I am working on a geographic project in Java.
The input are coordinates : 24.4444 N etc
Output: a PLAIN map (not round) showing the point of the coordinates.
I don't know the algorithm to transform from coordinates to x,y on a JComponent, can somebody help me?
The map looks like this:
http://upload.wikimedia.org/wikipedia/commons/7/74/Mercator-projection.jpg
Thank you
Given your sparse example, the range of your inputs will be (90.0N - 90.0S) and (180W - 180E). It is easiest - and standard - if you convert South and West to negatives giving you latitudes of (90.0..-90.0) and longitudes of (180.0..-180.0).
Given the size of your canvas - let's say it is 140x120 pixels - you get:
x = (latitude * canvas_height / 180.0) + (canvas_height / 2)
y = (longitude * canvas_width / 360.0) + (canvas_width / 2)
or:
x = (longitude * 120.0 / 180.0) + (120/2)
y = (latitude * 140.0 / 360.0) + (140/2)
where I have ordered the operations to minimize rounding error. This assumes the canvas has point (0,0) in the upper-left or, if not, that you are Australian.
Added: you just threw in the bit about Mercator projections making my simple answer incorrect (but possibly still usable by you if you don't actually care about projection)
MSW provided a good example. Ultimately the algorithm depends on the map projection used. Here are a couple of good resources I used in the past.
The following link is a good reference to a number of different map projections with enough math formulas to choke a horse.
http://www.remotesensing.org/geotiff/proj_list/
Here is a decent reference for doing this in PhP. While not Java, it should be straight forward enough to apply the principles outlined.
http://www.web-max.ca/PHP/article_1.php
Related
I'm trying to recreate a map of the Netherlands from Mike Bostock's tutorial. I get the first step done and actually see the smaller map. But when I go to the second step and try to change the projection everything is blank. Is it possible that this is caused by the data including the Dutch Antilles? They are so far it apart that I might be looking at the ocean?
My files
It seems to me that setting the center attribute on the projection was messing things up, it might be because your data was crossing date line? I notice the the bounding box stretch way off to the south and west.
My approach was to set the scale and translation based on one of the centrally located provinces. The scale and translation were automatically calculated based on Mike's code in this stack overflow question. The idea is to use a unit projection and then to calculate the bounds of a given feature. These bounds are then used to calculate appropriate scale and translation (avoiding using the center attribute). The projection is then updated using the recalculated scale and transform.
The relevant code is:
//select a province to center on
var l = topojson.feature(nld, nld.objects.subunits).features[8],
//calculate the bounds
b = path.bounds(l),
//calculate the scale based on the bounds (note that I've set the proportion to
//less than one so you can see all of the Netherlands)
s = .125 / Math.max((b[1][0] - b[0][0]) / width, (b[1][1] - b[0][1]) / height),
//calculate the translation based on the bounds
t = [(width - s * (b[1][0] + b[0][0])) / 2, (height - s * (b[1][1] + b[0][1])) / 2];
//update the projection
projection
.scale(s)
.translate(t);
And you can find an example here
I'm trying to deduct the 2D-transformation parameters from the result.
Given is a large number of samples in an unknown X-Y-coordinate system as well as their respective counterparts in WGS84 (longitude, latitude). Since the area is small, we can assume the target system to be flat, too.
Sadly I don't know which order of scale, rotate, translate was used, and I'm not even sure if there were 1 or 2 translations.
I tried to create a lengthy equation system, but that ended up too complex for me to handle. Basic geometry also failed me, as the order of transformations is unknown and I would have to check every possible combination order.
Is there a systematic approach to this problem?
Figuring out the scaling factor is easy, just choose any two points and find the distance between them in your X-Y space and your WGS84 space and the ratio of them is your scaling factor.
The rotations and translations is a little trickier, but not nearly as difficult when you learn that the result of applying any number of rotations or translations (in 2 dimensions only!) can be reduced to a single rotation about some unknown point by some unknown angle.
Suddenly you have N points to determine 3 unknowns, the axis of rotation (x and y coordinate) and the angle of rotation.
Calculating the rotation looks like this:
Pr = R*(Pxy - Paxis_xy) + Paxis_xy
Pr is your rotated point in X-Y space which then needs to be converted to WGS84 space (if the axes of your coordinate systems are different).
R is the familiar rotation matrix depending on your rotation angle.
Pxy is your unrotated point in X-Y space.
Paxis_xy is the axis of rotation in X-Y space.
To actually find the 3 unknowns, you need to un-scale your WGS84 points (or equivalently scale your X-Y points) by the scaling factor you found and shift your points so that the two coordinate systems have the same origin.
First, finding the angle of rotation: take two corresponding pairs of points P1, P1' and P2, P2' and write out
P1' = R(P1-A) + A
P2' = R(P2-A) + A
where I swapped A = Paxis_xy for brevity. Subtracting the two equations gives:
P2'-P1' = R(P2-P1)
B = R * C
Bx = cos(a) * Cx - sin(a) * Cy
By = cos(a) * Cx + sin(a) * Cy
By + Bx = 2 * cos(a) * Cx
(By + Bx) / (2 * Cx) = cos(a)
...
(By - Bx) / (2 * Cy) = sin(a)
a = atan2(sin(a), cos(a)) <-- to get the right quadrant
And you have your angle, you can also do a quick check that cos(a) * cos(a) + sin(a) * sin(a) == 1 to make sure either you got all the calculations correct or that your system really is an orientation-preserving isometry (consists only of translations and rotations).
Now that we know a we know R and so to find A we do:
P1` = R(P1-A) + A
P1' - R*P1 = (I-R)A
A = (inverse(I-R)) * (P1' - R*P1)
where the inversion of a 2x2 matrix is easy.
EDIT: There is an error in the above, or more specifically one case that needs to be treated separately.
There is one combination of translations and rotations that does not reduce to a single rotation and that is a single translation. You can think of it in terms of fixed points (how many points are unchanged after the operation).
A translation has no fixed points (all points are changed) and a rotation has 1 fixed point (the axis doesn't change). It turns out that two rotations leave 1 fixed point and a translation and a rotation leaves 1 fixed point, which (with a little proof that says the number of fixed points tells you the operation performed) is the reason that arbitrary combinations of these result in a single rotation.
What this means for you is that if your angle comes out as 0 then using the method above will give you A = 0 as well, which is likely incorrect. In this case you have to do A = P1' - P1.
If I understood the question correctly, you have n points (X1,Y1),...,(Xn,Yn), the corresponding points, say, (x1,y1),...,(xn,yn) in another coordinate system, and the former are supposedly obtained from the latter by rotation, scaling and translation.
Note that this data does not determine the fixed point of rotation / scaling, or the order in which the operations "should" be applied. On the other hand, if you know these beforehand or choose them arbitrarily, you will find a rotation, translation and scaling factor that transform the data as supposed to.
For example, you can pick an any point, say, p0 = [X1, Y1]T (column vector) as the fixed point of rotation & scaling and subtract its coordinates from those of two other points to get p2 = [X2-X1, Y2-Y1]T, and p3 = [X3-X1, Y3-Y1]T. Also take the column vectors q2 = [x2-x1, y2-y1]T, q3 = [x3-x1, y3-y1]T. Now [p2 p3] = A*[q2 q3], where A is an unknwon 2x2 matrix representing the roto-scaling. You can solve it (unless you were unlucky and chose degenerate points) as A = [p2 p3] * [q2 q3]-1 where -1 denotes matrix inverse (of the 2x2 matrix [q2 q3]). Now, if the transformation between the coordinate systems really is a roto-scaling-translation, all the points should satisfy Pk = A * (Qk-q0) + p0, where Pk = [Xk, Yk]T, Qk = [xk, yk]T, q0=[x1, y1]T, and k=1,..,n.
If you want, you can quite easily determine the scaling and rotation parameter from the components of A or combine b = -A * q0 + p0 to get Pk = A*Qk + b.
The above method does not react well to noise or choosing degenerate points. If necessary, this can be fixed by applying, e.g., Principal Component Analysis, which is also just a few lines of code if MATLAB or some other linear algebra tools are available.
I have two sets of 3D points (original and reconstructed) and correspondence information about pairs - which point from one set represents the second one. I need to find 3D translation and scaling factor which transforms reconstruct set so the sum of square distances would be least (rotation would be nice too, but points are rotated similarly, so this is not main priority and might be omitted in sake of simplicity and speed). And so my question is - is this solved and available somewhere on the Internet? Personally, I would use least square method, but I don't have much time (and although I'm somewhat good at math, I don't use it often, so it would be better for me to avoid it), so I would like to use other's solution if it exists. I prefer solution in C++, for example using OpenCV, but algorithm alone is good enough.
If there is no such solution, I will calculate it by myself, I don't want to bother you so much.
SOLUTION: (from your answers)
For me it's Kabsch alhorithm;
Base info: http://en.wikipedia.org/wiki/Kabsch_algorithm
General solution: http://nghiaho.com/?page_id=671
STILL NOT SOLVED:
I also need scale. Scale values from SVD are not understandable for me; when I need scale about 1-4 for all axises (estimated by me), SVD scale is about [2000, 200, 20], which is not helping at all.
Since you are already using Kabsch algorithm, just have a look at Umeyama's paper which extends it to get scale. All you need to do is to get the standard deviation of your points and calculate scale as:
(1/sigma^2)*trace(D*S)
where D is the diagonal matrix in SVD decomposition in the rotation estimation and S is either identity matrix or [1 1 -1] diagonal matrix, depending on the sign of determinant of UV (which Kabsch uses to correct reflections into proper rotations). So if you have [2000, 200, 20], multiply the last element by +-1 (depending on the sign of determinant of UV), sum them and divide by the standard deviation of your points to get scale.
You can recycle the following code, which is using the Eigen library:
typedef Eigen::Matrix<double, 3, 1, Eigen::DontAlign> Vector3d_U; // microsoft's 32-bit compiler can't put Eigen::Vector3d inside a std::vector. for other compilers or for 64-bit, feel free to replace this by Eigen::Vector3d
/**
* #brief rigidly aligns two sets of poses
*
* This calculates such a relative pose <tt>R, t</tt>, such that:
*
* #code
* _TyVector v_pose = R * r_vertices[i] + t;
* double f_error = (r_tar_vertices[i] - v_pose).squaredNorm();
* #endcode
*
* The sum of squared errors in <tt>f_error</tt> for each <tt>i</tt> is minimized.
*
* #param[in] r_vertices is a set of vertices to be aligned
* #param[in] r_tar_vertices is a set of vertices to align to
*
* #return Returns a relative pose that rigidly aligns the two given sets of poses.
*
* #note This requires the two sets of poses to have the corresponding vertices stored under the same index.
*/
static std::pair<Eigen::Matrix3d, Eigen::Vector3d> t_Align_Points(
const std::vector<Vector3d_U> &r_vertices, const std::vector<Vector3d_U> &r_tar_vertices)
{
_ASSERTE(r_tar_vertices.size() == r_vertices.size());
const size_t n = r_vertices.size();
Eigen::Vector3d v_center_tar3 = Eigen::Vector3d::Zero(), v_center3 = Eigen::Vector3d::Zero();
for(size_t i = 0; i < n; ++ i) {
v_center_tar3 += r_tar_vertices[i];
v_center3 += r_vertices[i];
}
v_center_tar3 /= double(n);
v_center3 /= double(n);
// calculate centers of positions, potentially extend to 3D
double f_sd2_tar = 0, f_sd2 = 0; // only one of those is really needed
Eigen::Matrix3d t_cov = Eigen::Matrix3d::Zero();
for(size_t i = 0; i < n; ++ i) {
Eigen::Vector3d v_vert_i_tar = r_tar_vertices[i] - v_center_tar3;
Eigen::Vector3d v_vert_i = r_vertices[i] - v_center3;
// get both vertices
f_sd2 += v_vert_i.squaredNorm();
f_sd2_tar += v_vert_i_tar.squaredNorm();
// accumulate squared standard deviation (only one of those is really needed)
t_cov.noalias() += v_vert_i * v_vert_i_tar.transpose();
// accumulate covariance
}
// calculate the covariance matrix
Eigen::JacobiSVD<Eigen::Matrix3d> svd(t_cov, Eigen::ComputeFullU | Eigen::ComputeFullV);
// calculate the SVD
Eigen::Matrix3d R = svd.matrixV() * svd.matrixU().transpose();
// compute the rotation
double f_det = R.determinant();
Eigen::Vector3d e(1, 1, (f_det < 0)? -1 : 1);
// calculate determinant of V*U^T to disambiguate rotation sign
if(f_det < 0)
R.noalias() = svd.matrixV() * e.asDiagonal() * svd.matrixU().transpose();
// recompute the rotation part if the determinant was negative
R = Eigen::Quaterniond(R).normalized().toRotationMatrix();
// renormalize the rotation (not needed but gives slightly more orthogonal transformations)
double f_scale = svd.singularValues().dot(e) / f_sd2_tar;
double f_inv_scale = svd.singularValues().dot(e) / f_sd2; // only one of those is needed
// calculate the scale
R *= f_inv_scale;
// apply scale
Eigen::Vector3d t = v_center_tar3 - (R * v_center3); // R needs to contain scale here, otherwise the translation is wrong
// want to align center with ground truth
return std::make_pair(R, t); // or put it in a single 4x4 matrix if you like
}
For 3D points the problem is known as the Absolute Orientation problem. A c++ implementation is available from Eigen http://eigen.tuxfamily.org/dox/group__Geometry__Module.html#gab3f5a82a24490b936f8694cf8fef8e60 and paper http://web.stanford.edu/class/cs273/refs/umeyama.pdf
you can use it via opencv by converting the matrices to eigen with cv::cv2eigen() calls.
Start with translation of both sets of points. So that their centroid coincides with the origin of the coordinate system. Translation vector is just the difference between these centroids.
Now we have two sets of coordinates represented as matrices P and Q. One set of points may be obtained from other one by applying some linear operator (which performs both scaling and rotation). This operator is represented by 3x3 matrix X:
P * X = Q
To find proper scale/rotation we just need to solve this matrix equation, find X, then decompose it into several matrices, each representing some scaling or rotation.
A simple (but probably not numerically stable) way to solve it is to multiply both parts of the equation to the transposed matrix P (to get rid of non-square matrices), then multiply both parts of the equation to the inverted PT * P:
PT * P * X = PT * Q
X = (PT * P)-1 * PT * Q
Applying Singular value decomposition to matrix X gives two rotation matrices and a matrix with scale factors:
X = U * S * V
Here S is a diagonal matrix with scale factors (one scale for each coordinate), U and V are rotation matrices, one properly rotates the points so that they may be scaled along the coordinate axes, other one rotates them once more to align their orientation to second set of points.
Example (2D points are used for simplicity):
P = 1 2 Q = 7.5391 4.3455
2 3 12.9796 5.8897
-2 1 -4.5847 5.3159
-1 -6 -15.9340 -15.5511
After solving the equation:
X = 3.3417 -1.2573
2.0987 2.8014
After SVD decomposition:
U = -0.7317 -0.6816
-0.6816 0.7317
S = 4 0
0 3
V = -0.9689 -0.2474
-0.2474 0.9689
Here SVD has properly reconstructed all manipulations I performed on matrix P to get matrix Q: rotate by the angle 0.75, scale X axis by 4, scale Y axis by 3, rotate by the angle -0.25.
If sets of points are scaled uniformly (scale factor is equal by each axis), this procedure may be significantly simplified.
Just use Kabsch algorithm to get translation/rotation values. Then perform these translation and rotation (centroids should coincide with the origin of the coordinate system). Then for each pair of points (and for each coordinate) estimate Linear regression. Linear regression coefficient is exactly the scale factor.
A good explanation Finding optimal rotation and translation between corresponding 3D points
The code is in matlab but it's trivial to convert to opengl using the cv::SVD function
You might want to try ICP (Iterative closest point).
Given two sets of 3d points, it will tell you the transformation (rotation + translation) to go from the first set to the second one.
If you're interested in a c++ lightweight implementation, try libicp.
Good luck!
The general transformation, as well the scale can be retrieved via Procrustes Analysis. It works by superimposing the objects on top of each other and tries to estimate the transformation from that setting. It has been used in the context of ICP, many times. In fact, your preference, Kabash algorithm is a special case of this.
Moreover, Horn's alignment algorithm (based on quaternions) also finds a very good solution, while being quite efficient. A Matlab implementation is also available.
Scale can be inferred without SVD, if your points are uniformly scaled in all directions (I could not make sense of SVD-s scale matrix either). Here is how I solved the same problem:
Measure distances of each point to other points in the point cloud to get a 2d table of distances, where entry at (i,j) is norm(point_i-point_j). Do the same thing for the other point cloud, so you get two tables -- one for original and the other for reconstructed points.
Divide all values in one table by the corresponding values in the other table. Because the points correspond to each other, the distances do too. Ideally, the resulting table has all values being equal to each other, and this is the scale.
The median value of the divisions should be pretty close to the scale you are looking for. The mean value is also close, but I chose median just to exclude outliers.
Now you can use the scale value to scale all the reconstructed points and then proceed to estimating the rotation.
Tip: If there are too many points in the point clouds to find distances between all of them, then a smaller subset of distances will work, too, as long as it is the same subset for both point clouds. Ideally, just one distance pair would work if there is no measurement noise, e.g when one point cloud is directly derived from the other by just rotating it.
you can also use ScaleRatio ICP proposed by BaoweiLin
The code can be found in github
I am extracting in OpenGL the Model Matrix with
glGetFloatv (GL_MODELVIEW_MATRIX, (float*)x)
And would like to extract from the resulting 4x4 matrix the x,y and z axis rotations. How Can I do that ?
Thanks !
First you should know, that x,y,z axis rotations, called Euler Angles suffer from serious numerical problems. Also they're not unambigous. So either you store a rotation angle and the rotation axis, thus effectively forming a quaternion in disguise, or you stick with the full rotation matrix.
Find the quaternion from a rotation matrix is called an eigenvalue problem. Technically you're determining the eigenvector of the rotation matrix, which is the axis and the magnitude designates the angle.
I'm writing a CAD-like app, so I understand your problem, we 'in the business' know how awful Euler angles are for linear transformations - but the end-user finds them far more intuitive than matrices or quaternions.
For my app I interpreted Ken Shoemake's wonderful algorithm, it's one of the very few that support arbitrary rotation orders. It's from '93, so it's in pure C code - not for the faint hearted!
http://tog.acm.org/resources/GraphicsGems/gemsiv/euler_angle/
Something like this should give you what you're after.
final double roll = Math.atan2(2 * (quat.getW() * quat.getX() + quat.getY() * quat.getZ()),
1 - 2 * (quat.getX() * quat.getX() + quat.getY() * quat.getY()));
final double pitch = Math.asin(2 * (quat.getW() * quat.getY() - quat.getZ() * quat.getY()));
final double yaw = Math.atan2(2 * (quat.getW() * quat.getZ() + quat.getX() * quat.getY()), 1 - 2 * (quat.getY()
* quat.getY() + quat.getZ() * quat.getZ()));
I use this as a utility function to print out camera angles when I'm using SLERP to interpolate between 2 quaternions that I've derived from 2 4x4 matrices (i.e. camera movement between 2 3D points).
I'm trying to figure out if I have points that make for example a square:
* *
* *
and let's say I know the center of this square.
I want a formula that will make it for eample twice its size but from the center
* *
* *
* *
* *
Therefore the new shape is twice as large and from the center of the polygon. It has to work for any shape not just squares.
I'm looking more for the theory behind it more than the implementation.
If you know the center point cp and a point v in the polygon you would like to scale by scale, then:
v2 = v - cp; // get a vector to v relative to the centerpoint
v2_scaled = v2 * scale; // scale the cp-relative-vector
v1_scaled = v2_scaled + cp; // translate the scaled vector back
This translate-scale-translate pattern can be performed on vectors of any dimension.
If you want the shape twice as large, scale the distance of the coordinates to be sqrt(2) times further from the center.
In other words, let's say your point is at (x, y) and the center is (xcent, ycent). Your new point should be at
(xcent + sqrt(2)*(x - xcent), ycent + sqrt(2)*(y - ycent))
This will scale the distances from the new 'origin', (xcent, ycent) in such a way that the area doubles. (Because sqrt(2)*sqrt(2) == 2).
I'm not sure there's a clean way to do this for all types of objects. For relatively simple ones, you should be able to find the "center" as the average of all the X and Y values of the individual points. To double the size, you find the length and angle of a vector from the center to the point. Double the length of the vector, and retain the same angle to get the new point.
Edit: of course, "twice the size" is open to several interpretations (e.g., doubling the perimeter vs. doubling the area) These would change the multiplier used above, but the basic algorithm would remain essentially the same.
To do what you want you need to perform three operations: translate the square so that its centroid coincides with the origin of the coordinate system, scale the resulting square, translate it back.