1994
DOI: 10.1016/0165-1684(94)90059-0
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Watershed of a continuous function

Abstract: The notion of watershed, used in morphological segmentation, has only a digital definition. In this paper, we propose to extend this definition to the continuous plane. Using this continuous definition, we present the watershed differences with classical edge detectors. We then present a metric in the plane for which the watershed is a skeleton by influence zones and show the lower semicontinuous behaviour of the associated skeleton. This theoretical approach suggests an algorithm for solving the eikonal equat… Show more

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Cited by 249 publications
(164 citation statements)
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“…It must be specify that here the standard framework of watershed transform based on the flooding algorithm is adopted despite to there are other alternative frameworks based on a continuous formulation using topographic distance [25,26]; the topological watershed based on discrete geometry tools [27,28]; graph-based watershed using minimum spanning-tree algorithms [29,30]; the power watershed algorithm [31]; the viscous watershed [32]; etc.…”
Section: Introductionmentioning
confidence: 99%
“…It must be specify that here the standard framework of watershed transform based on the flooding algorithm is adopted despite to there are other alternative frameworks based on a continuous formulation using topographic distance [25,26]; the topological watershed based on discrete geometry tools [27,28]; graph-based watershed using minimum spanning-tree algorithms [29,30]; the power watershed algorithm [31]; the viscous watershed [32]; etc.…”
Section: Introductionmentioning
confidence: 99%
“…(12)) is di!erent from the one proposed in [15] which constituted the basis for the dynamics of contours. In [15] the use of the line integral expresses a measure of the work needed to move a point a towards another point b, following a steepest descent path.…”
Section: Minimum Cost Path Saliencymentioning
confidence: 99%
“…(12)) is di!erent from the one proposed in [15] which constituted the basis for the dynamics of contours. In [15] the use of the line integral expresses a measure of the work needed to move a point a towards another point b, following a steepest descent path. For this purpose, the gradient vector "eld is used to combine the work calculation and the notion of topographic distance, as introduced in [13].…”
Section: Minimum Cost Path Saliencymentioning
confidence: 99%
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“…In the continuous domain and assuming that the image is smooth and has isolated critical points, the continuous watershed is equivalent to finding a skeleton by influence zones with respect to a weighted distance function that uses points in the regional minima of the image as sources and η = ||∇f || as the field of indices [9,7]. If other markers different than the minima are to be used as sources, then the homotopy of the function must be modified via morphological reconstruction to impose these markers as the only minima.…”
Section: Continuous Watershed and Eikonal Pdementioning
confidence: 99%