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Entropy2016,9, 337
As expected, onlymoves normal to the trajectorywill change at ïŹrst order the value of the
criterion: thedisplacementof thecurveÎłjwill thusbeperformedat t in thenormalbundle toÎłj and
isgiven,upto the (âNi=1 li) â1 term,by:
â«
Ω (
Îłj(t)âx
âÎłj(t)âxâ )
N KâČ (âÎłj(t)âxâ) log(dË(x))dxâÎłâČj(t)â
â (â«
Ω K (âÎłj(t)âxâ) log(dË(x))dx) ( ÎłâČâČj (t)
âÎłâČj(t)â )
N
+ (â«
Ω dË(x) log(dË(x))dx )( ÎłâČâČj (t)
âÎłâČj(t)â )
N . (19)
TheïŹrst termintheexpressionwill favormoves towardsareasofhighdensity,while thesecond
andthirdonesaremovingalongnormalvectorandwill straightenthe trajectory. This lastpointcanbe
enlightenedbyconsideringthecaseofasingleplanarcurvewithïŹxedendpoints.
Proposition3. Let a,bbeïŹxedpoints inR2 andKbeakernel as in (7). Thesegment [a,b] is a criticalpoint
for the entropyassociatedwith the curve systeminR2 consistingof single smoothpathswith endpoints a,b.
Proof. Let the segment [a,b] be parametrized as Îł: t â [0,1] â a+ tvwith v the vector (bâ a).
Startingwith theexpression(19), it is clear that thesecondandthirdtermsoccurring in the formula
will vanishas thesecondderivativeofÎł is zero. Letube theunitnormalvector toÎł. Anypoint x
inR2 canbewrittenasx= a+Ξv+Οu, Ξ,ΟâR, so
thatÎł(t)âx=(tâΞ)vâΟuandâÎł(t)âxâ=â
(tâΞ)2âbâaâ2+Ο2. Thechangeofvariablesxâ (Ξ,Ο)has Jacobianâvâ= âbâaâ. ForaïŹxed
tâ [0,1], itbecomes:
â«
R2 ( Îł(t)âx
âÎł(t)âxâ )
N KâČ(âÎł(t)âxâ) log(dË(x))dxâÎłâČ(t)â=
âbâaâ2 â«
R â«
R âΟâ
(tâΞ)2âbâaâ2+Ο2K âČ (â
(tâΞ)2âbâaâ2+Ο2 )
log(dË(Ξ,Ο))dΟdΞ. (20)
Thedensity dË for theÎłcurve isexpressed inΟ,Ξ coordinatesas:
â«
[0,1] K (â
(tâΞ)2âbâaâ2+Ο2 )
dt
andisanevenfunction inΟ. Thesameis true forKâČ(âÎł(t)âxâ). Finally, themapping:
Ο â âΟâ
(tâΞ)2âbâaâ2+Ο2
is odd for aïŹxed Ξ, so that thewhole integrand is oddas a functionof Ο. By theFubini theorem,
integratingïŹrst inΟwill thereforeyieldavanishing integral,provingtheassertion.
The result still holds inRq, the only different aspect being that x is now expanded as x =
a+Ξv+â qâ1
i=1 Οiui withui, i = 1,. . . ,qâ1 anorthonormal basis of the orthogonal complement of
Rv inRq. RewritingÎł(t)âx=(tâΞ)vââqâ1i=1 Οiui andâÎł(t)âxâ= â
(tâΞ)2âbâaâ2+âqâ1i=1 Ο2i ,
thesameparityargumentcanbeappliedonanyof thecomponentsΟi, i=1,. . . ,qâ1, showingthat
the integral isvanishing.
Theeffectofcurvestraighteningispresentwhenminimizingtheentropyofawholecurvesystem,
but is counterbalancedbythegatheringeffect.Dependingonthechoiceof thekernelbandwidth,one
or theothereffect isdominant: straightening ispreeminent for lowvalues,beingtheonlyremaining
396
Differential Geometrical Theory of Statistics
- Titel
- Differential Geometrical Theory of Statistics
- Autoren
- Frédéric Barbaresco
- Frank Nielsen
- Herausgeber
- MDPI
- Ort
- Basel
- Datum
- 2017
- Sprache
- englisch
- Lizenz
- CC BY-NC-ND 4.0
- ISBN
- 978-3-03842-425-3
- Abmessungen
- 17.0 x 24.4 cm
- Seiten
- 476
- Schlagwörter
- Entropy, Coding Theory, Maximum entropy, Information geometry, Computational Information Geometry, Hessian Geometry, Divergence Geometry, Information topology, Cohomology, Shape Space, Statistical physics, Thermodynamics
- Kategorien
- Naturwissenschaften Physik