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backgrounds.md

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Generic backrgound models

Here is incomplete list of background-like models - the models that often could be used to describe the background distribution

Polynomial models

Here the list of the most useful polynomial models:

  • PolyPos_pdf : positive (non-negative) polynomial
  • PolyEven_pdf : positibe (non-negative) symmetric polynomial: p(x)= p(2*x0-x), where x0=0.5*(xmin+xmax)
  • Monotonic_pdf : positive (non-negative) polynomial with fixed sign of the first derivative: posynomial either non-decreasing or non-increasing
  • Convex_pdf : positive (non-negative) polynomial with fixed signs of the first (non-decreasing or non-increasing) and second (convex or concave) derivatives
  • ConvexOnly_pdf : positive (non-negative) polynomial with fixed sign of the second (convex or concave) derivative

Phasespace-based models

Here the list of the most useful phasespace-based models:

  • PS2_pdf : 2-body phase space (no parameters)
  • PSLeft_pdf : Low edge of N-body phase space
  • PSRight_pdf : High edge of L-body phase space from N-body decays
  • PSNL_pdf : approximation for L-body phase space from N-body decays
  • PS23L_pdf : 2-body phase space from 3-body decays with orbital momenta

Polynomial-based models

  • Bkg_pdf : The exponential function, modulated by the positive polynomial. In practice it is the most useful function to describe the combinatorial background
  • PSPol_pdf : L-body phase space from N-body decays modulated by a positive polynomial
  • Sigmoid_pdf : sigmoid function (atanh) modulated by the positive polynomial
  • TwoExpoPoly_pdf : difference of two exponents, modulated by the positive polynomial

Spline-based models

The models, based on B-splines :

  • PSpline_pdf : positive (non-negative) spline
  • MSpline_pdf : positive (non-negative) monothonic (non-decreasing or non-increasing) spline
  • CSpline_pdf : positive (non-negative) monothonic (non-decreasing or non-inclreasing) convex or concave spline
  • CPSpline_pdf : positive (non-negative) convex or concave spline