Transmission Spectroscopy
Astro 497, Week 9, Friday
TableOfContents()
Project Outline Feedback
Analyze/plot data for one object at a time
Allow user to select which object to analyze
Most transiting planets won't have mass measurements
question(md"""Is transmission spectroscopy limited by the thickness of a planet's atmosphere?
Since it gets more dense closer to the center of the planet, are we only able to resolve what makes up the outer edges of said planet's atmosphere?""")
Is transmission spectroscopy limited by the thickness of a planet's atmosphere?
Since it gets more dense closer to the center of the planet, are we only able to resolve what makes up the outer edges of said planet's atmosphere?
question(md"""While analyzing atmosphere composition, how to distinguish between the spectrum footprint produced by the planet and that produced by the observed background star?""")
While analyzing atmosphere composition, how to distinguish between the spectrum footprint produced by the planet and that produced by the observed background star?
LocalResource("../_assets/week2/circular_diagram.png", :width=>"80%")
Example Transmission Spectrum of WASP-43b
Main figure is transmission spectrum from Hubble WFC3
Inset figure is emission spectrum is Spitzer/IRAC 3.6 & 4.5μm
–- Kreidberg et al. 2015 & chapter from Handbook of Exoplanets
question(md"""Are the different filters used in a large variety of ways? Or or they just used based on certain properties of the planets that are being detected?""")
Are the different filters used in a large variety of ways? Or or they just used based on certain properties of the planets that are being detected?
What sets the scale for transmission spectroscopy signal?
Atmospheric Scale Height
$$H = \frac{k_B T}{\mu_m g}$$
Temperature: $T$
Mean molecular mass: $\mu_m$
Gravitational acceleration: $g$
Boltzmann constant: $k_B$
Assumes an isothermal atmosphere in hydrostatic equilbirum.
$$\rho(z) = \rho_0 \exp(-z/H)$$
Standard Transit depth
$$\delta \simeq \frac{\pi R_p^2}{\pi R_\star^2}$$
Radius of Planet: $R_p$ (where optically think at all wavelengths observed)
Radius of Star: $R_\star$
Increase in transit depth
$$\Delta\delta(\lambda) = \frac{\pi (R_p + N_H(\lambda) H)^2}{\pi R_\star^2} - \frac{\pi R_p^2}{\pi R_\star^2} \simeq 2 N_H \delta \left(\frac{H}{R_p}\right)$$
Number of scale heights of additional absorption: $N_H(\lambda)\simeq 2$ for cloud-free atmospheres at low resolution
Measurement wavelength: $\lambda$
Representative values
Planet | $\delta$ | $T$ | $g$ | $\mu_m$ | $\Delta\delta$ |
---|---|---|---|---|---|
(K) | (m/s) | (amu) | |||
Hot-Jupiter | $\simeq 10^{-2}$ | $\simeq 1300$ | $\simeq 25$ | $\simeq 2$ | $\simeq 10^{-4}$ |
Earth | $\simeq 10^{-4}$ | 273 | 10 | 28 | $\simeq 10^{-6}$ |
question(md"""Is a planet's transmission spectrum dependent on its temperature and mean molecular mass?
Is this a confounding factor when determining its atmospheric composition?""")
Is a planet's transmission spectrum dependent on its temperature and mean molecular mass?
Is this a confounding factor when determining its atmospheric composition?
Gallery of Transmission Spectroscopy measurements
–- Archive fo Exoplanet Transmission Spectra & Wakeford (2020)
question(md"""What information can we get about planets using transmission spectroscopy?""")
What information can we get about planets using transmission spectroscopy?
Things to look for
Sodium absorption ~0.6μm (HAT-P-1)
Rayleigh scattering (HD 189733b)
Lack of rayleigh scattering → clouds (GJ 436b, GJ 1214b)
Water Absorption ~1.4μm (WASP-127b, WASP-39b, WASP-107b, WASP-52b, HAT-P26b)
Lack of features (TRAPPIST)
question(md"If we are able to gather the light that has run into a planet's atmosphere, is there enough data to detect what the atmosphere of exoplanets consist of?")
If we are able to gather the light that has run into a planet's atmosphere, is there enough data to detect what the atmosphere of exoplanets consist of?
How to prioritize planets for detailed atmospheric characterization?
Transmission spectroscopy metric
$$\begin{eqnarray} \mathrm{TSM} & = & (\mathrm{Scale\; factor}) \times \left(\frac{R_p}{R_\oplus}\right)^3 \left(\frac{M_\oplus}{M_p}\right) \left(\frac{R_\odot}{R_\star}\right)^2 \left(\frac{T_{eq}}{K}\right) \times 10^{-m_J/5} \\ & \propto & R_p \frac{H}{R_\star} \left(\mathrm{stellar\; flux}\right) \end{eqnarray}$$
Proportional to SNR for transmission spectroscopy measurement
Starts with scale height model → assumes isothermal atmosphere with no clouds or hazes
Adds assumption of equilibrium temperature: $T_{eq} \equiv T_{\star,eff} \sqrt{\frac{R_\star}{a}} \left(2^{-1/4}\right)$
assumes zero albedo, full day-night heat redsitribution
Original TSM uses Apparent aagnitude in J band: $m_J$ → roughly corresponding to JWST's Near IR Imager and Slitless Spectrograph (NIRISS)
Variations on TSM use apparent magnitude in other bands.
question(md"""Are there any drawbacks to transmission spectroscopy?""")
Are there any drawbacks to transmission spectroscopy?
Reading Questions
Setup & Helper Code
ChooseDisplayMode()
using PlutoUI, PlutoTeachingTools
question(str; invite="Question") = Markdown.MD(Markdown.Admonition("tip", invite, [str]))
question (generic function with 1 method)
Built with Julia 1.8.2 and
PlutoTeachingTools 0.2.3PlutoUI 0.7.44
To run this tutorial locally, download this file and open it with Pluto.jl.
To run this tutorial locally, download this file and open it with Pluto.jl.
To run this tutorial locally, download this file and open it with Pluto.jl.
To run this tutorial locally, download this file and open it with Pluto.jl.