Test functions
Rana
The Rana function is a non-separable, highly multimodal function.
The left figure shows the two dimensional landscape of the non-rotated version.
The best solutions are at the corners.
Applying a simple parameter shift makes
this function non-symmetric. The right figure shows the rotated version.
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F101
Like the Rana function, F101 is a non-separable and highly multimodal.
The left figure shows the two dimensional non-rotated landscape.
The right landscape has been rotated 20 degrees.
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Schwefel
The schwefel function is symmetric, separable and multimodal (left).
Rotating this function creates a non-separable surface with similar features (Salomon 1996).
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Rosenbrock
Rosenbrock's function is symmetric, unimodal and non-separable.
The long narrow ridge makes this problem difficult for some algorithms.
Rotation makes this problem easier for most algorithms.
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Static Corrections
There are many difficult optimization problems in geophysics.
One such problem is the ``static corrections'' problem, where
seismic reflection surveys are used to construct subsurface
images of geologic strata.
We introduce a synthetic static correction problem as
a test function.
The figure below shows a single trial of CHC on this problem.
Notice that the target profile is not actually the optimal
solution.
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