Today's Edition
ABU DHABI (WAM)
New York University Abu Dhabi (NYUAD) Research Scientist, Jasmina Blecic, and Associate Professor, Ian Dobbs-Dixon, from the Centre for Astrophysics and Space Science (CASS), along with colleagues from the James Webb Space Telescope Transiting Exoplanet Early Release Science (JTEC-ERS) team, have harnessed the power of NASA’s James Webb Telescope to discover new insights about the climate of a giant, Jupiter-sized exoplanet.
This includes the first observation of its dust-filled clouds.
Recently published in Nature Astronomy, the researchers detail how they tested the unparalleled capabilities of Webb’s Mid-Infrared Instrument (MIRI) in the study and observed the entire orbit of WASP-43b, a giant, gas-filled exoplanet.
These “phase curve” observations, conducted during Webb’s inaugural year, revealed the temperature distribution across the entire planet and shed light on the planetary climate.
Researchers found thick clouds, a surprising lack of methane on the planet’s nightside, and ubiquitous water presence throughout its atmosphere.
This is the first time clouds have been inferred on the nightside of the planet; they were found at much higher altitudes in the planetary atmosphere compared to typical clouds observed on Earth.
WASP-43b shares a comparable size and mass with Jupiter, yet it diverges significantly in its planetary characteristics.
Its host star, WASP-43A, is much cooler and redder than our sun and is around 86 light years away from the Earth.
WASP-43b orbits closely to its star, resulting in a year lasting only 19.5 hours.
This proximity causes the planet's rotation to synchronize with its orbit, with one side always facing the star, similar to the tidal locking observed with our moon.
As a result, one-half of the planet (dayside) is permanently illuminated and very hot, while the other half (nightside) is permanently shadowed and much colder.
Blecic said, "We observed this planet while it orbits around its star using an infrared spectrometer so that we could study the light emerging from the different regions of its atmosphere."
“This allowed us to distinguish between the day and nightside temperatures, and identify the presence of clouds and various molecules. Different chemical species absorb light at different wavelengths in infrared. Combining this fact with observations of the entire orbit, we were able to constrain the chemical composition, cloud coverage, and heat redistribution across the whole atmosphere and draw conclusions about the planet's climate,” he added.
The team found that WASP-43b’s permanently illuminated dayside is as hot as 2285°F (1250°C), while the planet’s nightside, although permanently shadowed, is still very hot at 1,115°F (600°C).
“The absence of direct sunlight on the planet's nightside causes significant temperature differences between the day and night sides, which prompts the formation of exceptionally strong winds,” said Dobbs-Dixon, an expert in 3-dimensional atmospheric models and heat redistribution of exoplanetary atmospheres.
“While winds on Earth form in a similar manner due to variations in temperature, the close proximity of WASP-43b to its host star results in much more extreme temperature differences. This produced winds of thousands of kilometres per hour, far surpassing those on Earth, crucial for the distribution of heat and shaping the overall planetary climate.”
Additionally, comparisons of the planet’s temperature map with complex 3D atmospheric models demonstrated that this temperature contrast is stronger than expected for a cloud-free atmosphere. This suggests that the planet’s nightside is shrouded in a thick layer of clouds that blocks much of the infrared radiation that would otherwise be observed. Unlike Earth’s water clouds, the clouds on this extremely hot planet resemble dust and are composed of rocks and minerals.
Despite this thick layer of clouds, the JTEC-ERS team also detected clear signals of water on the planet's nightside.
This allowed them to determine, for the first time, the cloud height and thickness, unveiling their unusual altitude and density compared to Earth's clouds.
The researchers also detected wind-driven mixing, called “chemical disequilibrium”, that swiftly transports gas throughout the planet's atmosphere and results in uniform atmospheric chemistry.
