Given a "density" scalar field in the plane, how can I divide the plane into nice (low moment of inertia) regions so that each region contains a similar amount of "mass"?
That's not the best description of what my actual problem is, but it's the most concise phrasing I could think of.
I have a large map of a fictional world for use in a game. I have a pretty good idea of approximately how far one could walk in a day from any given point on this map, and this varies greatly based on the terrain etc. I would like to represent this information by dividing the map into regions, so that one day of walking could take you from any region to any of its neighboring regions. It doesn't have to be perfect, but it should be significantly better than simply dividing the map into a hexagonal grid (which is what many games do).
I had the idea that I could create a gray-scale image with the same dimensions as the map, where each pixel's color value represents how quickly one can travel through the pixel in the same place on the map. Well-maintained roads would be encoded as white pixels, and insurmountable cliffs would be encoded as black, or something like that.
My question is this: does anyone have an idea of how to use such a gray-scale image (the "density" scalar field) to generate my "grid" from the previous paragraph (regions of similar "mass")?
I've thought about using the gray-scale image as a discrete probability distribution, from which I can generate a bunch of coordinates, and then use some sort of clustering algorithm to create the regions, but a) the clustering algorithms would have to create clusters of a similar size, I think, for that idea to work, which I don't think they usually do, and b) I barely have any idea if any of that even makes sense, as I'm way out of my comfort zone here.
Sorry if this doesn't belong here, my idea has always been to solve it programatically somehow, so this seemed the most sensible place to ask.
UPDATE: Just thought I'd share the results I've gotten so far, trying out the second approach suggested by #samgak - recursively subdividing regions into boxes of similar mass, finding the center of mass of each region, and creating a voronoi diagram from those.
I'll keep tweaking, and maybe try to find a way to make it less grid-like (like in the upper right corner), but this worked way better than I expected!
Building upon #samgak's solution, if you don't want the grid-like structure, you can just add a small random perturbation to your centers. You can see below for example the difference I obtain:
without perturbation
adding some random perturbation
A couple of rough ideas:
You might be able to repurpose a color-quantization algorithm, which partitions color-space into regions with roughly the same number of pixels in them. You would have to do some kind of funny mapping where the darker the pixel in your map, the greater the number of pixels of a color corresponding to that pixel's location you create in a temporary image. Then you quantize that image into x number of colors and use their color values as co-ordinates for the centers of the regions in your map, and you could then create a voronoi diagram from these points to define your region boundaries.
Another approach (which is similar to how some color quantization algorithms work under the hood anyway) could be to recursively subdivide regions of your map into axis-aligned boxes by taking each rectangular region and choosing the optimal splitting line (x or y) and position to create 2 smaller rectangles of similar "mass". You would end up with a power of 2 count of rectangular regions, and you could get rid of the blockiness by taking the centre of mass of each rectangle (not simply the center of the bounding box) and creating a voronoi diagram from all the centre-points. This isn't guaranteed to create regions of exactly equal mass, but they should be roughly equal. The algorithm could be improved by allowing recursive splitting along lines of arbitrary orientation (or maybe a finite number of 8, 16, 32 etc possible orientations) but of course that makes it more complicated.
Multiple points on a 2D plane are given. They represent a window frame of mostly rectangular form with some possible variations. The points which are part of each side are not guaranteed to form a perfect line. Each side of the window should be measured.
A rotating electronic device attached to a window measures the distance in all directions providing a 360 degree measurements. By using the rotation angle and the distance, a set of points are plotted on a 2D coordinate system. So far so good.
Now comes the harder part. The measured window frame could have some variations. The points should be converted to straight lines and the length of each line should be measured.
I imagine that the following steps are required:
Group the different points into straights lines. This means approximating each line “between” the points that form it.
Drawing those lines, getting rid of the separate points used to construct the lines.
Find the points where each two lines intersect.
Measure the distance between those points. However not all distances between all points are interesting. For example diagonals within a frame are irrelevant.
Any Java libraries dealing with geometry that could solve the problem are acceptable. I will write the solution in Kotlin/Java, but any algorithmic insights or code examples and ideas in any other languages or pseudo code are welcome.
Thank you in advance!
New Image
I would solve this in 2 stages:
Data cleaning: round the location (X, Y) of each point to its nearest multiple of N (vary N for varying degrees of precision)
Apply the gift-wrapping algorithm (also known as Jarvis March)
You now have only those points that are not co-linear, and the lines between them, and the order in which they need to be traversed to form the perimeter.
Iterate over the points in order, take point Px and P(x+1), and calculate the distance between them.
Contour lines (aka isolines) are curves that trace constant values across a 2D scalar field. For example, in a geographical map you might have contour lines to illustrate the elevation of the terrain by showing where the elevation is constant. In this case, let's store contour lines as lists of points on the map.
Suppose you have map that has several contour lines at known elevations, and otherwise you know nothing about the elevations of the map. What algorithm would you use to fill in additional contour lines to approximate the unknown elevations of the map, assuming the landscape is continuous and doesn't do anything surprising?
It is easy to find advise about interpolating the elevation of an individual point using contour lines. There are also algorithms like Marching Squares for turning point elevations into contour lines, but none of these exactly capture this use case. We don't need the elevation of any particular point; we just want the contour lines. Certainly we could solve this problem by filling an array with estimated elevations and then using Marching Squares to estimate the contour lines based on the array, but the two steps of that process seem unnecessarily expensive and likely to introduce artifacts. Surely there is a better way.
IMO, about all methods will amount to somehow reconstructing the 3D surface by interpolation, even if implicitly.
You may try by flattening the curves (turning them to polylines) and triangulating the resulting polygons thay they will define. (There will be a step of closing the curves that end on the border of the domain.)
By intersection of the triangles with a new level (unsing linear interpolation along the sides), you will obtain new polylines corresponding to new isocurves. Notice that the intersections with the old levels recreates the old polylines, which is sound.
You may apply a post-smoothing to the curves, but you will have no guarantee to retrieve the original old curves and cannot prevent close surves to cross each other.
Beware that increasing the density of points along the curves will give you a false feeling of accuracy, as the error due to the spacing of the isolines will remain (indeed the reconstructed surface will be cone-like, with one of the curvatures being null; the surface inside the bottommost and topmost lines will be flat).
Alternatively to using flat triangles, one may think of a scheme where you compute a gradient vector at every vertex (f.i. from a least square fit of a plane on the vertex and its neighbors), and use this information to generate a bivariate polynomial surface in the triangle. You must do this in such a way that the values along a side will coincide for the two triangles that share it. (Unfortunately, I have no formula to give you.)
The isolines are then obtained by a further subdivision of the triangle in smaller triangles, with a flat approximation.
Actually, this is not very different from getting sample points, (Delaunay) triangulating them and fitting picewise continuous patches to the triangles.
Whatever method you will use, be it 2D or 3D, it is useful to reason on what happens if you sweep the range of z values in a continous way. This thought experiment does reconstruct a 3D surface, which will possess continuity and smoothness properties.
A possible improvement over the crude "flat triangulation" model could be to extend every triangle side between to iso-polylines with sides leading to the next iso-polylines. This way, higher order interpolation (cubic) can be achieved, giving a smoother reconstruction.
Anyway, you can be sure that this will introduce discontinuities or other types of artifacts.
A mixed method:
flatten the isolines to polylines;
triangulate the poygons formed by the polylines and the borders;
on every node, estimate the surface gradient (least-square fit of a plane to the node and its neighborrs);
in every triangle, consider the two sides along which you need to interpolate and compute the derivative at endpoints (from the known gradients and the side directions);
use Hermite interpolation along these sides and solve for the desired iso-levels;
join the points obtained on both sides.
This method should be a good tradeoff between complexity and smoothness. It does reconstruct a continuous surface (except maybe for the remark below).
Note that is some cases, yo will obtain three solutions of the cubic. If there are three on each side, join them in order. Otherwise, make a decision on which to join and use the remaining two to close the curve.
Given a set of 2D points, I want to calculate a measure of how horizontally symmetrical and vertically symmetrical those points are.
Alternatively, for each set of points I will also have a rasterised image of the lines between those points, so is there any way to calculate a measure of symmetry for images?
BTW, this is for use in a feature vector that will be presented to a neural network.
Clarification
The image on the left is 'horizontally' symmetrical. If we imagine a vertical line running down the middle of it, the left and right parts are symmetrical. Likewise, the image on the right is 'vertically' symmetrical, if you imagine a horizontal line running across its center.
What I want is a measure of just how horizontally symmetrical they are, and another of just how vertically symmetrical they are.
This is just a guideline / idea, you'll need to work out the details:
To detect symmetry with respect to horizontal reflection:
reflect the image horizontally
pad the original (unreflected) image horizontally on both sides
compute the correlation of the padded and the reflected images
The position of the maximum in the result of the correlation will give you the location of the axis of symmetry. The value of the maximum will give you a measure of the symmetry, provided you do a suitable normalization first.
This will only work if your images are "symmetric enough", and it works for images only, not sets of points. But you can create an image from a set of points too.
Leonidas J. Guibas from Stanford University talked about it in ETVC'08.
Detection of Symmetries and Repeated Patterns in 3D Point Cloud Data.
I've been working on a visualization project for 2-dimensional continuous data. It's the kind of thing you could use to study elevation data or temperature patterns on a 2D map. At its core, it's really a way of flattening 3-dimensions into two-dimensions-plus-color. In my particular field of study, I'm not actually working with geographical elevation data, but it's a good metaphor, so I'll stick with it throughout this post.
Anyhow, at this point, I have a "continuous color" renderer that I'm very pleased with:
The gradient is the standard color-wheel, where red pixels indicate coordinates with high values, and violet pixels indicate low values.
The underlying data structure uses some very clever (if I do say so myself) interpolation algorithms to enable arbitrarily deep zooming into the details of the map.
At this point, I want to draw some topographical contour lines (using quadratic bezier curves), but I haven't been able to find any good literature describing efficient algorithms for finding those curves.
To give you an idea for what I'm thinking about, here's a poor-man's implementation (where the renderer just uses a black RGB value whenever it encounters a pixel that intersects a contour line):
There are several problems with this approach, though:
Areas of the graph with a steeper slope result in thinner (and often broken) topo lines. Ideally, all topo lines should be continuous.
Areas of the graph with a flatter slope result in wider topo lines (and often entire regions of blackness, especially at the outer perimeter of the rendering region).
So I'm looking at a vector-drawing approach for getting those nice, perfect 1-pixel-thick curves. The basic structure of the algorithm will have to include these steps:
At each discrete elevation where I want to draw a topo line, find a set of coordinates where the elevation at that coordinate is extremely close (given an arbitrary epsilon value) to the desired elevation.
Eliminate redundant points. For example, if three points are in a perfectly-straight line, then the center point is redundant, since it can be eliminated without changing the shape of the curve. Likewise, with bezier curves, it is often possible to eliminate cetain anchor points by adjusting the position of adjacent control points.
Assemble the remaining points into a sequence, such that each segment between two points approximates an elevation-neutral trajectory, and such that no two line segments ever cross paths. Each point-sequence must either create a closed polygon, or must intersect the bounding box of the rendering region.
For each vertex, find a pair of control points such that the resultant curve exhibits a minimum error, with respect to the redundant points eliminated in step #2.
Ensure that all features of the topography visible at the current rendering scale are represented by appropriate topo lines. For example, if the data contains a spike with high altitude, but with extremely small diameter, the topo lines should still be drawn. Vertical features should only be ignored if their feature diameter is smaller than the overall rendering granularity of the image.
But even under those constraints, I can still think of several different heuristics for finding the lines:
Find the high-point within the rendering bounding-box. From that high point, travel downhill along several different trajectories. Any time the traversal line crossest an elevation threshold, add that point to an elevation-specific bucket. When the traversal path reaches a local minimum, change course and travel uphill.
Perform a high-resolution traversal along the rectangular bounding-box of the rendering region. At each elevation threshold (and at inflection points, wherever the slope reverses direction), add those points to an elevation-specific bucket. After finishing the boundary traversal, start tracing inward from the boundary points in those buckets.
Scan the entire rendering region, taking an elevation measurement at a sparse regular interval. For each measurement, use it's proximity to an elevation threshold as a mechanism to decide whether or not to take an interpolated measurement of its neighbors. Using this technique would provide better guarantees of coverage across the whole rendering region, but it'd be difficult to assemble the resultant points into a sensible order for constructing paths.
So, those are some of my thoughts...
Before diving deep into an implementation, I wanted to see whether anyone else on StackOverflow has experience with this sort of problem and could provide pointers for an accurate and efficient implementation.
Edit:
I'm especially interested in the "Gradient" suggestion made by ellisbben. And my core data structure (ignoring some of the optimizing interpolation shortcuts) can be represented as the summation of a set of 2D gaussian functions, which is totally differentiable.
I suppose I'll need a data structure to represent a three-dimensional slope, and a function for calculating that slope vector for at arbitrary point. Off the top of my head, I don't know how to do that (though it seems like it ought to be easy), but if you have a link explaining the math, I'd be much obliged!
UPDATE:
Thanks to the excellent contributions by ellisbben and Azim, I can now calculate the contour angle for any arbitrary point in the field. Drawing the real topo lines will follow shortly!
Here are updated renderings, with and without the ghetto raster-based topo-renderer that I've been using. Each image includes a thousand random sample points, represented by red dots. The angle-of-contour at that point is represented by a white line. In certain cases, no slope could be measured at the given point (based on the granularity of interpolation), so the red dot occurs without a corresponding angle-of-contour line.
Enjoy!
(NOTE: These renderings use a different surface topography than the previous renderings -- since I randomly generate the data structures on each iteration, while I'm prototyping -- but the core rendering method is the same, so I'm sure you get the idea.)
Here's a fun fact: over on the right-hand-side of these renderings, you'll see a bunch of weird contour lines at perfect horizontal and vertical angles. These are artifacts of the interpolation process, which uses a grid of interpolators to reduce the number of computations (by about 500%) necessary to perform the core rendering operations. All of those weird contour lines occur on the boundary between two interpolator grid cells.
Luckily, those artifacts don't actually matter. Although the artifacts are detectable during slope calculation, the final renderer won't notice them, since it operates at a different bit depth.
UPDATE AGAIN:
Aaaaaaaand, as one final indulgence before I go to sleep, here's another pair of renderings, one in the old-school "continuous color" style, and one with 20,000 gradient samples. In this set of renderings, I've eliminated the red dot for point-samples, since it unnecessarily clutters the image.
Here, you can really see those interpolation artifacts that I referred to earlier, thanks to the grid-structure of the interpolator collection. I should emphasize that those artifacts will be completely invisible on the final contour rendering (since the difference in magnitude between any two adjacent interpolator cells is less than the bit depth of the rendered image).
Bon appetit!!
The gradient is a mathematical operator that may help you.
If you can turn your interpolation into a differentiable function, the gradient of the height will always point in the direction of steepest ascent. All curves of equal height are perpendicular to the gradient of height evaluated at that point.
Your idea about starting from the highest point is sensible, but might miss features if there is more than one local maximum.
I'd suggest
pick height values at which you will draw lines
create a bunch of points on a fine, regularly spaced grid, then walk each point in small steps in the gradient direction towards the nearest height at which you want to draw a line
create curves by stepping each point perpendicular to the gradient; eliminate excess points by killing a point when another curve comes too close to it-- but to avoid destroying the center of hourglass like figures, you might need to check the angle between the oriented vector perpendicular to the gradient for both of the points. (When I say oriented, I mean make sure that the angle between the gradient and the perpendicular value you calculate is always 90 degrees in the same direction.)
In response to your comment to #erickson and to answer the point about calculating the gradient of your function. Instead of calculating the derivatives of your 300 term function you could do a numeric differentiation as follows.
Given a point [x,y] in your image you could calculate the gradient (direction of steepest decent)
g={ ( f(x+dx,y)-f(x-dx,y) )/(2*dx),
{ ( f(x,y+dy)-f(x,y-dy) )/(2*dy)
where dx and dy could be the spacing in your grid. The contour line will run perpendicular to the gradient. So, to get the contour direction, c, we can multiply g=[v,w] by matrix, A=[0 -1, 1 0] giving
c = [-w,v]
Alternately, there is the marching squares algorithm which seems appropriate to your problem, although you may want to smooth the results if you use a coarse grid.
The topo curves you want to draw are isosurfaces of a scalar field over 2 dimensions. For isosurfaces in 3 dimensions, there is the marching cubes algorithm.
I've wanted something like this myself, but haven't found a vector-based solution.
A raster-based solution isn't that bad, though, especially if your data is raster-based. If your data is vector-based too (in other words, you have a 3D model of your surface), you should be able to do some real math to find the intersection curves with horizontal planes at varying elevations.
For a raster-based approach, I look at each pair of neighboring pixels. If one is above a contour level, and one is below, obviously a contour line runs between them. The trick I used to anti-alias the contour line is to mix the contour line color into both pixels, proportional to their closeness to the idealized contour line.
Maybe some examples will help. Suppose that the current pixel is at an "elevation" of 12 ft, a neighbor is at an elevation of 8 ft, and contour lines are every 10 ft. Then, there is a contour line half way between; paint the current pixel with the contour line color at 50% opacity. Another pixel is at 11 feet and has a neighbor at 6 feet. Color the current pixel at 80% opacity.
alpha = (contour - neighbor) / (current - neighbor)
Unfortunately, I don't have the code handy, and there might have been a bit more to it (I vaguely recall looking at diagonal neighbors too, and adjusting by sqrt(2) / 2). I hope this enough to give you the gist.
It occurred to me that what you're trying to do would be pretty easy to do in MATLAB, using the contour function. Doing things like making low-density approximations to your contours can probably be done with some fairly simple post-processing of the contours.
Fortunately, GNU Octave, a MATLAB clone, has implementations of the various contour plotting functions. You could look at that code for an algorithm and implementation that's almost certainly mathematically sound. Or, you might just be able to offload the processing to Octave. Check out the page on interfacing with other languages to see if that would be easier.
Disclosure: I haven't used Octave very much, and I haven't actually tested it's contour plotting. However, from my experience with MATLAB, I can say that it will give you almost everything you're asking for in just a few lines of code, provided you get your data into MATLAB.
Also, congratulations on making a very VanGough-esque slopefield plot.
I always check places like http://mathworld.wolfram.com before going to deep on my own :)
Maybe their curves section would help? Or maybe the entry on maps.
compare what you have rendered with a real-world topo map - they look identical to me! i wouldn't change a thing...
Write the data out as an HGT file (very simple digital elevation data format used by USGS) and use the free and open-source gdal_contour tool to create contours. That works very well for terrestrial maps, the constraint being that the data points are signed 16-bit numbers, which fits the earthly range of heights in metres very well, but may not be enough for your data, which I assume not to be a map of actual terrain - although you do mention terrain maps.
I recommend the CONREC approach:
Create an empty line segment list
Split your data into regular grid squares
For each grid square, split the square into 4 component triangles:
For each triangle, handle the cases (a through j):
If a line segment crosses one of the cases:
Calculate its endpoints
Store the line segment in the list
Draw each line segment in the line segment list
If the lines are too jagged, use a smaller grid. If the lines are smooth enough and the algorithm is taking too long, use a larger grid.