I have a wind field : eastward component u and northward component v, in m s-1. I want to make a quiver plot of this field in north stereographic projection. I would expect the correct command to be:
ax = plt.axes(projection =ccrs.NorthPolarStereo())
ax.quiver(lon, lat, u, v, transform = ccrs.PlateCarree(), angles = "xy")
( The complete test code is below.) However, this produces arrows in the wrong direction. It appears that the way to obtain the correct direction for the arrows is to write:
ax.quiver(lon, lat, u / np.cos(lat / 180 * np.pi) , v, transform = ccrs.PlateCarree(), angles = "xy")
Note that the magnitude of the vector is not correct then, we should also renormalize it to get the correct magnitude. Compare this with the behavior of basemap:
m = basemap.Basemap(projection="npstere", boundinglat = 50, lon_0 = 0)
u_rot, v_rot, x, y = m.rotate_vector(u, v, lon ,lat, returnxy=True)
m.quiver(x, y, u_rot, v_rot, angles = "xy")
which produces correct arrows.
I think this is a bug, or a bad feature of cartopy. The problem comes from the transform_vectors method, as shown in the test code below. In this test code, we want to plot a single vector at longitude 0掳, latitude 89掳N. The vector is almost westward: u < 0 and v is very small compared to u. In the north stereographic projection, the components of the projected vector should be almost the same than the original components. We see with the test code below that the rotate_vector method of basemap correctly produces this result. However, the transform_vectors of cartopy surprisingly does not produce this result. To get the correct result with transform_vectors, we have to divide u by the cosine of latitude, and renormalize the result from transform_vectors. It seems that transform_vectors expects the derivative of longitude instead of the wind. This is quite awkward to use and counter-intuitive, I think, or a bug. The test code below goes on to plot the single vector, with basemap and with cartopy. We see the red arrow with cartopy in the wrong direction.
Here is the complete test code.
#!/usr/bin/env python3
from mpl_toolkits import basemap
import cartopy.crs as ccrs
import matplotlib.pyplot as plt
import numpy as np
m = basemap.Basemap(projection="npstere", boundinglat = 50, lon_0 = 0)
proj = ccrs.NorthPolarStereo()
src_crs = ccrs.PlateCarree()
lon = np.array([0])
lat = np.array([89])
u = np.array([-3])
v = np.array([0.1])
print("m.rotate_vector(u, v, lon ,lat):", m.rotate_vector(u, v, lon ,lat))
print("proj.transform_vectors(src_crs, lon, lat, u, v):",
proj.transform_vectors(src_crs, lon, lat, u, v))
u_rot, v_rot = proj.transform_vectors(src_crs, lon, lat,
u / np.cos(lat /180 * np.pi), v)
print("u_rot, v_rot:", u_rot, v_rot)
renorm = np.sqrt((u**2 + v**2) / (u_rot**2 + v_rot**2))
print("array((u_rot, v_rot)) * renorm:", np.array((u_rot, v_rot)) * renorm)
plt.figure()
u_rot, v_rot, x, y = m.rotate_vector(u, v, lon ,lat, returnxy=True)
m.quiver(x, y, u_rot, v_rot, angles = "xy")
m.drawcoastlines()
plt.title("with basemap")
plt.figure()
ax = plt.axes(projection = proj)
ax.coastlines()
ax.set_extent((-180, 180, 50, 90), src_crs)
ax.quiver(lon, lat, u, v, transform = src_crs, angles = "xy", color = "red")
ax.quiver(lon, lat, u / np.cos(lat / 180 * np.pi), v, transform = src_crs,
angles = "xy")
plt.title("with cartopy")
plt.show()
Here is the standard output of the script:
m.rotate_vector(u, v, lon ,lat): (array([-2.99999999]), array([ 0.10000035]))
proj.transform_vectors(src_crs, lon, lat, u, v): (array([-1.3922597]), array([ 2.65925044]))
u_rot, v_rot: [-171.80062661] [ 5.72817851]
array((u_rot, v_rot)) * renorm: [[-2.99999913]
[ 0.10002601]]
And here are the two resulting figures:


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Made a test with the Mercator projection instead of north polar stereographic and the problem is the same. So I guess the problem is for all projections.
Confirming that the transform_vectors algorithm is based on "derivatives of source coordinate system". This is documented at https://scitools.org.uk/cartopy/docs/latest/crs/index.html#cartopy.crs.CRS.transform_vectors, though there is no doubt that it could be made even more explicit (your help would be greatly appreciated there).
I believe there are three cases:
cc @ajdawson as the original transform_vectors author.
In putting together the summary above, I had the following example:
src = ccrs.PlateCarree()
nx, ny = 6, 5
xs = np.linspace(*src.x_limits, nx+2)[1:-1]
ys = np.linspace(*src.y_limits, ny+2)[1:-1]
# u and v are in the x and y direction of src.
u = 5 # m/s, or some other non-src CRS bound system.
v = 0 # m/s
xs, ys = np.meshgrid(xs, ys)
us = np.tile(u, xs.shape)
vs = np.tile(v, ys.shape)
Which when visualised in the source CRS:
plt.figure(figsize=(10, 10))
ax = plt.axes(projection=src)
ax.coastlines()
ax.quiver(xs, ys, us, vs, angles="xy", color="red")

And in a projected CRS:
plt.figure(figsize=(10, 10))
ax = plt.axes(projection=ccrs.NorthPolarStereo(central_longitude=0))
ax.coastlines()
ax.quiver(xs, ys, us, vs, angles="xy", color="red", transform=src)

Reprojecting that case:
plt.figure(figsize=(10, 10))
ax = plt.axes(projection=ccrs.NorthPolarStereo(central_longitude=0))
ax.coastlines()
ax.quiver(xs, ys, us, vs, angles="xy", color="red", transform=src, regrid_shape=20)

It is quite clear that the magnitude of the vectors is preserved ref and that direction is based on the source grid.
I've thought over this some more, and now wonder if cases 1 and 2 are actually the same thing, and we are looking at a bug that is acute for this projection. In particular, I think the transform_vectors algorithm uses a forward difference to compute the rotation, but a central difference would provide a much better estimation.
Thank you for your answer. Maybe I am missing something in your line of thought but it seems to me that the example you have chosen does not illustrate the problem. The problem comes from the difference between the directions of (u /cos (latitude), v) and (u, v). So if you choose v = 0, there is no difference in direction. That is why I chose : u = -3, v =0.1 and latitude = 89掳, in my post above.
Second, thanks for confirming that the transform_vectors algorithm is based on derivatives of source coordinate system. My point is then that I think the public interface of quiver with cartopy is very inconvenient. The majority of use cases of quiver in Cartopy is probably to plot a wind field in some projection, with the wind given by its eastward and northward components. In order to plot this wind field now in Cartopy, I have to do something like:
u_src_crs = u / np.cos(lat[:, np.newaxis] / 180 * np.pi)
v_src_crs = v
magnitude = ma.sqrt(u**2 + v**2)
magn_src_crs = ma.sqrt(u_src_crs**2 + v_src_crs**2)
ax.quiver(lon, lat, u_src_crs * magnitude / magn_src_crs, v_src_crs * magnitude / magn_src_crs,
transform = src_crs)
I should not have to do all this just to plot a wind field. There should be a one-line command for this, included with cartopy.
+1 for simple way of plotting vectors with starting point given by lat & lon and direction and length given by geographic north & east components in some physical units. In my case this would be geomagnetic and geoelectric fields with north and east components of nT and mV/km respectively.
Ideally there would also be a boolean toggle to choose between making vector lengths depend only on the physical quantity (in addition automatic or user defined global scaling) or also depend on how far they seem to be located from the camera.
Did anyone ever resolve this or find a way of doing something like rotate_vector without Basemap? That was a pretty useful function but it's hard to use this without needing to define the projection with Basemap too...
Using the "angles" keyword in call to quiver seems to work fine.
Edit: using "angles" keyword, with array of angles in degrees seems to work fine.
I do not think it does in a convenient way : that is what I tried to show in submitting this issue. See the example in my post at the top of this issue.
I total agree with @lguez , the current user interface for vector rotation in Cartopy is inconvenient at the least. I don't think this issue is clearly documented so the first time users may not realize they need to rescale the u/v components (like @lguez's code above) before feeding the vectors into transform_vectors . This will end up with wrong vector maps. Can someone add a short example to showcase the correct way to rotate vectors to the documentation before there is a fix for this? I am sure I am not the only one trying to figure out why the wind maps look funny in the polar regions.
+1 for documentation on (optionally simple) way of plotting vectors with starting point given by lat & lon and direction and length given by geographic north & east components in some physical units
Most helpful comment
Thank you for your answer. Maybe I am missing something in your line of thought but it seems to me that the example you have chosen does not illustrate the problem. The problem comes from the difference between the directions of (u /cos (latitude), v) and (u, v). So if you choose v = 0, there is no difference in direction. That is why I chose : u = -3, v =0.1 and latitude = 89掳, in my post above.
Second, thanks for confirming that the transform_vectors algorithm is based on derivatives of source coordinate system. My point is then that I think the public interface of quiver with cartopy is very inconvenient. The majority of use cases of quiver in Cartopy is probably to plot a wind field in some projection, with the wind given by its eastward and northward components. In order to plot this wind field now in Cartopy, I have to do something like:
I should not have to do all this just to plot a wind field. There should be a one-line command for this, included with cartopy.