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The Exozodiacal Dust Problem for Direct Observations of Exo-Earths

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Published 2012 August 17 © 2012. The Astronomical Society of the Pacific. All rights reserved. Printed in U.S.A.
, , Citation Aki Roberge et al 2012 PASP 124 799 DOI 10.1086/667218

1538-3873/124/918/799

ABSTRACT

Debris dust in the habitable zones of stars—otherwise known as exozodiacal dust—comes from extrasolar asteroids and comets and is thus an expected part of a planetary system. Background flux from the solar system's zodiacal dust and the exozodiacal dust in the target system is likely to be the largest source of astrophysical noise in direct observations of terrestrial planets in the habitable zones of nearby stars. Furthermore, dust structures like clumps, thought to be produced by dynamical interactions with exoplanets, are a possible source of confusion. In this article, we qualitatively assess the primary impact of exozodiacal dust on high-contrast direct imaging at optical wavelengths, such as would be performed with a coronagraph. Then we present the sensitivity of previous, current, and near-term facilities to thermal emission from debris dust at all distances from nearby solar-type stars, as well as our current knowledge of dust levels from recent surveys. Finally, we address the other method of detecting debris dust, through high-contrast imaging in scattered light. This method is currently far less sensitive than thermal emission observations, but provides high spatial resolution for studying dust structures. This article represents the first report of NASA's Exoplanet Exploration Program Analysis Group (ExoPAG).

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1. INTRODUCTION

Interplanetary dust interior to the solar system's asteroid belt is called the zodiacal dust, which comes from comet comae and asteroid collisions, just like the dust in any debris disk. At least 16% of nearby solar-type stars harbor cold, outer debris dust much denser than the dust in the solar system's Kuiper Belt (Trilling et al. 2008). Sensitive new far-IR surveys probing similar stars for cold dust down to about 10 times the solar system Kuiper Belt level find a detection rate of ∼25% (Eiroa et al. 2012, in preparation). Unfortunately, we know little about warmer exozodiacal dust (exozodi) in the inner reaches of nearby systems, i.e., within the stars' habitable zones. About 1% of nearby solar-type stars show a large amount of emission from warm dust ( ≳1000 times the expected zodiacal dust emission in the wavelength range from 8.5 μm to 12 μm; Lawler et al. 2009). However, a more sensitive survey for exozodiacal dust around a smaller set of nearby stars with the Keck Nulling Interferometer (KIN) found mostly nondetections (discussed further below; Millan-Gabet et al. 2011). As will be shown, background flux from our local zodiacal dust and the exozodi will likely dominate the signal of an Earth-analog exoplanet (an exo-Earth, for short) in direct images and spectra, even if exozodi levels are no greater than the solar system level.

Furthermore, debris disks often display dust structures, such as narrow rings (e.g., HR 4796A; Schneider et al. 2009), clumps (e.g., epsilon Eri; Greaves et al. 2005), and warps/inclined subdisks (e.g., AU Mic; Krist et al. 2005). A notable example of a warped disk—the famous β Pictoris system—is shown in Figure 1. Such structures are thought to be produced by the dynamical influence of a planet, as are the clumps of zodiacal dust leading and trailing the Earth in its orbit (Dermott et al. 1994). Dust clumps are likely to be the most troublesome source of confusion in direct imaging of Earth-size planets, since dynamical clumps orbit the star, though not necessarily with the same period as the perturbing planet (e.g., Kuchner & Holman 2003).

Fig. 1.—

Fig. 1.— Composite image of β Pictoris system showing the edge-on debris disk and the exoplanet β Pic b (Lagrange et al. 2010). The disk image was obtained with the ESO 3.6 m telescope; the innermost portion of the disk is obscured. The planet, imaged at two epochs with ESO's VLT, is likely responsible for a warp seen in the inner disk (Heap et al. 2000), revealed as an inclined subdisk in HST ACS coronagraphic images (Golimowski et al. 2006). Image credit: ESO and A.-M. Lagrange.

Therefore, exozodiacal dust complicates direct imaging of exoplanets in two ways: (1) as a source of noise and (2) as a source of confusion. The exozodiacal dust levels around nearby stars will be as important to the success of efforts to find and characterize Earth-like exoplanets as the fraction of stars with potentially habitable planets ( η). There is a strong need to sensitively probe nearby stars for small amounts of dust in their habitable zones. In this article, we will first demonstrate the effect of exozodi emission as a source of increased noise in direct imaging of exoplanets, then assess the current knowledge of debris dust abundances and expected progress toward increasing our knowledge.

1.1. Quantifying Debris Dust: What is a "Zodi"?

Debris disk observers typically express the amount of dust in a debris disk using the system's fractional dust luminosity, Ldust/L, which is the light absorbed by the dust and reemitted at thermal wavelengths (infrared to millimeter) relative to the stellar luminosity. This parameter, often also called the fractional infrared luminosity, is determined by integrating the total long-wavelength excess flux seen in a disk spectral energy distribution (SED) over frequency. Therefore, it can be measured from unresolved photometry, more easily at long wavelengths, where the stellar emission is relatively faint. Ldust/L is not a unit of optical depth, dust mass, or surface brightness. In the optically thin case, it is proportional to the dust mass but is affected by grain properties like size and composition.

In the context of direct exo-Earth observations, the abundance of debris dust in habitable zones is typically given in units of "zodis," which arose as a convenient way of quickly expressing some sort of ratio to the solar system zodiacal dust. However, extreme caution must be taken when interpreting the unit, since different workers have used different dust properties when constructing their one zodi. The definition adopted largely depended on what was useful or possible for the analysis at hand. For example, Gaidos (1999) defined one zodi (spelled "zody") as the effective emitting area of the solar system's zodiacal dust. Roberge & Kamp (2010) took one zodi to be the fractional dust luminosity of the zodiacal dust ( Ldust/L ∼ 10-7; Nesvorný et al. 2010), in order to relate the dust abundances of known debris disks to the solar system (by this standard, β Pictoris has about 10,000 zodis of cold dust).

Others assume that one zodi is a debris disk identical to the solar system's zodiacal dust in every respect, including total mass, spatial distribution, grain size distribution, albedo, scattering phase function, etc. (e.g., Millan-Gabet et al. 2011). Here, we will refer to such a disk as a zodiacal-twin disk; around a Sun-twin star, we call it a solar system-twin disk and it has Ldust/L ∼ 10-7. However, care must be taken when applying a zodiacal-twin disk to a star different from the Sun, since such a disk around another type of star may not be both self-consistent and truly identical to the zodiacal dust in every way. ZODIPIC8 is a publicly available code that is frequently used to calculate zodiacal-twin disks for any type of star, using the zodiacal dust model in Kelsall et al. (1998), which was itself based on fits to observations of the zodiacal dust emission with the COBE DIRBE instrument. The code does not change the dust density distribution when varying the central star, as expected for a zodiacal-twin disk. However, the inner disk radius set by the dust sublimation temperature does move outward with increasing stellar luminosity, to prevent an unphysical situation with dust at impossibly high temperatures. The unfortunate consequence of this is that the total dust mass and Ldust/L value of a ZODIPIC zodiacal-twin disk decreases as the stellar luminosity increases.

Nonetheless, for direct observations of exoplanets at any wavelength, it is the surface brightness of the dust thermal or scattered emission near the location of the exoplanet that matters. While Ldust/L can be measured for debris disks, it is not straightforward to convert Ldust/L into a surface brightness; one must assume the spatial distribution of the dust, as well as many other properties that are also typically unknown (e.g., albedo). But declaring one zodi to be a zodiacal-twin disk is also perilous. For most debris disks, we do not know if the inner dust matches the zodiacal dust, and in some cases we know it cannot (e.g., HD 69830; Beichman et al. 2005). Furthermore, this definition is typically applied to stars that are not identical to the Sun without any adjustment to the radial dust distribution, which is not likely to provide an accurate comparison with the solar system (discussed further below). Because of these problems, we eschew use of the unit "zodi" in this article, although we acknowledge its convenience and anticipate its continued usage.

1.2. Exozodi Surface Brightness

In the next section of this article, we show the impact of exozodi emission on direct observations of exo-Earths at optical wavelengths. To do this, we need a reference value for the scattered-light surface brightness. For a solar system-twin disk viewed at 60° inclination (the most likely value in a random distribution of inclinations), the modeled surface brightness at a projected separation of 1 AU in the plane of the disk (the quadrature position for a planet) and λ = 0.55 μm is about 22 mag arcsec-2. Other brightness values calculated with ZODIPIC appear in Table 1.B-1 of the TPF-C STDT Final Report.9 The inclination of the system strongly affects the observed surface brightness; at 1 AU, the surface brightness of a ZODIPIC zodiacal-twin disk viewed edge-on is nearly 3 times greater than when viewed face-on.

To apply the above surface brightness value to another star, we take advantage of the fact that, by definition, the habitable zone is the region around a star where an Earth-like planet receives the right amount of energy for it to have liquid water on its surface. Therefore, the habitable zone moves with changing stellar luminosity to keep the incident flux constant, such that

where EEID stands for "Earth equivalent insolation distance." No matter the star, bodies in the habitable zone always receive about the same total amount of flux; if their physical properties are the same, they also reflect or emit about the same total flux.

One consequence of this is that the absolute bolometric magnitude of an Earth-twin in the habitable zone does not change from star to star, assuming the same viewing geometry. Another is that, assuming identical grain properties and inclination, the same amount of dust in the habitable zones of different stars has roughly the same surface brightness. Therefore, we can reasonably adopt the surface brightness at 1 AU of a solar system-twin disk viewed at 60° inclination as a reference value for the exozodi brightness at the EEID for all stars.

The movement of the habitable zone with stellar luminosity explains the aforementioned problem with applying an unmodified zodiacal-twin disk to stars that are not Sun-like. For an earlier-type/later-type star, the EEID will be at a larger/smaller radius than 1 AU, probing a more/less distant region of the zodiacal-twin disk where the surface density may not be the same; in fact, the Kelsall et al. (1998) model says it should be lower/higher. If one was expecting the same amount of dust in the star's habitable zone as in the solar system's, the zodiacal-twin disk would need to be stretched/shrunk in radius by the square root of the stellar luminosity.

2. IMPACT OF EXOZODIACAL EMISSION ON EXOPLANET DIRECT IMAGING

The importance of zodiacal and exozodiacal background emission is shown by comparing the counts from both sources with the counts from an exo-Earth. Note that the following discussion applies to ordinary high-contrast imaging, such as would be performed with a coronagraph. The impact of exozodi on mid-IR nulling interferometers intended for direct exo-Earth observations (e.g., ESA's Darwin mission concept) is extensively discussed in Defrère et al. (2010). Following the approach in Brown (2005) and assuming a uniform exozodi distribution near the planet location, the counts ratio is

where npix is the number of pixels in a critically sampled, diffraction-limited point-spread function (PSF) from a partially obscured circular aperture ( npix = 1/sharpness ≈ 1/0.07 ≈ 14.3); is the angular area of a pixel at wavelength λ for a telescope of diameter D; z is the surface brightness of the local zodiacal dust, which depends on the direction to the target star (a generic value is ≈23 mag arcsec-2 at λ = 0.55 μm); epsilon is the exozodi surface brightness at the EEID relative to the brightness of a solar system-twin disk; x is the surface brightness at the EEID (1 AU) of a solar system-twin disk viewed at 60° inclination ( ≈22 mag arcsec-2 for λ = 0.55 μm); Mp is the absolute magnitude of the planet ( MV = 29.7 mag for an Earth-twin orbiting at the EEID, viewed at quadrature); and d is the distance to the system in pc.

The left-hand panel of Figure 2 shows the counts ratio versus exozodi brightness (epsilon), assuming λ = 0.55 μm, d = 10 pc, the parameter values given above, and three different telescope diameters. For a 4 m telescope, the counts from the local zodiacal dust plus a solar system-twin disk of exozodi viewed at 60° inclination are about 5 times greater than the counts from the Earth at 10 pc. While this may sound disastrous, astronomers commonly observe targets that are fainter than the surrounding background, at the price of increased noise and longer exposure times. Assuming background-limited imaging and including unsuppressed light from the central star, the time to detect an exoplanet at some signal-to-noise ratio (S/N) in an image is

where F0 is the specific flux for zero magnitude in the image bandpass ( ≈9500 counts s-1 cm-2 nm-1 in V band); Δλ is the image bandpass width; T is the total facility throughput; ; ζ is the contrast level at the position of the exoplanet with respect to the theoretical Airy peak of the stellar image ( < 10-10 for instruments designed for direct imaging of exo-Earths); and m is the stellar apparent magnitude (for more details on the derivation of this equation, see Brown [2005]).

Fig. 2.—

Fig. 2.— Impact of exozodiacal dust emission on direct observations of exo-Earths. For both plots, we assumed that the exozodi has a uniform surface brightness. Both x-axes give the exozodi surface brightness at the EEID relative to the brightness of a solar system-twin disk (epsilon in eqs. [2] and [3]). Left: Dust counts and imaging exposure time vs. exozodi brightness. The left y-axis is the background counts from zodiacal plus exozodiacal dust divided by the counts from an Earth-twin around a Sun-twin at 10 pc, both calculated for V band (solid lines). The right y-axis is the exposure time (in arbitrary units) required to detect the Earth-twin with some S/N, assuming background-limited imaging (dashed lines). The counts ratios and exposure times were calculated for three different telescope aperture diameters: 2 m (black lines), 4 m (red lines), and 8 m (orange lines). Smaller apertures are more sensitive to background emission. Right: The combined effect of exozodi emission and η on the yield of a direct imaging/spectroscopy exoplanet mission. The y-axis is the fraction of stars with an Earth-size planet in the habitable zone. The curves were created using a simple mission planning code that chooses real stars within 30 pc for observation until 5 mission years is reached, assuming a 4 m telescope, some value of η, and that all the stars have the same exozodi level. At each value of η, the "tolerable exozodi" ( x-axis) is the largest exozodi level for which the desired mission yield (expected number of exo-Earths characterized) is achieved. The analysis was performed for three values of mission yield: high (dotted line), medium (dashed line), and low (solid line). The smaller η is, the lower the exozodi level that can be tolerated while still characterizing the desired number of exo-Earths. A full description of the code appears in Turnbull et al. (2012); however, the general behavior shown here should be similar for all direct-observation exo-Earth missions.

The terms within the square brackets of equation (3) account for the background sources: the first for local zodiacal dust, the second for exozodi, and the third for unsuppressed starlight. The third term is much smaller than the sum of the other two for all known mission concepts designed for direct exo-Earth observations at optical/near-IR wavelengths. This equation does not include any dark current or read noise, which are negligible compared with the other noise terms. The important points to take away are that in this idealized situation, (1) the exposure time decreases as D4—one factor of D2 for the collecting area and another for the smaller PSF leading to less background blended with the planet—and (2) the time increases linearly with increasing exozodi surface brightness. This is shown in the left-hand panel of Figure 2, where the imaging time is also plotted for the three telescope diameters.

The goal of a mission to obtain direct exo-Earths observations is to maximize the number of planets imaged and then characterized with spectra, while maintaining a reasonable mission architecture and lifetime. The right-hand panel of Figure 2 shows how η and the exozodi level combine to impact the performance of such a mission (ignoring confusion). The plot was created using a simple mission planning code that chooses real stars within 30 pc of the Sun for observation until the mission lifetime is reached (the mission parameters and planning code are detailed in Turnbull et al. [2012]). It shows that the smaller η is, the lower the exozodiacal dust level that can be tolerated while still obtaining direct observations of a sufficient number of exoplanets over the mission lifetime.

The analysis in this section demonstrates the primary effect of exozodi on direct exo-Earth observations: i.e., increased background noise and longer exposure times. However, equation (3) applies exactly only in the ideal case of uniform background emission and no systematic errors (i.e., no speckles). Furthermore, the methods used to extract the exoplanet signal from the background will affect the achievable S/N. If the background contains no unresolved structures, then matched filtering should be an efficient way of identifying point sources like exoplanets (see Kasdin & Braems 2006). However, since unresolved dust clumps and other background sources (e.g., stars and galaxies) should often be present, this technique will not resolve all confusion issues. Another option is to produce a model for the exozodi emission, fitting to portions of the exoplanet image, then subtract the model from the image. This should remove smoothly varying exozodi emission fairly easily. To account for unresolved dust clumps, more complex dynamical modeling of the whole system (dust and exoplanets together) may be required. There are also observing strategies to mitigate sources of confusion (e.g., multiepoch imaging, multicolor imaging, or even direct spectroscopy). But as of this writing, the problem of confusion for direct exoplanet imaging has not been thoroughly studied.

3. THERMAL EMISSION FROM DUST

Now that we have established the importance of exozodi, we assess our knowledge of the debris dust levels around nearby solar-type stars. Assuming that the stellar spectrum is well described by a Rayleigh-Jeans law (as it typically is at mid-IR and longer wavelengths) and the dust thermal emission is single-temperature blackbody radiation, the fractional dust luminosity may be expressed as

where Fdust and F are the dust and stellar fluxes at some frequency ν, Td is the dust temperature, and T is the stellar effective temperature (e.g., Bryden et al. 2006). For blackbody grains, assuming that all the dust is at the same temperature is equivalent to assuming that all the grains are at the same distance from the star (i.e., a ringlike disk). In reality, grains of different sizes will have different temperatures at the same distance. That being said, most debris disk SEDs are fairly well described by either a cold ( ∼ tens of kelvins) single-temperature blackbody—an outer dust ring—or the sum of a cold blackbody and a warmer one—outer and inner dust rings, an architecture reminiscent of the solar system's Kuiper Belt and asteroid belt (e.g., Chen et al. 2006, 2009).

Using equation (4), we may estimate the sensitivity of recent, current, and near-term telescope facilities to exozodiacal dust at different temperatures. Figure 3 shows the estimated 3σ sensitivity curves for the Spitzer Space Telescope (Spitzer), the Wide-field Infrared Survey Explorer (WISE), the Keck Interferometer Nuller (KIN), the Herschel Space Observatory (Herschel), the Large Binocular Telescope Interferometer (LBTI), the James Webb Space Telescope (JWST), and the Atacama Large Millimeter Array (ALMA). The relevant facility performance parameters—the instruments, years of operation (actual or expected), observation wavelengths, and uncertainties—appear in Table 1.

Fig. 3.—

Fig. 3.— Sensitivity limits for detection of debris dust around nearby Sun-like stars, for various recent (Spitzer, WISE), current (KIN, Herschel) and near-term facilities (LBTI, JWST, ALMA). The curves show 3σ detection limits in terms of the fractional dust luminosity ( Ldust/L) vs. its temperature. Recent and current facilities are plotted with solid lines and near-term ones are plotted with dashed lines. The instrument data assumed for these curves appear in Table 1. The temperature ranges for dust in two zones around the Sun are shown with vertical bars, calculated assuming blackbody grains. The habitable zone (0.8–1.8 AU) is shown in pink; the Kuiper Belt (30–55 AU) is shown in light blue. The modeled Ldust/L values for the solar system's Kuiper Belt dust ( ∼10-7; Vitense et al. 2012) and the zodiacal dust ( ∼10-7; Nesvorný et al. 2010) are marked with horizontal light blue and pink bars.

To calculate the sensitivity curves, we assumed a stellar effective temperature equal to the Sun's. For each instrument, the 1σ photometric uncertainty at the observation wavelength (col. [6] of Table 1) was converted into an uncertainty on the flux relative to the stellar flux at that wavelength ( σFdust/F in col. [7]). We then replaced Fdust/F in equation (4) with 3 times the relative flux uncertainties and plotted Ldust/L as a function of Td. Each curve has a minimum at the temperature for which the dust blackbody emission curve peaks at the frequency of observation ( Tpeak in col. [4]). Emission from dust warmer/cooler than Tpeak can be detected with reduced sensitivity. However, in most systems, emission from dust at temperatures near Tpeak will swamp any emission from much warmer/cooler dust, which is why a survey for habitable-zone dust is best done with an instrument that operates near 10 μm. Note that although JWST/MIRI will have only moderate absolute photometric accuracy, the telescope's large collecting area will allow MIRI to achieve this accuracy for fainter stars than other facilities covering its bandpass.

The temperature ranges for dust in the habitable zone and in the Kuiper Belt of a Sun-like star are overlaid in Figure 3. The temperature range for the habitable zone is 208–312 K, calculated assuming that the zone extends from 0.8 AU to 1.8 AU (Kasting et al. 2009). For the Kuiper Belt, we assumed an annulus extending from 30 AU to 55 AU, giving a temperature range of 38–51 K. In both cases, the dust temperatures were calculated assuming blackbody dust grains in radiative equilibrium with a Sun-like star. The modeled Ldust/L values for the zodiacal dust ( ∼10-7; Nesvorný et al. 2010) and dust in solar system's Kuiper Belt ( ∼10-7; Vitense et al. 2012) are marked with horizontal bars. The latter value is highly dependent on poorly known characteristics of the source bodies (Kuiper Belt objects); it was revised downward by about a factor of 10 in the last two years, based on new knowledge from in situ detections of dust grains with the Student Dust Counter on board NASA's New Horizons mission (Poppe et al. 2010; Han et al. 2011).

For nulling instruments (KIN and LBTI), to convert the null leakage to a relative flux ( Fdust/F), one must account for the fact that some dust emission may be removed by the dark fringes, depending on the exact spatial distribution of the dust. A recent KIN exozodiacal dust survey found an average value of 0.4 for the fraction of dust emission transmitted through the fringes, assuming unmodified zodiacal-twin disks (Millan-Gabet et al. 2011). The null leakage error must be divided by this transmission factor to give the correct uncertainty on the relative flux. However, the correct factor assuming a ringlike dust distribution, as we have done here, is not presently known and could be as large as 1. Therefore, we have chosen to ignore the transmission factor in calculating the sensitivity curves for nulling instruments.

Over the last several years, high-precision visibility measurements with near-IR interferometers (VLTI/VINCI, CHARA/FLUOR) have been used to detect circumstellar dust around a few nearby stars (e.g., di Folco et al. 2007). These observations can detect large amounts of hot dust (CHARA/FLUOR 3σ sensitivity ∼5000 times a solar system-twin disk for ∼1700 K dust; O. Absil 2012, private communication). While these observations are most sensitive to dust interior to habitable zones, they raise interesting questions about the origin of large amounts of dust so close to the central stars; one possibility is star-grazing comets (Absil et al. 2006). Another new instrument with sensitivity to hot dust is the Palomar Fiber Nuller (PFN; Hanot et al. 2011). Recent PFN observations at 2.2 μm of a debris disk system with a hot-dust detection from CHARA (Vega) limit the dust to ≲0.2 AU from the central star (or ≳2 AU if there is a significant scattered-light contribution [Mennesson et al. 2011]). Unfortunately, we cannot accurately estimate the sensitivity of these near-IR instruments with equation (4), since the assumption that the stellar spectrum is well described by a Rayleigh-Jeans law breaks down; therefore, we have not included CHARA/FLUOR or PFN sensitivity curves in Figure 3.

Examination of Figure 3 shows that previous and current facilities (Spitzer, WISE, KIN, Herschel) are relatively insensitive to dust in the habitable zone of Sun-like stars. To date, the most sensitive survey for habitable-zone dust around nearby solar-type stars was performed with the KIN (Millan-Gabet et al. 2011). While the mean 3σ detection limit for an individual star in this survey was 480 times a zodiacal-twin disk (shown in Fig. 3), the ensemble of nondetections was used to infer a 3σ upper limit on the mean exozodi level of 150 times a zodiacal-twin disk. Unfortunately, these limiting values are far too high to reliably estimate the performance of a future mission aimed at direct observations of Earth-analog planets. The sole near-term facility sensitive enough to assess the habitable-zone dust around solar-type stars is LBTI, which should have a 3σ detection limit of about 10 times a solar system-twin disk for ∼300 K dust. An LBTI survey for exozodiacal dust around a set of about 60–100 nearby stars is expected to begin in late 2012.10

Turning to dust structures, observations of dust thermal emission are typically unresolved; at best, SED modeling provides information only on the radial distribution of the dust. Dust clumps caused by an Earth-mass planet orbiting 1 AU from a Sun-like star may be expected to have sizes of about 0.2 AU, corresponding to 0.02'' for a star at 10 pc (Dermott et al. 1994). For each facility considered above, the spatial resolution at the reference wavelength is given in Table 1. Of the current and near-term facilities, only ALMA will have spatial resolution high enough to resolve dust clumps as small as those produced by an Earth-mass planet; unfortunately, ALMA is not sensitive to warm dust in habitable zones. However, note that more massive planets can create larger clumps (Stark & Kuchner 2008).

Looking beyond the time frame covered above, the next generation of ground-based Extremely Large Telescopes (ELTs) should begin operation in the early 2020s. For these telescopes with apertures larger than 25 m, detecting and spatially resolving thermal emission from habitable-zone dust around nearby stars should be a tractable problem. Assuming a solar system-twin disk, the exozodi flux at 10 μm relative to the stellar flux is Fdust/F ≈ 5 × 10-5, or about 85 μJy for a system at 10 pc; this is well within the photometric detection limits of planned ELTs (A. Weinberger 2012, private communication). The spatial resolution of a 25 m aperture at that wavelength ( λ/D ≈ 83 mas) could allow us to resolve thermal emission from regions at radii ≳0.8 AU for a system at 10 pc, as long as light from the central star is sufficiently suppressed and removed at such a small angular separation.

So instead of an unresolved measurement of the combined light from the star and dust (all the instruments discussed above do this, except the infrared interferometers and ALMA in the extended array mode), an ELT with advanced high-contrast imaging instrumentation could directly image the thermal emission from habitable-zone dust around nearby stars. In the next few years, new coronagraphs operating at near-IR wavelengths on ground-based telescopes should reach 10-6 contrast at small angular separations, using extreme adaptive optics and reference PSF subtraction (fuller discussion of coronagraphic imaging appears in the next section). This contrast will also be possible at 10 μm in the next decade; in fact, it will probably be easier to achieve, thanks to the higher Strehl ratio possible at the longer wavelength. A simulation of coronagraphic imaging of habitable-zone dust around a nearby solar-type star with an ELT appears in Figure 4.11 It seems likely that by sometime in the 2020s, ELTs will measure low levels of dust in the habitable zones of stars within ∼10 pc.

Fig. 4.—

Fig. 4.— Simulated high-contrast imaging of exozodi thermal emission with a ground-based ELT. Left: A model for a face-on debris disk around τ Ceti, a Sun-like star at 3.7 pc (Stark & Kuchner 2008). The disk has a dust abundance equal to that of a zodiacal-twin disk and an embedded planet orbiting at 1 AU (planet located at 12 o'clock). Image credit: C. Stark. Middle: A simulated 10 μm imaging observation of the model using an idealized coronagraph designed to produce high Strehl ratios ( ∼98% at 10 μm) on the Giant Magellan Telescope (25 m aperture); theoretically, the instrument suppresses the light from the central star by a factor of ∼103. Telescope and sky background emission were included in the simulation. Right: The simulated image after subtraction of a reference PSF image, achieving a contrast of ∼10-6 at an angular separation of 1λ/D (83 mas). Slightly different seeing was assumed for the target and PSF observations.

4. HIGH-CONTRAST IMAGING IN SCATTERED LIGHT

Debris disks may also be detected through coronagraphic imaging of scattered light; such observations have high spatial resolution and are best for revealing dust structures (see Fig. 5). However, current coronagraphy is far less sensitive at all distances from the central stars than thermal emission photometry, and it cannot image the habitable zones at all. This is due to the difficulty of suppressing diffracted and scattered light from the bright central star (using a coronagraph) and then removing residual starlight through subtraction of a reference PSF. The accuracy with which this can be done largely depends on the stability of the telescope PSF, whether one is using a space-based or ground-based facility.

Fig. 5.—

Fig. 5.— High-contrast imaging of the HR 4796A debris disk in scattered light. For this disk, Ldust/L = 4.7 × 10-3 (Moór et al. 2006). Left: Optical wavelength HST/STIS coronagraphic image. Image credit: Schneider et al. (2009). Right: Near-IR wavelength Subaru/HiCIAO image. Image credit: Thalmann et al. (2011).

PSF subtraction can be improved using differential imaging techniques, which distinguish between PSF artifacts and real sources. Some examples are angular differential imaging (ADI), which images the target at many rotation angles (e.g., Marois et al. 2006); chromatic differential imaging (CDI), which uses the known wavelength dependence of PSF artifacts to identify and remove them (e.g., Crepp et al. 2011); and polarimetric differential imaging (PDI), which compares images of the target in different polarizations to remove unpolarized starlight (e.g., Quanz et al. 2011). Note that ADI and CDI are best at searching for faint point sources and work less well on extended structures like debris disks. There are also postobservation techniques that can help with PSF subtraction, like locally optimized combination of images (LOCI; Lafrenière et al. 2007).

To date, the most sensitive scattered-light images of debris disks were obtained with the Hubble Space Telescope (HST), due to its excellent PSF stability compared with ground-based telescopes, even those with adaptive optics (AO) systems. Several HST instruments have had high-contrast imaging capability; they are listed in Table 2. This table also lists the Ldust/L value for the faintest disk successfully imaged in scattered light with each HST instrument. Examination of these values quickly demonstrates the much greater sensitivity of thermal emission observations (compare with Fig. 3).

A new generation of coronagraphs behind extreme AO systems on 8 m class ground-based telescopes is in the development and commissioning phase. These include the High Contrast Instrument for the Subaru Next Generation Adaptive Optics (HiCIAO) instrument on the Subaru Telescope, the Spectro-Polarimetric High-contrast Exoplanet REsearch (SPHERE) instrument on the VLT, and the Gemini Planet Imager (GPI) on the Gemini South Telescope. HiCIAO has begun science operations (e.g., Thalmann et al. 2011), while we expect the other two instruments to be commissioned in the next year. Further in the future, all three imaging instruments planned for JWST (NIRCam, NIRISS, and MIRI) include high-contrast capabilities; NIRCam and NIRISS (formerly known as TFI) will operate in the visible/near-IR and be sensitive to scattered light. More information about all these instruments and others may be found in Beichman et al. (2010).

Due to the inherent difficulties in assessing instrument performance before commissioning and also to the variety of observing and postobservation processing techniques available, it is difficult to predict the ultimate performance of these new instruments for high-contrast imaging of extended structures like debris disks. A preliminary measurement of the point-source contrast achievable using HiCIAO with ADI is available (see Table 2); so far, the faintest disk successfully imaged is HR 4796A, one of the very brightest debris disks (shown in the right-hand panel of Fig. 5). Table 2 also includes predictions for the contrast that will be achievable with GPI and JWST/NIRCam; however, these assumed that ADI would be used and may not accurately predict the instrument contrast for extended sources. A recent prediction of the GPI performance for debris disks suggests that compact (1'' diameter) disks with Ldust/L ≳ 2 × 10-5 can be imaged, using PDI and assuming moderately polarizing grains (B. Macintosh 2012, private communication). Unlike the other instruments, JWST/NIRISS uses sparse-aperture interferometric imaging to perform high-contrast imaging; a prediction for its point-source contrast appears in Table 2, but the expected extended-source performance is not yet available.

5. SUMMARY

  • 1.  
    Exozodiacal dust affects future efforts to directly observe Earth-like planets in the habitable zones of nearby stars in two ways: (1) background flux leading to increased noise and (2) dust structures causing confusion with unresolved exoplanets. The impact of second problem has not been thoroughly studied.
  • 2.  
    Assuming uniform exozodi surface brightness, a 4 m telescope aperture, and optical observing wavelengths, the counts from the local zodiacal dust plus a solar system-twin disk of exozodi are about 5 times greater than the counts from the Earth observed at quadrature orbiting 1 AU from a Sun-like star at 10 pc.
  • 3.  
    LBTI is the only previous, current, or near-term facility sensitive enough to detect exozodiacal dust in the habitable zones of nearby solar-type stars at levels approaching the solar system zodiacal dust level. This facility should begin surveying nearby stars for warm dust in 2012. A decade or so in the future, ground-based ELTs may be able to image low levels of habitable-zone dust around stars within ∼10 pc.
  • 4.  
    Dust structures like clumps located far from the central stars may currently be detected with high-contrast imaging of light scattered from dust disks. These observations are currently far less sensitive than observations of unresolved thermal emission. Cold clumps at large distances may soon also be imaged with ALMA. Unfortunately, dust structures in habitable zones are likely to prove elusive, although there is a chance that a new generation of ground-based coronagraphs may provide some information for the nearest stars.

This work was performed by members of the Debris Disks & Exozodiacal Dust Study Analysis Group (SAG #1), part of NASA's Exoplanet Exploration Program Analysis Group (ExoPAG). Current SAG #1 members are O. Absil, J.-C. Augereau, G. Bryden, J. H. Catanzarite, C. H. Chen, T. P. Greene, P. M. Hinz, M. J. Kuchner, C. M. Lisse, B. A. Macintosh, R. Millan-Gabet, M. C. Noecker, S. T. Ridgway, A. Roberge (Team Lead), R. Soummer, K. R. Stapelfeldt, C. C. Stark, A. J. Weinberger, and M. C. Wyatt.

Footnotes

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10.1086/667218