"Like Sir George Cayley's balloon, his own was an
ellipsoid. Its length was thirteen feet six inches - height, six feet eight inches.
To cover several kinds of mismatches together, the adaptive flat
ellipsoid models are introduced in our method as tight as possible.
To avoid both the inconsistency of the basic convex combination and the lack of performance of the covariance intersection method, internal
ellipsoid approximation fusion (IEAF) has been proposed [15].
Obviously, such scatterers will all lie on the surface of an
ellipsoid, with the transmit and receive aircraft located in the foci of this
ellipsoid.
At each sampling instant, the predicted future states on the finite horizon are bounded by using a sequence of
ellipsoids. The terminal
ellipsoid is contained in a target set guaranteeing stability.
For MJS (1), an
ellipsoid set [THETA] = {x [member of] [R.sup.[n.sub.x]] | [x.sup.T.sub.k][P.sub.k]([r.sub.k])[x.sub.k] [less than or equal to] [[gamma].sub.k]} associated with the state is said to be asymptotically mode-dependent stable, if the following holds, whenever [x.sub.[k.sub.0]] [member of] [THETA], then [x.sub.k] [member of] [THETA] for k [greater than or equal to] [k.sub.0] and [x.sub.k] [right arrow] 0 when k [right arrow] [infinity].
Urediniospores subglobose,
ellipsoid or obovoid, yellowish brown, 19-25 x 28-35 (-40) um; wall echinulate, 1-1.5 um; germ pores upto 2, equatorial.
If this problem is extended to three-dimensions, the objective becomes that of finding the radius of a sphere such that the surface areas of the portions of the sphere and an
ellipsoid that are inside one another are equal.
The block model estimate was performed using interpolation according to the inverse of the distance from nearest composites and the
ellipsoid influenced distance in calculation which were adapted for the geology of the deposit by application of the variable direction search
ellipsoid special tool in Genesis software for folded deposits.
Within the area of the OpRegen cell transplant, signs of a reduction and change in drusen material, as well as improvements or possible restorations of the
ellipsoid zone and RPE layers, have persisted.
Where a, b and c are the semi-dimensions of the scalene
ellipsoid l/2, w/2 and t/2 respectively.
Mylonitic rocks formed as a result of heterogeneous shear strain in the ductile shear zone, and their fabric directly related to the strain rate, finite strain
ellipsoid shape and orientation (Watts and Williams, 1983; Zhang et al., 2010; Mulchrone and Talbot, 2014; Fossen and Cavalcante, 2017).