange multiplier controlled by the parameter

May 2005CTEQ Summer School19 The question of tolerance X : any variable that depends on PDF’s X 0 : the prediction in the standard set  2 (X) : curve of constrained fits For the specified tolerance (  2 = T 2 ) there is a corresponding range of uncertainty,   X. What should we use for T?

May 2005CTEQ Summer School20 Estimation of parameters in Gaussian error analysis would have T = 1 We do not use this criterion.

May 2005CTEQ Summer School21 Aside: The familiar ideal example Consider N measurements {  i } of a quantity  with normal errors {  i } Estimate  by minimization of  2, The mean of  combined is  true, the SD is The proof of this theorem is straightforward. It does not apply to our problem because of systematic errors. and ( =  /  N )

May 2005CTEQ Summer School22 To judge the PDF uncertainty, we return to the individual experiments. Lumping all the data together in one variable –  2 global – is too constraining. Global analysis is a compromise. All data sets should be fit reasonably well -- that is what we check. As we vary {a  }, does any experiment rule out the displacement from the standard set?

May 2005CTEQ Summer School23 In testing the goodness of fit, we keep the normalization factors (i.e., optimized luminosity shifts) fixed as we vary the shape parameters. End result e.g., ~100 for ~2000 data points. This does not contradict the  2 = 1 criterion used by other groups, because that refers to a different  2 in which the normalization factors are continually optimized as the {a  } vary.

May 2005CTEQ Summer School24 Some groups do use the criterion of  2 = 1 for PDF error analysis. Often they are using limited data sets – e.g., an experimental group using only their own data. Then the  2 = 1 criterion may underestimate the uncertainty implied by systematic differences between experiments. An interesting compendium of methods, by R. Thorne CTEQ6  2 = 100 (fixed norms) ZEUS  2 = 50 (effective) MRST01  2 = 20 H1  2 = 1 Alekhin  2 = 1 GKK not using  2