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The VLT Interferometer - ESO

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2.3. DERIVED DESIRED PROPERTIES FOR THE <strong>VLT</strong>I 39<br />

spots swept along by stellar rotation and possibly coupled with the disc?<br />

<strong>The</strong> typical variation time scale of T Tau stars ranges wi thin a few days.<br />

• Stars: Late Type Giants and Supergiants. <strong>The</strong> determination of statistical<br />

properties (mean size, mean contrast in temperature) of the turbulent<br />

eddies at the surface of these stars can be done without imaging; but<br />

imaging possibilities are required to measure the mean lifetime (perhaps a<br />

few days or tens days, in fact totally unknown because of the too primitive<br />

treatment of the convection in stellar mantles). Also mapping is required<br />

to survey large spots activity, related to the magnetic field behaviour;<br />

again, the typical timescale of these phenomena is not known.<br />

• Stars: Flare stars. <strong>The</strong> rising time of flare is steep, typically 1 minute; the<br />

mean lifetime of a flare is 20 minutes. So, images, possibly by differential<br />

interferometry, during flares will have very few pixels. But to be able to<br />

observe a star during an eruption will require: (i) monitoring the star<br />

photometry with a small telescope, the array being working on another<br />

program, and (ii) adapting very rapidly the array configuration to shift<br />

to the observation of the flare star as soon as the eruption· rises.<br />

• Exotic objects. <strong>The</strong> expected size of the accretion disc of SS433 ranges<br />

from 1 to a few marcsec. SS433 varies according to two periods: 13 and<br />

164 days, and the flux varies from cycle to cycle at given phase. Furthermore,<br />

who knows about those exotic objects which could be discovered<br />

by HST, by ISO, or by the <strong>VLT</strong> ?<br />

• Solar system. We have mentioned above the interest to survey planetary<br />

surfaces. This should be done at least in two cases: Neptune (period =<br />

15.8 hours) and 10 (period = 1.8 day). Volcanic eruptions change rapidly<br />

on 10 surface, so that a survey of 10 will bring information about the<br />

inner structure of that planet, about tidal interactions, and about the<br />

solar system formation. Also very exciting is the survey of Triton, which<br />

could have active giant geysers, from Voyager 2.<br />

At infrared wavelengths, we are in the so called bright source case, due to thermal<br />

noise. We need short integrations in the (u,v) plane, but many of them to<br />

obtain many pixels and to increase the dynamical range of images. <strong>The</strong> hypersynthesis<br />

technique proposed by [Vivekanand et al 1988] would provide that.<br />

It may also be more desirable for the user to reconfigure the array in this way<br />

within a night or so, instead of within several weeks.

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