Gaia FAQ - Gaia
Frequently Asked Questions
Here you find answers to some of the most frequently asked questions about the Gaia mission, its science and its data. Additional FAQs are available on the ESA Gaia corporate website.
For registered users who have questions on their Cosmos account and password resets, please visit the Cosmos FAQ.
If you can not find what you are looking for, please contact the Gaia Helpdesk.
General |
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How shall I acknowledge Gaia? When do I acknowledge Gaia? | ||
If you have used Gaia data in your research, please follow the credit and citation instructions as found here. When using Gaia DR1 data, we ask you to also cite certain Gaia Data Release 1 papers, as is indicated here as well. |
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Where will I be able to find all scientific papers that use Gaia data? | ||
Gaia Data Release 1 papers, Gaia Data Release 2 papers, publications in peer-reviewed journals or Gaia PhD Theses are all accessible through our publications page on the Gaia cosmos website. | ||
When did Gaia's routine science operations phase start? | ||
Routine scientific observations commenced on 25 July 2014 with one month of Ecliptic Pole Scanning Law switching to Nominal Scanning Law. More important moment in Gaia history can be found in the table given on this page. | ||
Which telescopes are being used to track Gaia from the ground? | ||
The following telescopes track Gaia from the ground: the Liverpool Robotic Telescope, the Faulkes Telescope North, the Faulkes Telescope South, and the ESO VLT survey telescope. Gaia is also regularly observed as part of the ground-based orbital tracking (GBOT) operations. Gaia is visible in the sky most of the night due to its orbit around the second Lagrange point (with some variability in the elevation over the seasons). However, Gaia is not too bright (less than 20th magnitude) so not that easy to spot for an amateur astronomer. The telescopes used by GBOT have an aperture of about 2 metres. | ||
What can amateur astronomers contribute to the mission? | ||
Amateurs can contribute, for instance, through the Gaia-Groundbased Observational Service for Asteroids (Gaia-GOSA) or by participating in the Gaia solar-system alerts (Gaia FUN-SSO). Another opportunity is through the follow-up of Gaia photometric science alerts. A description of follow-up opportunities is given in this image of the week. | ||
Science |
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What is Gaia's astrometric, photometric and spectroscopic performance? | ||
A summary of key astrometric, photometric and spectroscopic performance figures can be found here. An extended overview is available on the Science Performance pages. | ||
How many objects in our solar system will Gaia detect? | ||
Gaia will detect and observe all objects brighter than 20 mag that are not too extended, which means not too large in size and not too fast moving. This covers, among others, the largest moons in the Solar system, comets, Kuiper-Belt / trans-Neptunian objects, main-belt asteroids, near-Earth asteroids, and Trojan companions of planets. All in all, Gaia will observe some 350,000 objects in the Solar system, the vast majority of which are main-belt asteroids. | ||
What will be the most common type of star in the Gaia catalogue? | ||
Gaia provides an unbiased survey of the Milky Way, down to 20 mag. This covers all types of stars, including rare ones and stars with short-lived evolution phases. Whereas Gaia only observes a few hundred, hot, massive stars with spectral type O, it sees a few hundred million solar-type and less-massive G- and K-type stars. The vast majority of stars seen by Gaia are normal ('adult') main-sequence stars with only 10-20% of all stars being in their 'post-adult' giant phase. | ||
What is the Gaia scanning law and how does it work? | ||
The scanning law is the "law" describing how Gaia's fields of view scan the sky as function of time. The scanning is composed of two, independent, "superimposed" motions: (1) a rotation around the spacecraft spin axis with a period of 6 hours, and (2) a slow (~63-day-period) precession of the spin axis around the solar direction at a fixed solar-aspect angle of 45 degrees. Over the nominal 5-year mission, Gaia will complete 29 of these precession periods, leading to an optimally uniform sky coverage after 5 years. | ||
I'm not interested in stars, I'm interested in galaxies. What can Gaia do for me? | ||
Although Gaia is foremost a star-mapper mission aimed to observe the Milky Way, it also observes external galaxies brighter than 20 mag. For the nearest galaxies, like M31, individual stars are resolved and observed but a more typical case is an unresolved galaxy at a larger distance. Some one million of these, mostly elliptical galaxies, are observed by Gaia. In addition, Gaia observes around half a million quasars. All these objects undergo astrophysical classification and parametrisation, for instance morphology and star-formation history for galaxies and redshift for quasars. | ||
Is there an input catalogue for Gaia? If yes, how are transient objects like supernova discovered? | ||
Unlike the Hipparcos mission, which selected its targets for observation based on a pre-defined input catalogue loaded on board, Gaia will perform an unbiased survey of the sky. Since an all-sky input catalogue at the Gaia spatial resolution complete down to 20th magnitude does not exist, there has essentially been no choice but to implement on-board object detection, with the associated advantage that transient sources (supernovae, near-Earth asteroids, etc.) will not escape Gaia’s eyes. | ||
Is there any way to find out about transient objects immediately to do follow-up observations on-ground ? | ||
Gaia Photometric Science Alerts are published here. There is also a Gaia Follow-Up Network for Solar System Objects. | ||
What does the first Gaia catalogue look like? | ||
The data is contained in a database and can be extracted using various methods, for instance through a command-line interface based on the Table Access Protocol (TAP) or a web-based interface using simple query forms or using customised queries in Astronomical Data Query Language (ADQL). The Gaia Archive is accessible here. | ||
What is the Robust Scatter Estimate (RSE)? | ||
The “Robust Scatter Estimate” (RSE) is defined as 0.390152 times the difference between the 90th and 10th percentiles of the distribution of the variable. For a Gaussian distribution, it equals the standard deviation. Within the Gaia community, the RSE is used as a standardised, robust measure of dispersion (see, for instance, Lindegren et al. 2012). | ||
How can Gaia G, BP and/or RP values be transformed to V magnitudes? | ||
Pre-launch relations between Johnson, Gaia, and Sloan filters are published in: http://adsabs.harvard.edu/abs/2010A%26A...523A..48J (for instance Table 3). A post-launch discussion is available here. |
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What happens to newly detected solar system objects (Gaia asteroid observations)? | ||
Finding out whether an asteroid has a chance to hit our planet is an international effort: Gaia asteroid observations are sent to a central collection place called the Minor Planet Center (MPC). Position measurements from all observers on our planet are collected there and a first orbit estimate is done at MPC using a combination of all observations. A NASA-funded team at JPL in the US and a team in Pisa, working with ESA, then perform detailed computations to find possible impactors. Rules on informing affected countries are in place in some nations; at the UN-level this is the task of the recently formed IAWN. ESA is currently putting a warning mechanism in place addressing the needs of their member countries. | ||
Where can I check how many times and when Gaia will observe my favourite object? | ||
You can use the Gaia Observation Forecast Tool for this, which is available here. | ||
I'm not interested in stars, I'm interested in minor bodies in the Solar System. When will you start releasing information about them? Will you calculate orbital elements for them? | ||
Gaia will observe around 350,000 objects in the Solar system. Most of these are main-belt asteroids but the sample will include some near-Earth asteroids and comets. Keep an eye out for our data release scenario to see when data will be released. | ||
I can not find data for a bright star. Why is that? | ||
Some stars are too bright for Gaia to observe. Some of these bright stars are being observed with a special mode on board the spacecraft, requiring to predict when it passes the focal plane and then telling the on board computer to record the relevant pixels around the position of the star. These data should be processed eventually but cannot be handled automatically at this stage. | ||
The abstract of the Gaia DR1 release paper (Gaia Collaboration et al. 2016) states that "For the primary [TGAS] astrometric data set the typical uncertainty is about 0.3 mas for the ... parallaxes ... A systematic component of 0.3 mas should be added to the parallax uncertainties". This is confirmed at several places inside the paper. Is this really true? On the other hand, if a systematic error of 0.3 mas has been included already, how can many parallax standard errors in TGAS be close to 0.3 mas (or even be smaller)? | ||
Both the random and systematic errors have been included in the published "parallax_error" column in Gaia DR1 through the error "inflation" determined through a comparison with external data (see Equation 4 in Section 4.1 in Lindegren et al. 2016). So, what happened for TGAS stars with parallax standard errors below 0.3 mas? Did we forget to inflate their errors? No: some errors can be smaller than 0.3 mas because a different factor was applied for each star. The confusion is related to the 0.3 mas magic number, which might not have been explained sufficiently well. At some point, two particular AGIS test solutions using different sets of input observations (a different half of the focal plane) were created. The residuals showed significant structure, i.e., correlated errors. The typical difference was about +/-0.1 mas, but was much higher (or lower) in particular regions of the sky. The magic number 0.3 mas takes these regions into account but should not be interpreted as an RMS value for the whole sky. The problem is that we cannot quantify (and thus remove) these errors more precisely. Further details can be found in Lindegren et al. 2016, Appendices B and C. So, summarising:
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What is the meaning of ICRS, ICRF, J2000.0 epoch, and J2000.0 equinox? | ||
Gaia DR2 astrometry consistently uses the ICRS reference system and provides stellar coordinates valid for epoch J2015.5 (roughly mid-2015, where J stands for Julian year). Equinox J2000.0 is a currently obsolete concept linked to former, dynamical reference systems such as FK5 which were tied to the celestial equator at a particular time. As of 1 January 1998, the International Celestial Reference System (ICRS) is the standard celestial reference system adopted by the International Astronomical Union (IAU). The ICRS is the set of prescriptions and conventions together with the modelling required to define, at any given time, a triad of orthogonal axes. The ICRS has its origin is at the barycentre of the Solar System, with axes that are space-fixed and kinematically non-rotating with respect to the most distant sources in the Universe. In practice, the ICRS is materialised by the International Celestial Reference Frame (ICRF) through the coordinates of a defining set of extra-galactic objects (quasars). Prior to astronomers being able to define and use the ICRS and ICRF, dynamical reference systems were used based on observations of star positions tied in some way to moving objects in the Solar System. These reference systems refer to a mean equator and equinox at a given reference epoch (typically J2000.0), requiring precession/nutation models and corrections to deal with the time-variable fundamental plane. To within ~25 mas, mean J2000.0 equatorial coordinates are the same as ICRS coordinates such that, for "ordinary" applications, they can in practice be considered to be the same. For high-accuracy applications, the appropriate frame conversion shall be used. |
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Gaia Data |
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Where can I find information about upcoming data releases? | ||
Information about all upcoming data releases is provided in the "Gaia Data Release Scenario". | ||
Where can I find all relevant information on a specific Gaia data release? | ||
Overview pages were created for each release. These are the respective pages: Gaia data release 1 overview page, Gaia data release 2 overview page. | ||
Is data access limited? How is it regulated? | ||
Members of the scientific community will have access to Gaia data through intermediate catalogues, which will be released in the course of the mission (a release scenario is available). Formal 'data rights' (for example, through a Call for Proposals) will not be assigned to any scientist involved in any aspects of the mission, including those scientists who participate in the data processing. Early access to the reduced data could, however, be awarded to individuals and groups participating in the data analysis, its validation, and documentation, according to procedures to be established by the Gaia Science Team, in consultation with the AWG and the executive committee of the Data Processing and Analysis Consortium. The Gaia Data Rights are defined in the Gaia Science Management Plan ESA/SPC(2006)45 (SMP). |
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What types of data are being downlinked? | ||
The data downlinked from Gaia comprises astrometry, photometry, and spectroscopy. Most data, except for the 1% of the very brightest stars, comes down in small images which have been compressed (binned) into one number (the intensity/brightness of the light) in the so-called across-scan direction. This allows accurate timing and hence location estimation of the images (astrometry) as well as flux measurements (photometry). For the spectro-photometry and spectroscopy, the dispersion direction is orthogonal to the binning direction such that wavelength information is preserved. | ||
Are the data from the Gaia-ESO survey already public? If yes, where can I access them? | ||
Gaia ESO survey data is public and is being served from here. | ||
How is the Gaia data transferred to Earth? | ||
Gaia produces a lot of data that all needs to be transferred from the satellite in orbit around L2 to a ground station on Earth. Gaia uses the large ESA ground stations: Cebreros, Malargue and New Norcia. Downlinking data needs some preparation: the sky Gaia is looking at is modeled in advance to get an indication of how much data to expect and also the link budget is modeled (this is how fast data can be downlinked based on antenna performance). Both combined give an indication of how much time is needed each day for downloading the data without wasting ground station time. On average it takes about 14 hours a day to get the Gaia data down to a ground station. | ||
Data Processing |
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What is DPAC? | ||
The Data Processing and Analysis Consortium (DPAC) is a large pan-European team of expert scientists and software developers. It is responsible for processing the Gaia data with the final objective of producing the Gaia catalogue. DPAC has been in place since 2006 and has the task to develop the data processing algorithms, the corresponding software, and the IT infrastructure for Gaia. It also executes the algorithms during the mission in order to turn the raw telemetry from Gaia into the final scientific data products that will be released to the scientific community. More information about the consortium and its structure is available here. |
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How does the on-board processing system work? | ||
Gaia's focal-plane assembly contains 106 CCD detectors, comprising nearly a billion pixels, and operates in TDI mode with a line period of 1 milli-second. The enormous amount of data this detector system could continuously generate is a few orders of magnitude too large to be transmitted to ground. There are hence three on-board processes applied to the science data: 1: not all pixel data are read from the CCDs but only small areas, so-called windows, around objects of interest; 2: the two-dimensional images (windows) are, except for bright stars, binned in the direction orthogonal to the scanning direction; 3: the resulting along-scan intensity profiles are compressed on board without loss of information. The resulting, compressed star packets are transmitted to ground, typically within 24 hours after they are created, where they enter the data processing in the science ground segment. |
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How do you mitigate the effects of radiation damage? | ||
Mitigation takes places at two levels, in the spacecraft hardware and software and in the software for the data processing. The design of the spacecraft has several features to mitigate the impact of non-ionising radiation damage, including focal-plane shielding, a supplementary buried channel in the detectors, and a charge-injection mechanism for the detectors. In addition, the temperature and clocking characteristics of the detectors have been selected taking the impact of radiation damage into account. Also the on-board science software, in charge of placing the windows around the stars, takes the effect of radiation damage into account by allowing a non-centred, asymmetric placement. In the ground-processing software, radiation damage is calibrated using models inspired by and partially calibrated through extensive pre-launch laboratory test campaigns using flight-representative CCD detectors. | ||
What are the different steps in the Gaia data processing? | ||
The data processing is a complex task which is not easily summarised in a sentence or two. A concise description can be found in Section 7 of the Gaia mission paper. | ||
Spacecraft |
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What is the difference between Gaia's three different CCD variants? | ||
Gaia carries 106 charge-coupled-device (CCD) detectors. They come in three different types: the broad-band CCD, the blue(-enhanced) CCD, and the red(-enhanced) CCD. Each of these types has the same architecture (e.g. number of pixels, TDI gates, read-out register, etc.) but differ in their anti-reflection coating (and surface passivation), their thickness, and the resistivity of their Silicon waver. The broad-band and blue CCDs are both 16 micrometer thick and are both manufactured from standard-resistivity silicon; they differ only in their anti-reflection coating, which is optimised for short wavelengths for the blue CCD and optimised to cover a broad bandpass for the broad-band CCD. The red CCD, in contrast, is based on high-resistivity silicon, is 40 micrometer thick, and has an anti-reflection coating optimised for long wavelengths. The broad-band CCD is used in the star mapper (SM), the astrometric field (AF), and the wavefront sensor (WFS). The blue CCD is used in the blue photometer (BP). The red CCD is used in the basic-angle monitor (BAM), the red photometer (RP), and in the radial-velocity spectrograph (RVS). | ||
Why is there an angle of 106.5 degrees between Gaia's two telescopes? | ||
The choice of the so-called basic angle of Gaia was a non-trivial one. On the one hand, it should be of order 90 degrees to allow simultaneous measurements of stars separated by large angles on the sky. On the other hand, it should not be a harmonic ratio of a 360-degree circle (e.g., 60 deg, 90 deg, or 120 deg). Taking these considerations into account, acceptable ranges for the basic angle are 96.8 +/- 0.1 deg, 99.4 +/- 0.1 deg, 100.5 +/- 0.1 deg, 105.3 +/- 0.1 deg, 106.5 +/- 0.1 deg, 109.3 +/- 0.1 deg, 109.9 +/- 0.1 deg, etc. Accommodation aspects identified during industrial studies subsequently favoured 106.5 deg as the value finally adopted for Gaia. | ||
The spinning axis of Gaia seems to be fixed at 45 degrees with respect to the Sun. Is there any special reason why this value was chosen? | ||
The parallax factor, which means the measurable, along-scan parallactic displacement of a star, is proportional to the sine of the so-called solar-aspect angle (the angle between the spin axis and the direction to the Sun). Therefore, the highest signal to noise for parallax measurements would be reached for a solar-aspect angle of 90 degrees. This, however, would mean that the sunshield would not point to the Sun so that solar-cell-driven power generation would be inhibited and, more importantly, that sunlight would enter the telescope apertures. In the other extreme case, i.e., with a zero solar-aspect angle, power generation would be optimal but parallaxes could not be measured. In practice, given design considerations on the required size of the sunshield to keep the payload in permanent shadow and to generate sufficient power, the final compromise for Gaia ended up at 45 degrees. | ||
Why does Gaia have two telescopes? | ||
The goal of the Gaia mission is to perform global astrometry over the entire celestial sphere. For this purpose, the satellite is equipped with two telescopes whose viewing directions are separated by a large, so-called basic angle (106.5 deg). This allows to make simultaneous measurements of star positions at small and large angular scales, i.e., inside each telescope field of view and between the two fields of view. Since the parallax factor differs between the two fields of view, global astrometry can be performed (as compared to relative astrometry offered by a single field of view). Wide-angle measurements also guarantee a distortion-free and rigid system of coordinates and proper motions over the whole sky. | ||
What are the red and blue photometer used for? | ||
Photometric observations are collected with the photometric instrument, at the same angular resolution as the astrometric observations and for all objects observed astrometrically. The purpose of the photometry is to enable chromatic corrections of the astrometric observations and to provide astrophysical information for all objects, including astrophysical classification (for instance object type such as star, quasar, etc.) and astrophysical characterisation (for instance interstellar reddenings and effective temperatures for stars, photometric redshifts for quasars, etc.). | ||
How do you ensure the stability of the basic angle? | ||
The stability of the basic angle is achieved through the design of the spacecraft and mission (profile), including the choice of material for most payload structural parts (silicon-carbide), the absence of moving parts in the spacecraft (except for the thruster valves), the thermo-mechanical decoupling between the service and payload modules, a constant power dissipation of the payload, and the spacecraft orbit and attitude (ensuring a constant solar illumination without eclipses by the Earth). In addition, the basic-angle monitor provides continuous feedback on short-term basic-angle variations (P < 12 h), with long-term variations (P > 12 h) being calibrated within the data processing. | ||
What kind of mode do the CCDs operate in? | ||
The CCD detectors operate in Time-Delayed Integration (TDI) mode. That means that the photo-electrons generated by the starlight are transferred through the CCD with the same speed as the star images move, as a result of the slow spin / rotation of the spacecraft, over the detector surface. It takes an object 4.4 seconds to cross a CCD detector. | ||
When will Gaia stop observing? What happens with the satellite afterwards? | ||
The nominal, five-year mission ends in July 2019. The mission has been extended to the end of 2020, and has an indicative extension up to the end of 2022. The consumables of the spacecraft have been sized to allow for an extension of at least one year. Extrapolating the current cold-gas propellant consumption suggests that the mission could be extended, provided this is approved by the ESA advisory bodies, up to 2023 (with an uncertainty of plus or minus one year). After science operations are terminated, the spacecraft will be put into a disposal orbit (away from L2) to comply with space-debris regulations. | ||
How does the Gaia scanning law work? | ||
Gaia scans the sky in a complex way. First, the telescopes rotate around the spin axis every six hours to sweep great circles on the sky (with a height of about 0.7 deg). At the same time, the spin axis precesses slowly around the solar direction (at a fixed, 45-degree angle), as the Sun moves over the ecliptic, with a period of 63 days. This optimises the uniformity of the sky scanning over five years and leads to, on average, 70 astrometric and photometric transits across the focal plane (and 40 for the RVS instrument). |