ALMA Sensitivity Calculator

Estimate continuum RMS, spectral-line RMS per channel, and SEFD for Atacama Large Millimeter/submillimeter Array observations using practical interferometric inputs.

Observation Inputs

Set values for your observing setup. This calculator provides fast planning estimates and is not a substitute for official proposal tools.

Estimated Results

Noise values are idealized thermal estimates. Real observations include calibration, weather, imaging weighting, uv coverage, and decorrelation effects.

Continuum RMS
Expected sensitivity for total continuum bandwidth
Line RMS / Channel
Per-channel sensitivity for selected velocity width
SEFD (single antenna)
System Equivalent Flux Density estimate
Effective On-Source Time
After overhead factor adjustment

Ready to calculate.

Complete Guide to the ALMA Sensitivity Calculator

What an ALMA Sensitivity Calculator Does

An ALMA sensitivity calculator is an observing-planning tool that estimates the thermal noise floor expected in an interferometric measurement. In practical terms, it answers one of the most important questions in proposal development and data strategy: how faint a signal can be detected for a given setup and on-source time. The calculator on this page is designed for fast scenario testing. You can vary frequency, integration time, antenna count, spectral resolution, and bandwidth, then immediately see how your expected RMS changes.

Sensitivity is central to nearly every science case with the Atacama Large Millimeter/submillimeter Array. Whether your objective is dust continuum in high-redshift galaxies, kinematics in protoplanetary disks, molecular gas in nearby spirals, or line diagnostics in star-forming clouds, your detectability threshold is governed by noise. A solid sensitivity estimate helps you decide if your project is feasible, whether your requested time is realistic, and how to balance line resolution with signal-to-noise ratio.

This ALMA sensitivity calculator is intentionally transparent. Instead of treating noise as an opaque output, it exposes the core inputs so observers can build intuition. If you double observing time, RMS improves by the square root of two. If you narrow your spectral channels, line RMS rises because each channel contains less bandwidth. If system temperature increases due to higher frequency or weather conditions, sensitivity degrades. These are first-order effects every user should understand.

How Sensitivity Is Calculated

For a simplified interferometric estimate, the continuum RMS can be approximated from the radiometer relation using antenna-based SEFD and baseline averaging. A practical form is:

SEFD = (2 k Tsys) / (ηa Aeff) × 1e26 [Jy]
σ = SEFD / (ηc × sqrt(Nant (Nant - 1) Npol Δν t))

In this equation, k is Boltzmann's constant, Tsys is system temperature, ηa is aperture efficiency, Aeff is geometric dish area multiplied by ηa, ηc is correlator efficiency, Nant is the number of antennas, Npol is the polarization count, Δν is bandwidth in Hz, and t is on-source integration time in seconds. The result is an RMS flux-density estimate in Jy, typically shown in microjansky or millijansky for readability.

The exact sensitivity delivered by a real ALMA dataset depends on additional factors such as atmospheric stability, phase correction quality, calibration strategy, flagged data, weighting in imaging, and array configuration. However, this foundational relation remains highly useful for early planning and parameter trade studies.

Continuum vs Spectral-Line Sensitivity

Continuum sensitivity and line sensitivity are related but not interchangeable. Continuum observations integrate over large effective bandwidth, often many GHz. Because noise decreases with the square root of bandwidth, wideband continuum setups can reach very deep RMS quickly compared with narrowband channels. Spectral-line science, by contrast, often requires fine velocity resolution to preserve kinematic information. Fine channels mean smaller per-channel bandwidth and therefore higher noise per channel.

When planning line observations, it is common to estimate sensitivity at a physically meaningful velocity width. For example, if your target line profile is broad, binning channels to 10 or 20 km/s may improve detectability while preserving science utility. If your goal is to resolve narrow components or turbulence signatures, you may need 0.2 to 1 km/s channels and significantly longer integrations.

This is exactly why the ALMA sensitivity calculator includes both continuum bandwidth and velocity-channel inputs. You can quickly compare your expected depth in integrated continuum maps versus line cubes and decide if your science priorities require more time, different frequency tuning, or altered channel strategy.

Key Inputs and Why They Matter

1) Frequency and ALMA Band

Frequency affects atmospheric transmission, receiver performance, and often source brightness temperature behavior. Higher ALMA bands generally face higher Tsys and stricter weather demands. Even if your science line lies in a high-frequency window, testing nearby setup options can reveal major sensitivity differences.

2) Number of Antennas

Interferometric sensitivity scales with baseline count. More antennas produce more independent visibility pairs and lower RMS. In simple terms, increasing antenna count improves raw sensitivity and often image quality through better uv coverage.

3) On-Source Time

Noise decreases as 1/sqrt(t). This means long integrations produce diminishing returns, but they still matter for ultra-faint targets. A fourfold time increase yields roughly a twofold RMS improvement.

4) Bandwidth or Channel Width

Continuum setups benefit from wide bandwidth; spectral-line setups trade bandwidth for resolution. If you halve channel width, RMS per channel increases by about sqrt(2). Matching channel strategy to expected line width is one of the most powerful planning decisions you can make.

5) System Temperature

Tsys captures receiver and atmospheric contributions. Better weather and favorable frequency windows reduce Tsys and improve sensitivity. Under poor conditions, your effective sensitivity can degrade enough to change project feasibility.

6) Efficiency Terms

Aperture efficiency and correlator efficiency include real-world losses in collection and processing. They may appear subtle, but even small changes can meaningfully affect final RMS.

How to Plan Better with an ALMA Sensitivity Calculator

Start with your science threshold rather than instrument settings. Ask: what line luminosity, continuum flux density, or brightness temperature contrast must be detected to answer the science question? Translate that into a target RMS, then back-solve approximate time requirements with the calculator.

Next, run a parameter sweep. Hold source and line assumptions constant while varying channel width, time, and antenna count. This reveals which parameter gives the largest practical gain. In many cases, moderate channel binning can be more efficient than requesting large additional observing time.

Include realistic overhead thinking from the beginning. Slewing, calibration, and execution block structure all reduce net on-source efficiency. The overhead factor input in this calculator helps you test conservative versus optimistic assumptions quickly.

Finally, compare your quick estimates with official observatory tools before final submission. Fast calculators are best for strategy and intuition; official systems are best for final execution realism.

Common Sensitivity Planning Mistakes

A strong workflow is to compute a baseline estimate, test optimistic and pessimistic scenarios, and build a margin that reflects calibration and weather uncertainty. This approach reduces proposal risk and improves the chance that delivered data meet core science goals.

Interpreting Your Results Responsibly

If this ALMA sensitivity calculator reports a very low continuum RMS, verify that your assumed bandwidth and time are realistic for your setup. If line RMS appears too high, inspect velocity resolution first, then test whether mild binning preserves your science while improving detectability. If sensitivity is still marginal, prioritize transitions or frequencies where atmospheric and receiver performance are more favorable.

Remember that sensitivity alone does not guarantee success. Angular resolution, source morphology, uv sampling, and dynamic range all influence science quality. A balanced observing design integrates sensitivity, resolution, and calibration strategy rather than optimizing only one dimension.

Frequently Asked Questions

Is this ALMA sensitivity calculator official?

No. It is a fast planning calculator for educational and strategy use. Official sensitivity and feasibility checks should always be done with observatory-supported tools and current cycle documentation.

Why do my values differ from other tools?

Differences usually come from weather assumptions, weighting, effective bandwidth conventions, overhead treatment, flagging assumptions, or detailed instrumental models not included in quick calculators.

What is a good continuum RMS target?

It depends on your science. For faint extragalactic continuum, tens of microjansky may be required. For bright nearby structures, higher RMS may still be sufficient. Define RMS from required signal-to-noise on the feature of interest.

How should I choose line channel width?

Use a width that samples the expected profile with enough bins for kinematic interpretation while preserving sensitivity. Over-resolving channels without scientific need can severely increase integration time.

Can I use this for ACA 7 m planning?

Yes. Select 7 m dish diameter and adjust antenna count accordingly. Keep in mind that array characteristics and imaging goals differ from the 12 m main array.

Final Takeaway

A high-quality ALMA sensitivity calculator is not just a number generator. It is a decision framework. By connecting physical requirements to instrumental parameters, it helps observers design feasible, efficient, and scientifically focused programs. Use this page to test scenarios quickly, understand tradeoffs deeply, and arrive at better-informed observing plans before formal submission.