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This document is a work in progress, that will be expanded into a full guide. Right now it covers only one topic.
As explained in the section on Apparent right ascension and declination, Skyfield uses the IAU 2000A precession-nutation model to determine the orientation of the Earth’s axes on any given date. This is used in:
radec()
.wgs84
model.true_equator_and_equinox_of_date
reference frame that can be used to generate (x,y,z) coordinates
as described in the Coordinates chapter.itrs
object,
which combines the orientation of the poles and equinox
with the daily rotation of the Earth.In case you ever need to do low-level math of your own,
each time object offers a matrix t.M
that rotates coordinates from the ICRS
into the Earth equatorial coordinate system of that date and time.
See the section on Rotation Matrices
for a guide to using a rotation matrix.
It was discovered more than a century ago that the Earth’s crust has a slight freedom to wobble with respect to the Earth’s axis of rotation in space, because the continents and ocean basis are bound to the planet’s mass only through the fluid coupling of our planet’s viscous mantle. In Skyfield you can see the size of the effect by loading an official data file from the International Earth Rotation Service (IERS) and measuring the maximum excursions of the polar motion parameters x and y:
from skyfield.api import load
from skyfield.data import iers
url = load.build_url('finals2000A.all')
with load.open(url) as f:
finals_data = iers.parse_x_y_dut1_from_finals_all(f)
ts = load.timescale()
iers.install_polar_motion_table(ts, finals_data)
tt, x_arcseconds, y_arcseconds = ts.polar_motion_table
print('x:', max(abs(x_arcseconds)), 'arcseconds')
print('y:', max(abs(y_arcseconds)), 'arcseconds')
x: 0.32548 arcseconds
y: 0.596732 arcseconds
In what kinds of Skyfield calculations does the exact position of the Earth’s crust come into play?
At the most basic level,
the two polar motion rotations
are applied directly to the ITRS reference frame
in skyfield.framelib.itrs
,
supplementing the changes in the Earth’s orientation
that Skyfield was already expecting
thanks to its IAU 2000A precession and nutation models.
This, in turn, slightly affects:
To have Skyfield apply polar motion when computing positions and coordinates, simply install the IERS tables on your timescale object as shown in the example code above. Polar motion will be used everywhere that it applies.
If you want to double-check that Skyfield’s leap second table
agrees with other tools or software,
you can easily print it out.
Each timescale object offers an array of Julian dates leap_dates
and another array of the same length named leap_offsets
that offers the difference between UTC and TAI in seconds:
ts = load.timescale()
for jd, offset in zip(ts.leap_dates, ts.leap_offsets):
ymd = ts.tt_jd(jd).tt_strftime('%Y-%m-%d')
print(jd, ymd, '{:+}'.format(int(offset)))
2441499.5 1972-07-01 +11
2441683.5 1973-01-01 +12
2442048.5 1974-01-01 +13
...
2456109.5 2012-07-01 +35
2457204.5 2015-07-01 +36
2457754.5 2017-01-01 +37
Note that each leap second occurs just before the Julian date given in the table. Taking the second row as an example, the offset between TAI and UTC increased to +12 at the first moment of the day 1973-01-01. It did so because that day was immediately preceded by a leap second that was attached to the previous day as its final second. So the leap second followed the normal, non-leap second 1972-12-31 12:59:59 and had the special designation 1972-12-31 12:59:60.
On some systems, users have reported that Skyfield consumes 100% of all of their CPUs and makes it difficult to do other work.
This isn’t something that Skyfield has direct control over. It’s the underlying NumPy library that decides how to perform each of the math operations that Skyfield requests. And in this case, the user’s installed version of NumPy was deciding to run a vector operation in parallel across all the CPUs. (Ironically, this made the operation slower!)
In case you find NumPy misbehaving in the same way on your system, the user reported that they were able to force single-threaded behavior by setting this environment variable:
export OPENBLAS_NUM_THREADS=1
export MKL_NUM_THREADS=1
If you want to apply these settings right in your Python code, then you must modify these environment settings before importing NumPy:
# First set up the environment.
import os
os.environ['OPENBLAS_NUM_THREADS'] = '1'
os.environ['MKL_NUM_THREADS'] = '1'
# And only then import NumPy.
import numpy
The same solution might work on your system.