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TPF-I SWG Report - Exoplanet Exploration Program - NASA

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D ESIGN AND A R C H I T E C T U R E T RADE S TUDIES<br />

4.9 Imaging Properties<br />

The primary motivation for the Terrestrial Planet Finder missions is their ability to directly detect photons<br />

from Earth-sized planets. Orbit determination requires that the emission can be localized and tracked over<br />

time. Spectroscopy is only meaningful if the photons can be attributed to the right object. This may be<br />

straightforward for the case of a single planet orbiting a star, but it will be very difficult to establish this a<br />

priori. The publication of the first spectrum from an exo-solar Earth would be heavily compromised by<br />

the possibility of spectral contamination by unresolved confusing sources, whether background objects,<br />

lumps in the exozodiacal dust emission, or other planets. It is, therefore, very important that <strong>TPF</strong>-I can<br />

resolve the emission from the multiple sources that might be present. This is why we must understand the<br />

a)<br />

V<br />

M<br />

E<br />

b)<br />

Percentile<br />

c)<br />

Percentile<br />

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0<br />

Earth-Venus<br />

Earth-Mars<br />

Combination<br />

0 20 40 60 80 100 120 140 160 180<br />

Separation / mas<br />

Earth-Venus<br />

Earth-Mars<br />

Combination<br />

0 20 40 60 80 100 120 140 160 180<br />

Separation / mas<br />

Figure 4-22. Angular separations of the Earth–Mars–Venus system viewed at 15 pc. (a) The<br />

angular separations are reduced as the orbits are viewed closer to edge-on. (b) Results of Monte<br />

Carlo simulation showing the probability that planets are separated by less than a particular value.<br />

For example, in 50% of cases we expect that two of the planets will be separated by 45 mas or less.<br />

(c) Same as (b), but includes the anti-star negative images of the planets.<br />

85

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