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Astronomers use ALMA to map millimeter and submillimeter light from planet-forming disks, then separate dust emission from molecular signals in the gas. Continuum images reveal where dust is concentrated; spectral-line observations show which molecules are present and, when resolved by velocity, how gas moves. Rings and gaps are clues to disk structure—not automatic proof that a planet caused them.

What ALMA measures in a planet-forming disk

ALMA is an array of radio telescopes that observes at millimeter and submillimeter wavelengths. Its published receiver overview spans approximately 35–950 GHz, corresponding to wavelengths from about 8.6 mm to 0.32 mm. This is the receiver system’s technical range, not a guarantee that every band is available for every observing program; operational availability can change. ALMA’s receiver overview describes the system.

At these wavelengths, astronomers commonly study two complementary signals: continuum emission, which helps map dust, and spectral lines, which reveal emission from particular molecules in the gas. ALMA’s star and planet formation overview explains how its capabilities are applied to these systems.

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Continuum images trace dust

A continuum image maps emission across a range of frequencies rather than isolating one molecular transition. In a disk, this emission is used to trace the distribution of dust grains that radiate at millimeter wavelengths. Bright rings, dimmer gaps, and uneven patches can show that the emitting material is not spread uniformly.

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Brightness is a measured signal, not a direct, assumption-free inventory of all dust or total disk mass. Turning it into a physical quantity requires interpretation and models; the observed pattern itself does not establish what caused it.

Spectral lines trace gas and its motion

A spectral-line observation isolates emission at frequencies associated with molecules. Tracers such as carbon monoxide isotopologues (12CO and 13CO), CS, and N2H+ can help investigate gas distribution and conditions. Different species and isotopologues sample different conditions and locations, so astronomers compare tracers rather than treating any single line as a complete picture of the disk.

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Lines also carry velocity information. The observed frequency shifts and line profiles encode motion along the line of sight. When an observation has sufficient spectral resolution, astronomers can map how gas rotates or moves in relation to the disk instead of seeing only a static-looking outline.

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How astronomers turn observations into disk maps

An observing strategy starts with a scientific question: for example, whether a disk has dust substructure, how gas is distributed, or how material is moving. The team chooses a target, frequency range, angular resolution, spectral resolution, and suitable continuum or molecular tracers. Not every project uses the same bands, molecules, or data-processing choices.

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  1. Choose the signal. Use continuum data to study the pattern of millimeter-emitting dust, spectral lines to examine particular molecular tracers, or both to compare dust and gas.
  2. Set spatial and velocity detail. Angular resolution controls the scale of structure that can be distinguished. Spectral resolution controls how finely differences in line-of-sight velocity can be separated.
  3. Calibrate and image the observations. The measurements are processed into images and, for line observations, maps across frequency or velocity. Projects that combine observations taken at different times may need methods to align and clean the data consistently; the exoALMA team describes project-developed methods for that task.
  4. Compare tracers and interpret the result. Researchers compare continuum and line maps, then use physical models to connect measured emission to possible distributions, conditions, and motions in the disk.

Resolution is a choice matched to the question, not one fixed setting that defines every ALMA image. For example, the exoALMA survey reported 100 milliarcseconds of angular resolution—about 14 au at typical source distances—and 26 m/s of spectral resolution. Those figures describe that dataset, not a universal ALMA capability for every observation. The survey release reports its targets and measurements.

What rings, gaps, and bright patches can—and cannot—tell us

High-resolution continuum images can show rings, gaps, and asymmetries in the dust emission. Those features are valuable evidence about disk structure and the processes that may shape it, but morphology alone does not identify a unique cause. A gap is not, by itself, a planet detection; its interpretation depends on the broader evidence, including gas observations and physical modeling.

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HL Tau: a landmark view of rings and gaps

ALMA’s 2014 image of HL Tau used a 15 km baseline and showed concentric bright rings separated by gaps at roughly 35 milliarcseconds of image resolution. It demonstrated how fine spatial detail can reveal disk substructure, but the image should be read as evidence of rings and gaps—not as proof that every gap contains a planet. ALMA’s HL Tau release describes the observation.

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PDS 70: dust around a system with known planets

In PDS 70, an ALMA Band 3 observation at a wavelength of 3 mm reported localized dust accumulation outside the orbits of the system’s two known planets. This offers a useful example of placing a millimeter continuum map alongside knowledge of an established planetary system: ALMA observes the remaining disk material, while the interpretation draws on the system’s wider context. The PDS 70 release describes the observation.

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How survey and detailed observations answer different questions

A highly resolved study of selected disks can examine detailed structure and kinematics. A survey can instead compare disks across populations, environments, or ages. These approaches complement one another: a close look at a few systems provides detail, while a broader sample helps place disk behavior in context.

exoALMA: structure, temperature, and velocity

The exoALMA survey observed 12CO, 13CO, and CS alongside continuum. Its release reports that the program used the data to map disk density, temperature, and velocity structure, with the study-specific angular and spectral resolutions noted above. Comparing molecular tracers with continuum helps researchers investigate how gas and dust relate rather than relying on one image alone. Read the exoALMA survey account.

AGE-PRO: comparing disks across ages and regions

The AGE-PRO program observed 30 protoplanetary disks around Sun-like stars in Ophiuchus, Lupus, and Upper Scorpius. The sample included objects ranging from under one million to over five million years old, and the ALMA release reports 12 papers in a special issue of The Astrophysical Journal. Its comparison of gas and dust evolution illustrates a survey approach: looking across many systems to investigate how disks change, rather than using one especially detailed image as a stand-in for all disks. ALMA’s AGE-PRO release provides the program details.

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ALMA also observes disks in earlier and unusual environments

L1527 IRS: from infalling material to disk rotation

Not every ALMA result concerns a mature planet-forming disk. In 2026, an eDisk result described an approximately 16 au-wide transition zone in L1527 IRS between infalling envelope material and orderly disk rotation. Resolving that change in gas motion helps researchers study disk formation at an early protostellar stage; it should not be conflated with observations of a more evolved disk where planets are forming. ALMA’s eDisk release describes the result.

Orion: ionized gas around exposed disks

ALMA can also examine signals beyond the main dust-and-molecular-gas picture. In 2025, an observatory account described H41α recombination-line emission at 3.1 mm from ionized shells around proplyds—disks exposed to nearby massive stars—in Orion. This is a more specialized application that shows how line observations can probe ionized material as well as molecules. The Orion release reports the observation.

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