Python library for running the anisotropic version of MAIRE+
Project description
AniMAIRE
N.B. Currently this tool only runs on Linux-based machines (not on Windows)
A Python toolkit for calculating dose rates in Earth's atmosphere based on any incoming proton or alpha particle spectra, with any pitch angle distribution.
If you use this software for scientific research, please reference AniMAIRE as C. S. W. Davis, F. Lei, F. Baird, K. Ryden and C. Dyer (2023). AniMAIRE version {version number}. https://github.com/ssc-maire/AniMAIRE-public , https://pypi.org/project/AniMAIRE/ . Surrey Space Center, University of Surrey.
Installation
To install this toolkit from this Github repository, first clone this repository to your local system, and then from the cloned respository, run
sudo pip3 install .
in the cloned directory.
Note that there are quite a few sizeable data files within some of the dependencies for this package that get copied during installation (on the order of about several hundred megabytes in total) so installation may take a couple of minutes.
Usage
After installation, to import the toolkit into a particular Python script, run
from AniMAIRE import AniMAIRE
All of the main useful functions are contained within this AniMAIRE
module, and all other modules contained in this toolkit are primarily intended to be accessed internally (although don't let that stop you from using or editing them for your own purposes if you wish).
Calculating dose rates at any location in Earth's atmosphere
The basic function for performing a run to calculate dose rates in AniMAIRE
is the run_from_spectra
function, which has the format:
def run_from_spectra(
proton_rigidity_spectrum=None,
alpha_rigidity_spectrum=None,
reference_pitch_angle_latitude=None,
reference_pitch_angle_longitude=None,
proton_pitch_angle_distribution=isotropicPitchAngleDistribution(),
alpha_pitch_angle_distribution=isotropicPitchAngleDistribution(),
altitudes_in_kft=[0,10,20] + [i for i in range(25, 61 + 1, 3)],
altitudes_in_km=None,
Kp_index=None,
date_and_time=dt.datetime.now(),
array_of_lats_and_longs=default_array_of_lats_and_longs,
cache_magnetocosmics_run=True,
)
run_from_spectra
performs a run at a single date and time and Kp index to calculate dose rates across Earth's atmosphere based on proton, alpha particle, or proton + alpha particle spectra. Particle spectra here must be described in units of cm-2 s-1 sr-1 (GV/n)-1, and with respect to rigidity in units of GV.
Particle spectra, as well as pitch angle distributions, can be set as any 'callable' object in Python, i.e. a function, as will be shown in examples below. At least one particle spectrum must be specified, as well as a Kp index, so this function to execute successfully. For runs designed to simulate dose rates during particular dates and times, the argument date_and_time
must also be supplied with a Python datetime
corresponding to the timestamp being investigated (by default, the function assumes that the current date and time should be used).
Note that while this function takes an alpha particle spectrum as an input, it actually interpolates the dose rates due to alpha particles to those of heavier ions too, so outputted dose rates due to an alpha particle spectrum are in fact the combined total of all ions heavier than protons.
AniMAIRE
performs runs of the MAGNETOCOSMICS as part of dose rate calculations (using the AsympDirsCalculator package), and these currently take up by far the majority of AniMAIRE
runtime - on the order of over half an hour on the developer's computer versus less than 6 minutes for the rest of the program. Therefore if the cache_magnetocosmics_run
argument is set to True
, which it is by default, AniMAIRE
will cache the results of MAGNETOCOSMICS simulations in the directory that AniMAIRE
is run from in the generated cachedMagnetocosmicsRunData
and cacheAsymptoticDirectionOutputs
directories. This significantly speeds up any tasks where users wish to investigate a constant Kp_index
and date_and_time
, but wish to vary the spectrum and pitch angle distribution and investigate how dose rates are impacted, as magnetocosmics runs are only performed once.
Simple isotropic runs and plotting
A basic run of the run_from_spectra
function might look like this:
from AniMAIRE import AniMAIRE
import datetime as dt
test_isotropic_dose_rates = AniMAIRE.run_from_spectra(
proton_rigidity_spectrum=lambda x:2.56*(x**-3.41),
Kp_index=3,
date_and_time=dt.datetime(2006, 12, 13, 3, 0),
)
in this example, the proton rigidity spectrum is set to be a power law with a normalisation factor of 2.56 cm-2 s-1 sr-1 (GV/n)-1, and a spectral index of 3.41, using the commonly used lambda
approach to create a function within a single line. Kp index is set to be 3, and the date and time to simulate are set to be 13th of December 2006, 03:00. This function will likely take at least several minutes to run, depending on the speed of the machine and number of cores, and should output a Pandas DataFrame to test_isotropic_dose_rates
, giving:
latitude longitude altitude (km) edose adose dosee tn1 tn2 tn3 SEU SEL
0 -90.0 0.0 0.0000 0.010442 0.012540 0.010010 0.004437 0.002729 0.001828 2.729229e-16 2.729229e-11
1 -90.0 0.0 3.0480 0.101786 0.117658 0.085755 0.051895 0.033617 0.022979 3.361684e-15 3.361684e-10
2 -90.0 0.0 6.0960 0.672702 0.742332 0.457695 0.326731 0.211853 0.145046 2.118530e-14 2.118530e-09
3 -90.0 0.0 7.6200 1.442377 1.541670 0.975436 0.665785 0.431261 0.295516 4.312608e-14 4.312608e-09
4 -90.0 0.0 8.5344 2.165860 2.249419 1.426324 0.964791 0.623291 0.426927 6.232913e-14 6.232913e-09
... ... ... ... ... ... ... ... ... ... ... ...
42619 90.0 355.0 14.9352 16.953199 14.033322 9.762795 5.138425 3.234975 2.164808 3.234975e-13 3.234975e-08
42620 90.0 355.0 15.8496 21.327714 16.796347 11.858681 5.949880 3.711156 2.463976 3.711156e-13 3.711156e-08
42621 90.0 355.0 16.7640 26.122787 19.802434 14.318360 6.759204 4.182604 2.757482 4.182604e-13 4.182604e-08
42622 90.0 355.0 17.6784 31.856083 23.278901 17.431863 7.562120 4.638132 3.029771 4.638132e-13 4.638132e-08
42623 90.0 355.0 18.5928 38.265701 26.680896 20.232603 8.340509 5.067928 3.275415 5.067928e-13 5.067928e-08
when test_isotropic_dose_rates
is printed.
The outputted dose rate (or flux) labels represent the following dose rate/flux types:
label | dose rate/flux type |
---|---|
adose | ambient dose equivalent in µSv/hr |
edose | effective dose in µSv/hr |
dosee | dose equivalent in µSv/hr |
tn1 | >1 MeV neutron flux, in n/cm2/s |
tn2 | >10 MeV neutron flux, in n/cm2/s |
tn3 | >60 MeV neutron flux, in n/cm2/s |
SEU | single event upset rate for an SRAM device in upsets/second/bit |
SEL | single event latch-up rate for an SRAM device in latch-ups/second/device |
These dose rates are produced by default at every latitude and longitude corresponding to 5 by 5 degree intervals across Earth's surface, and for altitudes of 0 kilofeet, 10 kilofeet, 20 kilofeet and between 25 kilofeet and 61 kilofeet at intervals of 3 kilofeet. This can be altered using the altitudes_in_kft
, altitudes_in_km
and array_of_lats_and_longs
.
Any particular altitudes the user wants to use can be supplied to altitudes_in_kft
or altitudes_in_km
as a list
or numpy array.
If you want to perform calculations only at a specific set of latitudes and longitudes you should use the array_of_lats_and_longs
argument, supplying it as a 2 dimensional list
or numpy array, where the first column refers to latitudes and the second column refers to longitudes. All longitudes in this case should be specified in terms of longitude east (i.e. 0.00 degrees - 359.99 degrees). Using the array_of_lats_and_longs
argument significantly speeds up the running of AniMAIRE
if you're only interested in a small number of coordinates, so its use is highly recommended in those situations.
There are many ways you could plot this data. An example function, create_single_dose_map_plot
, has been supplied in AniMAIRE
that uses plotly to plot the dose rates across Earth (i.e. as a function of latitude and longitude) at a given altitude. Its specification is the following:
def create_single_dose_map_plot(DF_to_use,
selected_altitude_in_km)
where DF_to_use
is the Pandas DataFrame outputted by a run of AniMAIRE
and altitude is one of the altitudes in kilometers supplied to/outputted by the run.
To use this function to create a map of the isotropic situation as given as an example above, you could run
isotropic_dose_rate_map = AniMAIRE.create_single_dose_map_plot(test_isotropic_dose_rates,
selected_altitude_in_km = 12.1920)
which should plot the following figure as a plotly plot:
and assign the plot to the isotropic_dose_rate_map
variable for the user to use as they wish.
Anisotropic runs
run_from_spectra
defaults to an isotropic spectrum if no pitch angle distribution is supplied for either protons or alpha particles by the user.
To run an anisotropic spectrum, differential pitch angle distributions must be supplied to the proton_pitch_angle_distribution
and/or alpha_pitch_angle_distribution
arguments in run_from_spectra
along with a reference location specified in terms of latitude and longitude in the reference_pitch_angle_latitude
and reference_pitch_angle_longitude
arguments respectively. The pitch angle distributions must be supplied as 2 dimensional functions, where the first argument is the pitch angle, and the second argument is particle rigidity (in many cases the pitch angle distribution might not depend on rigidity, but for programmatic reasons the function must at least take in rigidity as an argument although it does not need to have a dependence on it). The pitch angle here must be specified in units of radians.
reference_pitch_angle_latitude
and reference_pitch_angle_longitude
are the reference latitude and longitude in GEO coordinates representing a pitch angle of 0 in the supplied pitch angle distribution used. AniMAIRE
currently makes the assumption that incoming particle distributions are cylindrically symmetric about this reference direction, and therefore that only the pitch angle with respect to this latitude and longitude are required to calculate dose rates anisotropically across Earth. Incoming solar particle events are frequently oriented near to the direction of the Interplanetary Magnetic Field (IMF), so you could specify pitch angles relative to the IMF here, and use the latitude and longitude of the IMF as the reference latitude and longitude.
The pitch angle distributions and rigidity spectrum must be specified in units normalised such that the product of the pitch angle distribution and rigidity spectrum multiplied together is in units of cm-2 s-1 sr-1 (GV/n)-1.
The pitch angle distributions can be specified using the Python lambda
as with the rigidity spectra, but with 2 dimensions rather than 1. For example, to specify a Gaussian pitch angle distribution you could use:
import numpy as np
sigma = np.sqrt(0.19)
test_pitch_angle_dist_function = lambda pitch_angle,rigidity:np.exp(-(pitch_angle**2)/(sigma**2))
where sigma
here has arbitrarily been chosen to be the square root of 0.19 for example purposes.
here pitch_angle_dist_function
would be a viable input as a pitch angle distribution to run_from_spectra
. While the function itself does not depend on rigidity
, rigidity
is specified as the second argument of the function nonetheless, as required for calculations to work.
An example of using this might be:
import numpy as np
from AniMAIRE import AniMAIRE
import datetime as dt
sigma = np.sqrt(0.19)
pitch_angle_reference_latitude = -17.0
pitch_angle_reference_longitude = 148.0
test_pitch_angle_dist_function = lambda pitch_angle,rigidity:np.exp(-(pitch_angle**2)/(sigma**2))
test_anisotropic_dose_rates = AniMAIRE.run_from_spectra(
proton_rigidity_spectrum=lambda x:2.56*(x**-3.41),
proton_pitch_angle_distribution=test_pitch_angle_dist_function,
reference_pitch_angle_latitude=pitch_angle_reference_latitude,reference_pitch_angle_longitude=pitch_angle_reference_longitude,
Kp_index=3,
date_and_time=dt.datetime(2006, 12, 13, 3, 0),
)
when run this should output a Pandas DataFrame to test_anisotropic_dose_rates
with the same general output format as given in the previously described isotropic dose rates case.
In this case printing test_anisotropic_dose_rates
should output:
latitude longitude altitude (km) edose adose dosee tn1 tn2 tn3 SEU SEL
0 -90.0 0.0 0.0000 1.976895e-07 2.027961e-07 3.222401e-07 1.286575e-08 7.877480e-09 5.401425e-09 7.877480e-22 7.877480e-17
1 -90.0 0.0 3.0480 4.838923e-07 4.869626e-07 7.032983e-07 7.429541e-08 4.866265e-08 3.410940e-08 4.866265e-21 4.866265e-16
2 -90.0 0.0 6.0960 1.453834e-06 1.411544e-06 2.045308e-06 2.472576e-07 1.611648e-07 1.136527e-07 1.611648e-20 1.611648e-15
3 -90.0 0.0 7.6200 2.352658e-06 2.382057e-06 3.304989e-06 3.720997e-07 2.420436e-07 1.708843e-07 2.420436e-20 2.420436e-15
4 -90.0 0.0 8.5344 2.970462e-06 2.791970e-06 4.201789e-06 4.473736e-07 2.919136e-07 2.063902e-07 2.919136e-20 2.919136e-15
... ... ... ... ... ... ... ... ... ... ... ...
42619 90.0 355.0 14.9352 1.062397e-06 7.975138e-07 5.902218e-07 2.766678e-07 1.764588e-07 1.216189e-07 1.764588e-20 1.764588e-15
42620 90.0 355.0 15.8496 1.289216e-06 9.183397e-07 6.964574e-07 3.063998e-07 1.945207e-07 1.338582e-07 1.945207e-20 1.945207e-15
42621 90.0 355.0 16.7640 1.525359e-06 1.040969e-06 8.062018e-07 3.339381e-07 2.112220e-07 1.452375e-07 2.112220e-20 2.112220e-15
42622 90.0 355.0 17.6784 1.777447e-06 1.163693e-06 9.297615e-07 3.568426e-07 2.248452e-07 1.543556e-07 2.248452e-20 2.248452e-15
42623 90.0 355.0 18.5928 2.036052e-06 1.275021e-06 1.040287e-06 3.755276e-07 2.357292e-07 1.614028e-07 2.357292e-20 2.357292e-15
which will produce the following plot when
anisotropic_dose_rate_map = AniMAIRE.create_single_dose_map_plot(test_anisotropic_dose_rates,
selected_altitude_in_km = 12.1920)
is run:
Functions for running AniMAIRE
for specific situations and for a past timestamp
In addition to the quite general run_from_spectra
function, AniMAIRE
currently contains several functions for running calculations for specific types of spectra and situations, to make it easier for users to perform runs without having to determine and feed in spectra to run_from_spectra
themselves.
The run_from_DLR_cosmic_ray_power_law
function allows users to run full atmospheric dose rate calculations (for cosmic ray only/'quiet' time periods only) from just a date and time, or alternatively from just a single OULU count rate, or just a value of 'W parameter', as well as Kp index. This function utilises the CosRayModifiedISO package to determine the spectra due to protons and alpha particles during cosmic ray only time periods, and then runs run_from_spectra
using both of those spectra under isotropic conditions. The specifications of run_from_DLR_cosmic_ray_power_law
are:
def run_from_DLR_cosmic_ray_model(OULU_count_rate_in_seconds=None,
W_parameter=None,
Kp_index=None,
date_and_time=None,
**kwargs)
**kwargs
here can be used to supply any arguments you wish to run_from_spectra
as specified previously, such as the list of altitudes and list of coordinates to perform calculations for. Details on what OULU_count_rate_in_seconds
and W_parameter
mean can be found at https://github.com/ssc-maire/CosRayModifiedISO . If either OULU_count_rate_in_seconds
or W_parameter
are used, only one of them should be specified. Otherwise, AniMAIRE
will determined their values using the date_and_time
parameter supplied.
In addition to running from the DLR-ISO isotropic cosmic ray model, you can also run AniMAIRE
from a combined power law rigidity spectrum and Gaussian pitch angle distribution. This can be done using the run_from_power_law_gaussian_distribution
function:
def run_from_power_law_gaussian_distribution(J0, gamma, deltaGamma, sigma,
reference_pitch_angle_latitude, reference_pitch_angle_longitude,
Kp_index,date_and_time,
**kwargs)
Here J0
, gamma
, deltaGamma
, sigma
, reference_pitch_angle_latitude
, reference_pitch_angle_longitude
are all defined as specified in the format of papers like Mishev, A., Usoskin, I. Analysis of the Ground-Level Enhancements on 14 July 2000 and 13 December 2006 Using Neutron Monitor Data. Sol Phys 291, 1225–1239 (2016). https://doi.org/10.1007/s11207-016-0877-2.
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