Astro 1: Introductory Astronomy David Cohen Spring 2014 Class 19: - - PowerPoint PPT Presentation

astro 1 introductory astronomy
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Astro 1: Introductory Astronomy David Cohen Spring 2014 Class 19: - - PowerPoint PPT Presentation

Astro 1: Introductory Astronomy David Cohen Spring 2014 Class 19: Tuesday, April1 Transits (left) for the planets radius and Doppler shift measurements (above) for the planets mass Kepler Mission (2009) With the masses of these


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Astro 1: Introductory Astronomy

David Cohen

Class 19: Tuesday, April1

Spring 2014

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Transits (left) for the planet’s radius and Doppler shift measurements (above) for the planet’s mass

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Kepler Mission (2009)

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With the masses of these planets found from their radial velocities, their densities can be calculated (next slide)

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The density trends make sense, but note some low density Jupiter-mass planets - they’re hot and bloated because they’re near their host stars

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secondary eclipse: the planet going behind its host star

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secondary eclipse: zoom-in - see how the brightness goes up before the eclipse? the planet is reflecting the most light right before the eclipse

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In our own Solar System, Venus reflects different amounts

  • f light depending on its position in its orbit (too)
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Summarizing

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Exoplanet atmospheres can be detected during transits schematic of spectroscopy of the atmosphere, as the starlight shines through it during an eclipse

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You can also think of this in terms of regular transit considerations The planet effectively has a bigger radius when you look at wavelengths at which its atmosphere is opaque vs.

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multiplanet systems (left); Note (below) lighter planets are discovered as time goes on.

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The Sun: stars have surface brightness variations. This limits the precision with which transits and Doppler shifts can be measured.

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Limb darkening...plus sunspots and a transit of Venus

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Exoplanet summary Exoplanets are common Many systems have planets very close to their host stars These “hot Jupiters” seem to have formed farther from their stars and migrated inward

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Direct imaging of exoplanets will be common someday (probably)

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Now let’s start on telescopes

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The Hubble Space Telescope – 200 km above the Earth, but it makes all the difference: above the distorting effects of the atmosphere

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In the public imagination, telescopes are refractors (i.e. have lenses) This tends to make them very long.

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Yerkes refractor: world’s biggest with a 40-inch lens There’s a physical limit to how big a telescope can get…without bending the tube or stressing the lens.

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Biggest telescopes are all reflectors (mirrors, not lenses) The light can bounce back and forth several times; they don’t need to be as long

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Huge telescopes are built only at the best sites: high altitude, dry air. Also, images from two big scopes can be combined, effectively making one huge telescope (albeit with a strange- shaped mirror).

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Kitt Peak in Arizona: More than ten telescopes, including the National Solar Observatory

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No astronomers put their eye up to a research telescope these days… Collect data on electronic detectors, such as this charge- couple device (CCD) (same type of detector as those in commercial digital cameras).

Magnified image of a CCD. Each little square is a pixel, in which photons get converted to electrons, which can be counted, or “read out”

1 m i l l i m e t e r

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The Hubble Space Telescope – 200 km above the Earth, but it makes all the difference: above the distorting effects of the atmosphere Also able to observe infrared (IR) and ultraviolet (UV) light, which is absorbed by the atmosphere.

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Now for some slides on refraction which is the basis for how lenses and telescopes work

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Since refraction bends light, but the total amount of light must be conserved, refraction by real objects tends to make patterns of light and dark…

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Where will the fisherman see the image of the fish?

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Where will the fisherman see the image of the fish?

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Where will the fisherman see the image of the fish?

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