Spitzer Phase Curve Constraints for WASP-43b at 3.6 and 4.5 microns

TL;DR

This study uses Spitzer phase curves to analyze heat redistribution and atmospheric composition of exoplanet WASP-43b, revealing potential cloud effects and deriving metallicity estimates consistent with solar values.

Contribution

First Spitzer phase curve observations of WASP-43b at 3.6 and 4.5 microns, revealing atmospheric dynamics and composition constraints, and proposing cloud/haze effects to explain deviations from models.

Findings

Strong day-night contrast consistent with HST data.

Derived water abundance and metallicity estimates near solar values.

Identified possible cloud/haze influence on thermal emission.

Abstract

Previous measurements of heat redistribution efficiency (the ability to transport energy from a planet's highly irradiated dayside to its eternally dark nightside) show considerable variation between exoplanets. Theoretical models predict a positive correlation between heat redistribution efficiency and temperature for tidally locked planets; however, recent HST WASP-43b spectroscopic phase curve results are inconsistent with current predictions. Using the Spitzer Space Telescope, we obtained a total of three phase curve observations of WASP-43b (P=0.813 days) at 3.6 and 4.5 microns. The first 3.6 micron visit exhibits spurious nightside emission that requires invoking unphysical conditions in our cloud-free atmospheric retrievals. The two other visits exhibit strong day-night contrasts that are consistent with the HST data. To reconcile the departure from theoretical predictions, WASP-43b would need to have a high-altitude, nightside cloud/haze layer blocking its thermal emission. Clouds/hazes could be produced within the planet's cool, nearly retrograde mid-latitude flows before dispersing across its nightside at high altitudes. Since mid-latitude flows only materialize in fast-rotating ($\lesssim1$ day) planets, this may explain an observed trend connecting measured day-night contrast with planet rotation rate that matches all current Spitzer phase curve results. Combining independent planetary emission measurements from multiple phases, we obtain a precise dayside hemisphere H2O abundance ($2.5\times 10^{-5} - 1.1\times 10^{-4}$ at 1$\sigma$ confidence) and, assuming chemical equilibrium and a scaled solar abundance pattern, we derive a corresponding metallicity estimate that is consistent with being solar (0.4 -- 1.7). Using the retrieved global CO+CO2 abundance under the same assumptions, we estimate a comparable metallicity of 0.3 - 1.7$\times$ solar. (Abridged)