I am trying to create a 3d surface plot like this, link available here :
https://plotly.com/python/3d-surface-plots/
But the problem is that I only have limited data available where I only have data for the peak location and the height of peak but the rest of the data is missing. In the example z-data need 25 X 25 values 625 data points to generate a valid surface plot.
My data looks something like this:
So my question is that, is it possible to use some polynomial function with the peak location value as a constrain to generate Z-data based on the information I have?
Open to any discussion. Any form of suggestion is appreciated.
Though I don't like this form of interpolation, which is pretty artificial, you can use the following trick:
F(P) = (Σ Fk / d(P, Pk)) / (Σ 1 / d(P, Pk))
P is the point where you interpolate and Pk are the known peak positions. d is the Euclidean distance. (This gives sharp peaks; the squared distance gives smooth ones.)
Unfortunately, far from the peaks this formula tends to the average of the Fk, giving an horizontal surface that is above some of the Fk, giving downward peaks. You can work around this by adding fake peaks of negative height around your data set, to lower the average.
I'm having trouble using the scipy interpolation methods to generate a nice smooth curve from the data points given. I've tried using the standard 1D interpolation, the Rbf interpolation with all options (cubic, gaussian, multiquadric etc.)
in the image provided, the blue line is the original data, and I'm looking to first smooth the sharp edges, and then have dynamically editable points from which to recalculate the curve. Each time a single point is edited it should auto calculate a new spline of some sort to smoothly transition between each point.
It kind of works when the points are within a particular range of each other as below.
But if the points end up too far apart, or too close together, I end up with issues like the following.
Key points are:
The curve MUST be flat between the first two points
The curve must NOT go below point 1 or 2 (i.e. derivative can't be negative)
~15 points (not shown) between points 2 and 3 are also editable and the line between is not necessarily linear. Full control over each of these points is a must, as is the curve going through each of them.
I'm happy to break it down into smaller curves that i then join/convolve, but just need to ensure a >0 gradient.
sample data:
x=[0, 37, 50, 105, 115,120]
y=[0.00965, 0.00965, 0.047850827205882, 0.35600416666667, 0.38074375, 0.38074375]
As an example, try moving point 2 (x=37) to an extreme value, say 10 (keep y the same). Just ensure that all points from x=0 to x=10 (or any other variation) have identical y values of 0.00965.
any assistance is greatly appreciated.
UPDATE
Attempted pchip method suggested in comments with the results below:
pchip method, better and worse...
Solved!
While I'm not sure that this is exactly true, it is as if the spline tools for creating Bezier curves treat the control points as points the calculated curve must go through - which is not true in my case. I couldn't figure out how to turn this feature off, so I found the cubic formula for a Bezier curve (cubic is what I need) and calculated my own points. I only then had to do a little adjustment to make the points fit the required integer x values - in my case, near enough is good enough. I would otherwise have needed to interpolate linearly between two points either side of the desired x value and determine the exact value.
For those interested, cubic needs 4 points - start, end, and 2 control points. The rule is:
B(t) = (1-t)^3 P0 + 3(1-t)^2 tP1 + 3(1-t)t^2 P2 + t^3 P3
Calculate for x and y separately, using a list of values for t. If you need to gradient match, just make sure that the control points for P1 and P2 are only moved along the same gradient as the preceding/proceeding sections.
Perfect result
Suppose, I have 7 timeseries, that represent a changing value measured in a point with coordinates x,y. Also I have a group of 20 points distributed spatially within the coverage of these 7 points.
Thus I want to get 20 time series, where every value is an interpolated value of initial 7 points on a corresponding moment. Timestep is day.
I know that kriging is the best interpolation method in my case. Also I know that kriging interpolation of several points over a regular grid is easy to perform with scikit-learn or pykrige packages. But I want time series (time cycle? wouldnt it work too slowly?) and I want irregular points as target positions of interpolated values, not a regular grid.
So, what is the optimal decision here?
I've seen this theme but there is no time cycling.
On the scheme are shown: points with measured time-series (x,y,value) as o and points which are targets for interpolation as x.
scheme of points
I'm using griddata() to interpolate my (irregular) 2-dimensional depth-measurements; x,y,depth. The method does a great job - but it interpolates over the entire grid where it can find to opposing points. I don't want that behaviour. I'd like to have an interpolation around the existing measurements, say with up to an extent of a certain radius.
Is it possible to tell numpy/scipy: don't interpolate if you're too far from an existing measurement? Resulting in a NODATA-value? ideal = griddata(.., .., .., radius=5.0)
edit example:
In the image below; black dots are the measurements. Shades of blue are the interpolated cells by numpy. The area marked in green is in fact part of the picture but is considered as NODATA by numpy (because there's no points in between). Now, the red areas, are interpolated, but I want to get rid of them. any ideas?
Ok cool. I don't think there is a built-in option for griddata() that does what you want, so you will need to write it yourself.
This comes down to calculating the distances between N input data points and M interpolation points. This is simple enough to do but if you have a lot of points it can be slow at ~O(M*N). But here's an example that calculates the distances to allN data points, for each interpolation point. If the number of data points withing the radius is at least neighbors, it keeps the value. Otherwise is writes the value of NODATA.
neighbors is 4 because griddata() will use biilinear interpolation which needs points bounding the interpolants in each dimension (2*2 = 4).
#invec - input points Nx2 numpy array
#mvec - interpolation points Mx2 numpy array
#just some random points for example
N=100
invec = 10*np.random.random([N,2])
M=50
mvec = 10*np.random.random([M,2])
# --- here you would put your griddata() call, returning interpolated_values
interpolated_values = np.zeros(M)
NODATA=np.nan
radius = 5.0
neighbors = 4
for m in range(M):
data_in_radius = np.sqrt(np.sum( (invec - mvec[m])**2, axis=1)) <= radius
if np.sum(data_in_radius) < neighbors :
interpolated_values[m] = NODATA
Edit:
Ok re-read and noticed the input is really 2D. Example modified.
Just as an additional comment, this could be greatly accelerated if you first build a coarse mapping from each point mvec[m] to a subset of the relevant data points.
The costliest step in the loop would change from
np.sqrt(np.sum( (invec - mvec[m])**2, axis=1))
to something like
np.sqrt(np.sum( (invec[subset[m]] - mvec[m])**2, axis=1))
There are plenty of ways to do this, for example using a Quadtree, hashing function, or 2D index. But whether this gives performance advantage depends on the application, how your data is structured, etc.
So, I have three numpy arrays which store latitude, longitude, and some property value on a grid -- that is, I have LAT(y,x), LON(y,x), and, say temperature T(y,x), for some limits of x and y. The grid isn't necessarily regular -- in fact, it's tripolar.
I then want to interpolate these property (temperature) values onto a bunch of different lat/lon points (stored as lat1(t), lon1(t), for about 10,000 t...) which do not fall on the actual grid points. I've tried matplotlib.mlab.griddata, but that takes far too long (it's not really designed for what I'm doing, after all). I've also tried scipy.interpolate.interp2d, but I get a MemoryError (my grids are about 400x400).
Is there any sort of slick, preferably fast way of doing this? I can't help but think the answer is something obvious... Thanks!!
Try the combination of inverse-distance weighting and
scipy.spatial.KDTree
described in SO
inverse-distance-weighted-idw-interpolation-with-python.
Kd-trees
work nicely in 2d 3d ..., inverse-distance weighting is smooth and local,
and the k= number of nearest neighbours can be varied to tradeoff speed / accuracy.
There is a nice inverse distance example by Roger Veciana i Rovira along with some code using GDAL to write to geotiff if you're into that.
This is of coarse to a regular grid, but assuming you project the data first to a pixel grid with pyproj or something, all the while being careful what projection is used for your data.
A copy of his algorithm and example script:
from math import pow
from math import sqrt
import numpy as np
import matplotlib.pyplot as plt
def pointValue(x,y,power,smoothing,xv,yv,values):
nominator=0
denominator=0
for i in range(0,len(values)):
dist = sqrt((x-xv[i])*(x-xv[i])+(y-yv[i])*(y-yv[i])+smoothing*smoothing);
#If the point is really close to one of the data points, return the data point value to avoid singularities
if(dist<0.0000000001):
return values[i]
nominator=nominator+(values[i]/pow(dist,power))
denominator=denominator+(1/pow(dist,power))
#Return NODATA if the denominator is zero
if denominator > 0:
value = nominator/denominator
else:
value = -9999
return value
def invDist(xv,yv,values,xsize=100,ysize=100,power=2,smoothing=0):
valuesGrid = np.zeros((ysize,xsize))
for x in range(0,xsize):
for y in range(0,ysize):
valuesGrid[y][x] = pointValue(x,y,power,smoothing,xv,yv,values)
return valuesGrid
if __name__ == "__main__":
power=1
smoothing=20
#Creating some data, with each coodinate and the values stored in separated lists
xv = [10,60,40,70,10,50,20,70,30,60]
yv = [10,20,30,30,40,50,60,70,80,90]
values = [1,2,2,3,4,6,7,7,8,10]
#Creating the output grid (100x100, in the example)
ti = np.linspace(0, 100, 100)
XI, YI = np.meshgrid(ti, ti)
#Creating the interpolation function and populating the output matrix value
ZI = invDist(xv,yv,values,100,100,power,smoothing)
# Plotting the result
n = plt.normalize(0.0, 100.0)
plt.subplot(1, 1, 1)
plt.pcolor(XI, YI, ZI)
plt.scatter(xv, yv, 100, values)
plt.title('Inv dist interpolation - power: ' + str(power) + ' smoothing: ' + str(smoothing))
plt.xlim(0, 100)
plt.ylim(0, 100)
plt.colorbar()
plt.show()
There's a bunch of options here, which one is best will depend on your data...
However I don't know of an out-of-the-box solution for you
You say your input data is from tripolar data. There are three main cases for how this data could be structured.
Sampled from a 3d grid in tripolar space, projected back to 2d LAT, LON data.
Sampled from a 2d grid in tripolar space, projected into 2d LAT LON data.
Unstructured data in tripolar space projected into 2d LAT LON data
The easiest of these is 2. Instead of interpolating in LAT LON space, "just" transform your point back into the source space and interpolate there.
Another option that works for 1 and 2 is to search for the cells that maps from tripolar space to cover your sample point. (You can use a BSP or grid type structure to speed up this search) Pick one of the cells, and interpolate inside it.
Finally there's a heap of unstructured interpolation options .. but they tend to be slow.
A personal favourite of mine is to use a linear interpolation of the nearest N points, finding those N points can again be done with gridding or a BSP. Another good option is to Delauney triangulate the unstructured points and interpolate on the resulting triangular mesh.
Personally if my mesh was case 1, I'd use an unstructured strategy as I'd be worried about having to handle searching through cells with overlapping projections. Choosing the "right" cell would be difficult.
I suggest you taking a look at GRASS (an open source GIS package) interpolation features (http://grass.ibiblio.org/gdp/html_grass62/v.surf.bspline.html). It's not in python but you can reimplement it or interface with C code.
Am I right in thinking your data grids look something like this (red is the old data, blue is the new interpolated data)?
alt text http://www.geekops.co.uk/photos/0000-00-02%20%28Forum%20images%29/DataSeparation.png
This might be a slightly brute-force-ish approach, but what about rendering your existing data as a bitmap (opengl will do simple interpolation of colours for you with the right options configured and you could render the data as triangles which should be fairly fast). You could then sample pixels at the locations of the new points.
Alternatively, you could sort your first set of points spatially and then find the closest old points surrounding your new point and interpolate based on the distances to those points.
There is a FORTRAN library called BIVAR, which is very suitable for this problem. With a few modifications you can make it usable in python using f2py.
From the description:
BIVAR is a FORTRAN90 library which interpolates scattered bivariate data, by Hiroshi Akima.
BIVAR accepts a set of (X,Y) data points scattered in 2D, with associated Z data values, and is able to construct a smooth interpolation function Z(X,Y), which agrees with the given data, and can be evaluated at other points in the plane.