ASTR 350 · Lecture 02

The Transit Method: Light Curves, Depth, and Duration

Catching a planet in silhouette

Learning Goals

  1. Derive the transit-depth relation connecting a dip in stellar brightness to the planet-to-star radius ratio.
  2. Derive an approximate transit-duration relation and explain what additional information a transit provides beyond radial velocity.
  3. Reproduce the real discovery measurement of HD 209458 b, the first transiting exoplanet, and cross-check it against this course’s computed values.

Reading anchor: OpenStax Astronomy 2e (local extracted reference copy: references/openstax-astronomy-2e-extracted.txt) introduces exoplanet detection methods in the "Exoplanets" section of Chapter 7 (Other Worlds: An Introduction to the Solar System) and astrobiology topics (habitable zone, biosignatures, the Drake equation) in Chapter 30 (Life in the Universe); these citations follow the ASTR320/330 precedent of using native OpenStax chapter numbering, extrapolated by analogy rather than independently cross-checked against embedded figure/table numbering this session -- flagged for human spot-check in reference-log.md. Nearly every quantitative derivation in this course (the radial-velocity semi-amplitude equation, transit depth/duration, the mass-radius interior degeneracy, the radiative-equilibrium habitable-zone boundary, and the Drake equation as a structured estimation framework) goes well beyond OpenStax Astronomy 2e’s introductory, descriptive treatment; each lecture states explicitly where this course extends beyond the assigned reading.

Why This Matters

Lecture 01’s radial-velocity method gives a planet’s mass (times sin i) but says nothing about its size. The transit method, derived here, supplies the missing radius -- and, combined with radial velocity for the same planet, breaks the sin(i) degeneracy exactly and yields the planet’s true mass, true radius, and therefore its bulk density (Lecture 06).

Opening Phenomenon

On September 9 and 16, 1999, David Charbonneau’s team measured a real, repeatable 1.5% dip in the brightness of HD 209458, lasting about 3 hours every 3.52 days -- the first confirmed transiting exoplanet, simultaneously announced by two independent teams in the same issue of the Astrophysical Journal, and the system this course uses throughout its atmospheres unit (Lectures 07-08).

First question: what here is directly observed or a published/live-verified measurement, and what follows only once a physical law is derived and applied?

Terms for This Lecture

transit

Definition: Transit denotes the physical quantity, process, or inference concept captured by this lecture-specific statement: For a planet of radius Rp transiting a star of radius Rstar, the fractional decrease in observed flux at mid-transit (ignoring stellar limb darkening) is the ratio of blocked area to total area: delta = (Rp/Rstar)^2, a purely geometric relation independent of the planet’s mass or...

Why it matters here: Lecture 01’s radial-velocity method gives a planet’s mass (times sin i) but says nothing about its size. The transit method, derived here, supplies the missing radius -- and, combined with radial velocity for the same planet, breaks the sin(i) degeneracy exactly and yields the planet’s true mass, true radius, and therefore its...

Relationships: It is used with transit depth to interpret the lecture model. The quantitative connection is the working relation \(\delta = \left(\dfrac{R_p}{R_\ast}\right)^{2}, \qquad T_{\rm dur} \approx \dfrac{P}{\pi}\arcsin\!\left(\dfrac{R_\ast}{a}\right)\).

Boundary or common confusion: Assuming transit depth alone gives a planet’s absolute size. Transit depth only ever gives the ratio Rp/Rstar; converting to an absolute planet radius requires an independently known stellar radius (from the star’s spectral type, parallax-based luminosity, or asteroseismology), so an error in the assumed stellar radius propagates directly and proportionally...

Evidence We Need to Explain

Derivation and Model

Quantitative Tool

\[ \delta = \left(\dfrac{R_p}{R_\ast}\right)^{2}, \qquad T_{\rm dur} \approx \dfrac{P}{\pi}\arcsin\!\left(\dfrac{R_\ast}{a}\right) \]

Worked Example

  1. HD 209458 b (live-verified this session): Rp = 1.359 RJup, Rstar = 1.20 Rsun. Computed transit depth delta = (Rp/Rstar)^2 = 1.30%, matching the discovery team’s measured 1.5% dip to within the precision of the adopted stellar radius.
  2. Computed transit duration from P = 3.525 d and a = 0.0475 AU: T = (P/pi) arcsin(Rstar/a) = 3.17 h, matching the discovery paper’s reported ≈3-hour transit.
  3. Cross-checking with Lecture 01’s method: HD 209458 b’s radial-velocity semi-amplitude, predicted from its independently known true mass (0.682 MJup) and inclination (86.71 degrees, from the transit), gives K = 82.8 m/s, matching the published measured value (84.27 m/s) -- direct confirmation that the two independent detection methods agree on the same real planet.

Visual Reasoning

Trace the reasoning chain from raw observation or live-verified/published data to derived physical law to inferred quantity in this lecture’s figure.

  • Which stage is directly observed or a real published measurement?
  • Which stage is the physical law or derivation step?
  • What would change if an assumption in the derivation failed?
Lecture 02: The Transit Method: Light Curves, Depth, and DurationTime from mid-transit (hours)Relative fluxHD 209458 b: measured transit depth 1.5% over ~3.0 h (Charbonneau et al. 2000); this course’s computed (Rp/Rs)² = 1.30%.
The Transit Method: Light Curves, Depth, and Duration: from observation to inferred quantity.

Common Misconception

Assuming transit depth alone gives a planet’s absolute size. Transit depth only ever gives the ratio Rp/Rstar; converting to an absolute planet radius requires an independently known stellar radius (from the star’s spectral type, parallax-based luminosity, or asteroseismology), so an error in the assumed stellar radius propagates directly and proportionally into every transiting planet’s reported radius.

Active Learning Segment

Using T ∝ P^(1/3) (from a ∝ P^(2/3) via Kepler’s third law) and Rstar/a ∝ a^(-1), explain qualitatively why short-period, close-in planets have both higher transit probability and shorter transit duration than long-period planets, and why this makes hot Jupiters disproportionately easy to detect by transit as well as by radial velocity.

Lab Connection

Lab 01 also reproduces this lecture’s HD 209458 b transit-depth and duration calculations and cross-checks the two independent detection methods against each other for the same real planet.

Synthesis

The transit method supplies exactly what radial velocity cannot: a planet’s radius and (via the transit-fixed inclination) an exact, not minimum, mass when combined with radial velocity -- together the two methods gave HD 209458 b the first bulk density ever measured for a world outside the solar system, opening the door to every interior and atmospheric characterization technique this course develops later.

References