The James Webb Space Telescope (JWST) has made a groundbreaking discovery, offering insights into the ancient origins of our planet. By observing two young stars' planet-forming disks in the Taurus star-forming region, located 430 light years away, James Webb Telescope detected a chilly "steam" or excess water vapour.
Scientists believe that planets, including Earth, form through a process called "pebble accretion." Tiny rocks, coated in ice, start in the outer regions of a planet-forming disk. As they drift inward, these icy pebbles pass a boundary known as the "snow line," where the disk's temperature is too high for water to exist as ice. This causes the icy coating on the pebbles to vaporise, releasing cold water vapour into the inner part of the disk, Space.com reported.
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JWST's Mid-Infrared Instrument (MIRI) detected this water vapour, supporting the theory of pebble accretion. Andrea Banzatti of Texas State University, lead author of a related paper, highlighted how JWST linked water vapour in the inner disk to the migration of icy pebbles.
The telescope observed four planet-forming disks, finding water vapour only in the two compact disks. The extended disks, belonging to systems CI Tau and IQ Tau, displayed rings in images taken by the Atacama Large Millimetre/submillimetre Array (ALMA) in Chile. One theory suggests that when migrating pebbles encounter higher pressure regions, their inward drift slows, forming rings.
Despite these findings, questions linger about the accretion process itself, how pebbles stick together to form larger objects without breaking apart. Colette Salyk of Vassar College notes that the JWST observations not only inform us about exoplanet formation but
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