Lab 04: Atmospheric Scale Height and Escape: HD 209458 b

Compute HD 209458 b's transmission-spectroscopy signal and Jeans escape parameter from first principles and compare to real HST measurements.

Apparatus and Setup

This lab computes HD 209458 b's atmospheric scale height and predicted transmission-spectroscopy signal amplitude (Lecture 07), then its Jeans escape parameter and naive mass-loss timescale (Lecture 08), comparing both to the real, published Hubble Space Telescope measurements.

Materials and Data

QuantityValue
Mass0.682 MJup
Radius1.359 RJup
Surface gravity (computed)9.57 m/s²
Exosphere temperature (real, HST-measured)10000 K
Real exosphere extent3.1 planetary radii
Real mass-loss rate3.0e+08 kg/s

Procedure

  1. Compute HD 209458 b's atmospheric scale height H at its exosphere temperature, for atomic hydrogen (mu=1 amu).
  2. Estimate the transit-depth signal amplitude for N=5 scale heights of absorbing atmosphere above the bulk continuum radius, using Lecture 07's formula, and compare to the real sodium-detection signal's approximate size.
  3. Compute HD 209458 b's Jeans escape parameter at the exosphere temperature and state whether the planet is in the classical Jeans-escape regime or the hydrodynamic blow-off regime.
  4. Compute the naive mass-loss timescale (current mass divided by the real, published mass-loss rate) and state whether the planet is in danger of complete evaporation within a typical few-Gyr system age at its current rate.

Analysis and Uncertainty

State explicitly that the naive mass-loss timescale assumes a constant mass-loss rate, which is very likely an overestimate of the timescale (an underestimate of total historical loss), because the host star's X-ray/UV activity -- and therefore the escape rate -- was almost certainly much higher earlier in the system's history (Lecture 08).

Deliverables

Assessment Criteria

References and Provenance