Getting Started with Simulating the Emission Spectrum
Last update: January 26th (2025) Hajime Kawahara for v2.0
In this getting started guide, we will use ExoJAX to simulate a high-resolution emission spectrum from an atmosphere with CO molecular absorption and hydrogen molecule CIA continuum absorption as the opacity sources. We will then add appropriate noise to the simulated spectrum to create a mock spectrum and perform spectral retrieval using NumPyro’s HMC NUTS.
The author wrote this Jupyter notebook on a gaming laptop equipped with an RTX 3080 GPU, so it is recommended to use a machine with similar or higher GPU specifications. However, except for the HMC NUTS part, the code should also work on lower-spec systems. Now, let’s get started!
First, we recommend 64-bit if you do not think about numerical errors. Use jax.config to set 64-bit. (But note that 32-bit is sufficient in most cases. Consider to use 32-bit (faster, less device memory) for your real use case.)
from jax import config
config.update("jax_enable_x64", True)
The following schematic figure explains how ExoJAX works; (1) loading
databases (*db
), (2) calculating opacity (opa
), (3) running
atmospheric radiative transfer (art
), (4) applying operations on the
spectrum (sop
)
In this “getting started” guide, there are two opacity sources, CO and
CIA. Their respective databases, mdb
and cdb
, are converted by
opa
into the opacity of each atmospheric layer, which is then used
in the radiative transfer calculation performed by art
. Finally,
sop
convolves the rotational effects and instrumental profiles,
generating the emission spectrum.
mdb
/cdb
–> opa
–> art
–> sop
—> spectrum
This spectral model is incorporated into the probabilistic model in NumPyro, and retrieval is performed by sampling using HMC-NUTS.
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Figure. Structure of ExoJAX
1. Loading a molecular database using mdb
ExoJAX has an API for molecular databases, called mdb
(or adb
for atomic datbases). Prior to loading the database, define the
wavenumber range first.
from exojax.utils.grids import wavenumber_grid
nu_grid, wav, resolution = wavenumber_grid(
22920.0, 23000.0, 3500, unit="AA", xsmode="premodit"
)
print("Resolution=", resolution)
xsmode = premodit xsmode assumes ESLOG in wavenumber space: xsmode=premodit ====================================================================== The wavenumber grid should be in ascending order. The users can specify the order of the wavelength grid by themselves. Your wavelength grid is in * descending * order ====================================================================== Resolution= 1004211.9840291934
/home/kawahara/exojax/src/exojax/spec/unitconvert.py:63: UserWarning: Both input wavelength and output wavenumber are in ascending order.
warnings.warn(
Then, let’s load the molecular database. We here use Carbon monoxide in
Exomol. CO/12C-16O/Li2015
means
Carbon monoxide/ isotopes = 12C + 16O / database name
. You can check
the database name in the ExoMol website (https://www.exomol.com/).
from exojax.spec.api import MdbExomol
mdb = MdbExomol(".database/CO/12C-16O/Li2015", nurange=nu_grid)
/home/kawahara/exojax/src/exojax/utils/molname.py:197: FutureWarning: e2s will be replaced to exact_molname_exomol_to_simple_molname.
warnings.warn(
/home/kawahara/exojax/src/exojax/utils/molname.py:91: FutureWarning: exojax.utils.molname.exact_molname_exomol_to_simple_molname will be replaced to radis.api.exomolapi.exact_molname_exomol_to_simple_molname.
warnings.warn(
/home/kawahara/exojax/src/exojax/utils/molname.py:91: FutureWarning: exojax.utils.molname.exact_molname_exomol_to_simple_molname will be replaced to radis.api.exomolapi.exact_molname_exomol_to_simple_molname.
warnings.warn(
HITRAN exact name= (12C)(16O)
radis engine = vaex
Molecule: CO
Isotopologue: 12C-16O
Background atmosphere: H2
ExoMol database: None
Local folder: .database/CO/12C-16O/Li2015
Transition files:
=> File 12C-16O__Li2015.trans
Broadening code level: a0
/home/kawahara/anaconda3/lib/python3.10/site-packages/radis-0.15.2-py3.10.egg/radis/api/exomolapi.py:685: AccuracyWarning: The default broadening parameter (alpha = 0.07 cm^-1 and n = 0.5) are used for J'' > 80 up to J'' = 152
warnings.warn(
2. Computation of the Cross Section using opa
ExoJAX has various opacity calculator classes, so-called opa
. Here,
we use a memory-saved opa, OpaPremodit
. We assume the robust
tempreature range we will use is 500-1500K.
from exojax.spec.opacalc import OpaPremodit
opa = OpaPremodit(mdb, nu_grid, auto_trange=[500.0, 1500.0], dit_grid_resolution=1.0)
/home/kawahara/exojax/src/exojax/spec/opacalc.py:215: UserWarning: dit_grid_resolution is not None. Ignoring broadening_parameter_resolution.
warnings.warn(
OpaPremodit: params automatically set.
default elower grid trange (degt) file version: 2
Robust range: 485.7803992045456 - 1514.171191195336 K
OpaPremodit: Tref_broadening is set to 866.0254037844389 K
# of reference width grid : 2
# of temperature exponent grid : 2
uniqidx: 0it [00:00, ?it/s]
Premodit: Twt= 1108.7151960064205 K Tref= 570.4914318566549 K
Making LSD:|####################| 100%
Then let’s compute cross section for two different temperature 500 and 1500 K for P=1.0 bar. opa.xsvector can do that!
P = 1.0 # bar
T_1 = 500.0 # K
xsv_1 = opa.xsvector(T_1, P) # cm2
T_2 = 1500.0 # K
xsv_2 = opa.xsvector(T_2, P) # cm2
Plot them. It can be seen that different lines are stronger at different temperatures.
import matplotlib.pyplot as plt
plt.plot(nu_grid, xsv_1, label=str(T_1) + "K") # cm2
plt.plot(nu_grid, xsv_2, alpha=0.5, label=str(T_2) + "K") # cm2
plt.yscale("log")
plt.legend()
plt.xlabel("wavenumber (cm-1)")
plt.ylabel("cross section (cm2)")
plt.show()
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3. Atmospheric Radiative Transfer
ExoJAX can solve the radiative transfer and derive the emission
spectrum. To do so, ExoJAX has art
class. ArtEmisPure
means
Atomospheric Radiative Transfer for Emission with Pure absorption. So,
ArtEmisPure
does not include scattering. We set the number of the
atmospheric layer to 200 (nlayer) and the pressure at bottom and top
atmosphere to 100 and 1.e-5 bar.
Since v1.5, one can choose the rtsolver (radiative transfer solver) from
the flux-based 2 stream solver (fbase2st
) and the intensity-based
n-stream sovler (ibased
). Use rtsolver
option. In the latter
case, the number of the stream (nstream
) can be specified. Note that
the default rtsolver for the pure absorption (i.e. no scattering nor
reflection) has been ibased
since v1.5. In our experience,
ibased
is faster and more accurate than fbased
.
from exojax.spec.atmrt import ArtEmisPure
art = ArtEmisPure(
nu_grid=nu_grid,
pressure_btm=1.0e1,
pressure_top=1.0e-5,
nlayer=100,
rtsolver="ibased",
nstream=8,
)
rtsolver: ibased
Intensity-based n-stream solver, isothermal layer (e.g. NEMESIS, pRT like)
Let’s assume the power law temperature model, within 500 - 1500 K.
\(T = T_0 P^\alpha\)
where \(T_0=1200\) K and \(\alpha=0.1\).
art.change_temperature_range(500.0, 1500.0)
Tarr = art.powerlaw_temperature(1200.0, 0.1)
Also, the mass mixing ratio of CO (MMR) should be defined.
mmr_profile = art.constant_mmr_profile(0.01)
Surface gravity is also important quantity of the atmospheric model, which is a function of planetary radius and mass. Here we assume 1 RJ and 10 MJ.
from exojax.utils.astrofunc import gravity_jupiter
gravity = gravity_jupiter(1.0, 10.0)
In addition to the CO cross section, we would consider collisional
induced
absorption
(CIA) as a continuum opacity. cdb
class can be used.
from exojax.spec.contdb import CdbCIA
from exojax.spec.opacont import OpaCIA
cdb = CdbCIA(".database/H2-H2_2011.cia", nurange=nu_grid)
opacia = OpaCIA(cdb, nu_grid=nu_grid)
H2-H2
Before running the radiative transfer, we need cross sections for
layers, called xsmatrix
for CO and logacia_matrix
for CIA
(strictly speaking, the latter is not cross section but coefficient
because CIA intensity is proportional density square). See
here for the details.
xsmatrix = opa.xsmatrix(Tarr, art.pressure)
logacia_matrix = opacia.logacia_matrix(Tarr)
Convert them to opacity
dtau_CO = art.opacity_profile_xs(xsmatrix, mmr_profile, mdb.molmass, gravity)
vmrH2 = 0.855 # VMR of H2
mmw = 2.33 # mean molecular weight of the atmosphere
dtaucia = art.opacity_profile_cia(logacia_matrix, Tarr, vmrH2, vmrH2, mmw, gravity)
Add two opacities.
dtau = dtau_CO + dtaucia
Then, run the radiative transfer. As you can see, the emission spectrum has been generated. This spectrum shows a region near 4360 cm-1, or around 22940 AA, where CO features become increasingly dense. This region is referred to as the band head. If you’re interested in why the band head occurs, please refer to Quatum states of Carbon Monoxide and Fortrat Diagram.
F = art.run(dtau, Tarr)
fig = plt.figure(figsize=(15, 4))
plt.plot(nu_grid, F)
plt.xlabel("wavenumber (cm-1)")
plt.ylabel("flux (erg/s/cm2/cm-1)")
plt.show()
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You can check the contribution function too! You should check if the
dominant contribution is within the layer. If not, you need to change
pressure_top
and pressure_btm
in ArtEmisPure
from exojax.plot.atmplot import plotcf
cf = plotcf(nu_grid, dtau, Tarr, art.pressure, art.dParr)
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4. Spectral Operators: rotational broadening, instrumental profile, Doppler velocity shift and so on, any operation on spectra.
The above spectrum is called “raw spectrum” in ExoJAX. The effects
applied to the raw spectrum is handled in ExoJAX by the spectral
operator (sop
). First, we apply the spin rotational broadening of a
planet.
from exojax.spec.specop import SopRotation
sop_rot = SopRotation(nu_grid, vsini_max=100.0)
vsini = 10.0
u1 = 0.0
u2 = 0.0
Frot = sop_rot.rigid_rotation(F, vsini, u1, u2)
fig = plt.figure(figsize=(15, 4))
plt.plot(nu_grid, F, label="raw spectrum")
plt.plot(nu_grid, Frot, label="rotated")
plt.xlabel("wavenumber (cm-1)")
plt.ylabel("flux (erg/s/cm2/cm-1)")
plt.legend()
plt.show()
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Then, the instrumental profile with relative radial velocity shift is
applied. Also, we need to match the computed spectrum to the data grid.
This process is called sampling
(but just interpolation though).
Below, let’s perform a simulation that includes noise for use in later
analysis.
from exojax.spec.specop import SopInstProfile
from exojax.utils.instfunc import resolution_to_gaussian_std
sop_inst = SopInstProfile(nu_grid, vrmax=1000.0)
RV = 40.0 # km/s
resolution_inst =70000.0
beta_inst = resolution_to_gaussian_std(resolution_inst)
Finst = sop_inst.ipgauss(Frot, beta_inst)
nu_obs = nu_grid[::5][:-50]
from numpy.random import normal
noise = 500.0
Fobs = sop_inst.sampling(Finst, RV, nu_obs) + normal(0.0, noise, len(nu_obs))
fig = plt.figure(figsize=(12, 6))
ax = fig.add_subplot(211)
plt.plot(nu_grid, Frot, label="rotated")
plt.plot(nu_grid, Finst, label="rotated+IP")
plt.ylabel("flux (erg/s/cm2/cm-1)")
plt.legend()
ax = fig.add_subplot(212)
plt.errorbar(nu_obs, Fobs, noise, fmt=".", label="rotated + RV + IP (sampling)", color="gray",alpha=0.5)
plt.xlabel("wavenumber (cm-1)")
plt.legend()
plt.show()
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5. Retrieval of an Emission Spectrum
Next, let’s perform a “retrieval” on the simulated spectrum created above. Retrieval involves estimating the parameters of an atmospheric model in the form of a posterior distribution based on the spectrum. To do this, we first need a model. Here, we have compiled the forward modeling steps so far and defined the model as follows. The spectral model has six parameters.
def fspec(T0, alpha, mmr, g, RV, vsini):
#molecule
Tarr = art.powerlaw_temperature(T0, alpha)
xsmatrix = opa.xsmatrix(Tarr, art.pressure)
mmr_arr = art.constant_mmr_profile(mmr)
dtau = art.opacity_profile_xs(xsmatrix, mmr_arr, opa.mdb.molmass, g)
#continuum
logacia_matrix = opacia.logacia_matrix(Tarr)
dtaucH2H2 = art.opacity_profile_cia(logacia_matrix, Tarr, vmrH2, vmrH2,
mmw, g)
#total tau
dtau = dtau + dtaucH2H2
F = art.run(dtau, Tarr)
Frot = sop_rot.rigid_rotation(F, vsini, u1, u2)
Finst = sop_inst.ipgauss(Frot, beta_inst)
mu = sop_inst.sampling(Finst, RV, nu_obs)
return mu
Let’s verify that spectra are being generated from fspec
with
various parameter sets.
fig = plt.figure(figsize=(12, 3))
plt.plot(nu_obs, fspec(1200.0, 0.09, 0.01, gravity_jupiter(1.0, 1.0), 40.0, 10.0),label="model")
plt.plot(nu_obs, fspec(1100.0, 0.12, 0.01, gravity_jupiter(1.0, 10.0), 20.0, 5.0),label="model")
[<matplotlib.lines.Line2D at 0x77fcf8b386a0>]
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NumPyro is a probabilistic programming language (PPL), which requires
the definition of a probabilistic model. In the probabilistic model
model_prob
defined below, the prior distributions of each parameter
are specified. The previously defined spectral model is used within this
probabilistic model as a function that provides the mean \(\mu\).
The spectrum is assumed to be generated according to a Gaussian
distribution with this mean and a standard deviation \(\sigma\).
i.e. \(f(\nu_i) \sim \mathcal{N}(\mu(\nu_i; {\bf p}), \sigma^2 I)\),
where \({\bf p}\) is the spectral model parameter set, which are the
arguments of fspec
.
from numpyro.infer import MCMC, NUTS
import numpyro.distributions as dist
import numpyro
from jax import random
def model_prob(spectrum):
#atmospheric/spectral model parameters priors
logg = numpyro.sample('logg', dist.Uniform(4.0, 5.0))
RV = numpyro.sample('RV', dist.Uniform(35.0, 45.0))
mmr = numpyro.sample('MMR', dist.Uniform(0.0, 0.015))
T0 = numpyro.sample('T0', dist.Uniform(1000.0, 1500.0))
alpha = numpyro.sample('alpha', dist.Uniform(0.05, 0.2))
vsini = numpyro.sample('vsini', dist.Uniform(5.0, 15.0))
mu = fspec(T0, alpha, mmr, 10**logg, RV, vsini)
#noise model parameters priors
sigmain = numpyro.sample('sigmain', dist.Exponential(1.e-3))
numpyro.sample('spectrum', dist.Normal(mu, sigmain), obs=spectrum)
Note that we did not account for the effects of limb darkening. However, in actual analyses, one possible approach might be to use an uninformative prior, such as the one proposed by Kipping.
from exojax.spec.limb_darkening import ld_kipping
q1 = numpyro.sample('q1', dist.Uniform(0.0,1.0))
q2 = numpyro.sample('q2', dist.Uniform(0.0,1.0))
u1,u2 = ld_kipping(q1,q2)
Now, let’s define NUTS and start sampling.
rng_key = random.PRNGKey(0)
rng_key, rng_key_ = random.split(rng_key)
num_warmup, num_samples = 500, 1000
#kernel = NUTS(model_prob, forward_mode_differentiation=True)
kernel = NUTS(model_prob, forward_mode_differentiation=False)
Since this process will take several hours, feel free to go for a long lunch break!
mcmc = MCMC(kernel, num_warmup=num_warmup, num_samples=num_samples)
mcmc.run(rng_key_, spectrum=Fobs)
mcmc.print_summary()
sample: 100%|██████████| 1500/1500 [3:32:24<00:00, 8.50s/it, 255 steps of size 2.63e-02. acc. prob=0.94]
mean std median 5.0% 95.0% n_eff r_hat
MMR 0.01 0.00 0.01 0.01 0.01 301.05 1.00
RV 39.95 0.06 39.95 39.84 40.05 675.86 1.00
T0 1196.47 6.93 1196.30 1183.85 1206.73 400.13 1.00
alpha 0.10 0.00 0.10 0.09 0.10 335.22 1.00
logg 4.45 0.06 4.45 4.37 4.56 354.23 1.00
sigmain 472.25 13.78 471.80 451.90 495.79 837.97 1.00
vsini 9.79 0.17 9.79 9.54 10.10 351.43 1.00
Number of divergences: 0
After returning from your long lunch, if you’re lucky and the sampling is complete, let’s write a predictive model for the spectrum.
from numpyro.diagnostics import hpdi
from numpyro.infer import Predictive
import jax.numpy as jnp
# SAMPLING
posterior_sample = mcmc.get_samples()
pred = Predictive(model_prob, posterior_sample, return_sites=['spectrum'])
predictions = pred(rng_key_, spectrum=None)
median_mu1 = jnp.median(predictions['spectrum'], axis=0)
hpdi_mu1 = hpdi(predictions['spectrum'], 0.9)
fig, ax = plt.subplots(nrows=1, ncols=1, figsize=(15, 4.5))
ax.plot(nu_obs, median_mu1, color='C1')
ax.fill_between(nu_obs,
hpdi_mu1[0],
hpdi_mu1[1],
alpha=0.3,
interpolate=True,
color='C1',
label='90% area')
ax.errorbar(nu_obs, Fobs, noise, fmt=".", label="mock spectrum", color="black",alpha=0.5)
plt.xlabel('wavenumber (cm-1)', fontsize=16)
plt.legend(fontsize=14)
plt.tick_params(labelsize=14)
plt.show()
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You can see that the predictions are working very well! Let’s also display a corner plot. Here, we’ve used ArviZ for visualization.
import arviz
pararr = ['T0', 'alpha', 'logg', 'MMR', 'vsini', 'RV']
arviz.plot_pair(arviz.from_numpyro(mcmc),
kind='kde',
divergences=False,
marginals=True)
plt.show()
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The correlation between T0
and alpha
arises because both are
parameters of the temperature model. The degeneracy between MMR and
logg
occurs because, in the case of molecular absorption alone,
opacity depends only on the ratio \(\text{MMR}/g\), leading to
complete degeneracy. However, the presence of CIA breaks this
degeneracy. For more details, please refer to Kawashima et
al.