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Entropy2016,9, 337 with1Uk thecharacteristic functionof thesetUk. It seemsnatural toextendthedensityobtainedfrom samples toanotheronebasedonthe trajectories themselvesusinganintegral form: dk=Ī»āˆ’1 N āˆ‘ i=1 ∫ 1 0 1Uk (γi(t))dt (2) where thenormalizingconstantĪ» is chosensothatdk isadiscreteprobabilitydistribution: Ī»= P āˆ‘ k=1 N āˆ‘ i=1 ∫ 1 0 1Uk (γi(t))dt= N āˆ‘ i=1 ∫ 1 0 P āˆ‘ k=1 1Uk (γi(t))dt andsinceUk,k=1,. . . ,P isapartition: P āˆ‘ k=1 1Uk (γi(t))=1 (3) so thatĪ»=N. Densitycanbeviewedasanempiricalprobabilitydistributionwith theUk consideredasbins inanhistogram. It is thusnatural toextendtheabovecomputationsoas togiverise toacontinuous distributiononĪ©. For thatpurpose, localweighting techniques, suchaskerneldensityestimation methods, arewell known in nonparametric statistics, because they are a useful data-drivenway toyield continuousdensity estimation. Many referencesmaybe found in the literature as in [5,6]. Giventheobservations, theresultingestimationwillbe thesumofweights taking intoaccount the distancebetweentheobservationsandthelocationxatwhichthedensityhastobeestimated; themore an observation is close to x, the greater is theweighting. Theweights are definedby selecting a summable functioncenteredontheobservations, calledakernel,usuallydenotedbyK :R→R+ in theunivariatecase,andasmoothedversionof theParzen–Rosenblattdensityestimator [7,8] isused. Standardchoices for theK functionare theonesusedfornonparametrickernelestimation, like the Epanechnikovfunction[9]: K : x → ( 1āˆ’x2 ) 1[āˆ’1,1](x). There exists a large variety of kernel functions, and any density function satisfying the normalizationconditioncanbeconsidered, so that theestimation isaprobabilitydensity.Moreover, thekernel function isasymmetricpositive function,with thefirstmomentequal tozeroandafinite secondordermoment. In themultivariatecase,amultivariatekernel functionK :Rq→R+ is selected that can be expressed bymeans of a real kernelK associatedwith a norm, denoted by ‖.‖, inRq as follows: K(x)=K(‖x‖), x∈Rq. Thenormalizationconditionbecomes:∫ Rq K(x)dx= ∫ Rq K(‖x‖)dx=1. Akernelversionof thedensity is thendefinedasamappingd fromĪ© to [0,1]: d: x → āˆ‘ N i=1 ∫1 0 K(‖xāˆ’Ī³i(t)‖)dt āˆ‘Ni=1 ∫ Ī© ∫1 0 K(‖xāˆ’Ī³i(t)‖)dtdx . (4) Normalizingthekernel isnotmandatory,as thenormalizationoccurswiththedefinitionofd. It is neverthelesseasier toconsider thesekindsofkernels, as isdone innonparametricdensityestimation. 389
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Differential Geometrical Theory of Statistics
Title
Differential Geometrical Theory of Statistics
Authors
FrƩdƩric Barbaresco
Frank Nielsen
Editor
MDPI
Location
Basel
Date
2017
Language
English
License
CC BY-NC-ND 4.0
ISBN
978-3-03842-425-3
Size
17.0 x 24.4 cm
Pages
476
Keywords
Entropy, Coding Theory, Maximum entropy, Information geometry, Computational Information Geometry, Hessian Geometry, Divergence Geometry, Information topology, Cohomology, Shape Space, Statistical physics, Thermodynamics
Categories
Naturwissenschaften Physik
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Differential Geometrical Theory of Statistics