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Astronomical Seeing

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... each cell will have a slightly different refractive index. ... If the cells of varying refractive index are far above the telescope, scintillation occurs. ... – PowerPoint PPT presentation

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Title: Astronomical Seeing


1
Astronomical Seeing
2
The Project
  • Students will be introduced to the concept of
    astronomical seeing and how it affects the
    quality of astronomical images.
  • The causes of seeing are discussed.
  • Students are presented with a selection of images
    taken under different conditions and are asked to
    chose which images have been taken under the best
    seeing conditions.
  • A discussion is then initiated on how best to
    identify the effects of seeing in an image and
    how scientists take seeing into account.

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3
Setting Up the Experiment 1
  • Students are presented the data twice.
  • Distribute copies of the image sets (.jpg format)
    for each object.
  • Images can then be analysed on computers by
    loading the images in your default image viewer
    or viewed collectively via projection.
  • Distribute a copy of the worksheet to each of the
    students.
  • Allow the students to quickly rank the quality of
    the astronomical image.
  • If the students cannot distinguish between an
    image, note this on the worksheet.

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4
Setting Up the Experiment 2
  • Deliver the lecture on seeing (concept
    introduction folder) , and allow the students to
    have a more detailed look at the images.
  • Using what they have learnt from the lecture. See
    if they can now distinguish between some of the
    better images.
  • Prompt the students to look for areas where two
    stars are close together the better the seeing
    the more resolvable (distinguishable) the two
    stars will be.
  • Look out for stars which are much dimmer in some
    images due diffusion through seeing effects.
  • Look for small features e.g. Craters on the Moon,
    the rings on Saturn or dust in galaxy and nebulae
    images. The sharper and better resolved the
    detail on these features, the better the seeing.

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5
Measuring and recording 1
  • Rank the images in order of their quality on the
    work sheet.
  • 1 Best and 6 Worst.
  • If you are unsure, place a joint ranking with the
    image you think is the closest.

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6
Astronomical Seeing
  • Even the best ground based optical telescopes are
    restricted by the presence of the Earths
    atmosphere.
  • Light from distant objects must pass through the
    Earths atmosphere before we can observe it.
  • The atmosphere contains a layer of turbulent air.
  • As the light passes through this turbulent layer
    the light waves are perturbed, altering how they
    are detected on the ground.
  • This effect is called seeing.

Image created by NSO
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7
Seeing and Meteorology
  • Variation in temperature, humidity and wind speed
    make the atmosphere very turbulent.
  • Turbulent air contains pockets or cells which
    have differing density to the region of air
    surrounding it.
  • It is cells such as these which cause clear-air
    turbulence, which is often experienced when
    flying in aircraft.
  • These cells will vary in size and shape and tend
    to drift around in the atmosphere.
  • Due to their differing density, each cell will
    have a slightly different refractive index.

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8
Refractive Index
  • Light in a vacuum travels at a constant velocity,
    c. (3x108 ms-1)
  • When light travels in a medium, the velocity
    changes by a factor of 1/n , where n is the
    refractive index of the medium.
  • The refractive index depends on the
    characteristics of the medium.
  • Changing from one medium to another will cause
    the angle of the incident light to change.
  • This occurs as the light travels from cell to
    cell.

Image created by NSO
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9
Seeing and Meteorology (2)
  • Large temperature gradients cause turbulence.
    These arise if air masses of different
    temperatures mix.
  • This will occur when hot air rises from the
    ground and meets the colder air at higher
    altitudes or when the wind drives in weather
    fronts from surrounding areas.
  • This means that seeing is better when
  • Observations are recorded at high altitude. i.e.
    The light passes through less of the turbulent
    air.
  • Observations are recorded during a period of high
    pressure, when wind speeds are low at all
    altitudes.
  • Observations are taken close to the zenith, where
    there is less atmosphere for the light to pass
    through.

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10
Scintillation
  • If the cells of varying refractive index are far
    above the telescope, scintillation occurs.
  • Scintillation is observed as irregular changes in
    the brightness of the observed objects.
  • This is what makes stars twinkle at night.
  • This will make dim objects and stars invisible on
    images taken during bad seeing.

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11
Oscillation
  • Light travelling through areas of differing
    refractive index will also change position in the
    focal plane.
  • This causes distortions in the recorded image.
  • This effect is called oscillation.
  • The distortion rate is very high, typically more
    than a 100 times a second.
  • Since exposure times are normally much longer
    than the distortion rate. Distortion is averaged
    over the time of exposure resulting in a blurry
    image.

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12
Seeing and Stars
  • The resolution limit of a telescope , or how well
    a telescope can see objects, is determined by the
    size of its main mirror.
  • However, telescope resolution is also limited by
    the diffraction of light.
  • The result of this is that distant point source
    objects, such as stars, spread out to a small
    spot known as the Airy disk.
  • Astronomical seeing causes this disk pattern to
    be disrupted into a speckle pattern.
  • This will cause stars next to each other to merge
    into a single object.
  • On larger telescopes the diffraction effects are
    very small due to the large size of the mirror.

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13
Pickering Scale
  • Due to oscillation, a point source such as a star
    will spread out and become speckled.
  • The Pickering scale is a method of quantifying
    how good or bad seeing is.
  • 1 Perfect seeing 10 Very bad seeing.

1 2 3 4
5
6 7 8 9
10
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14
Measuring and recording 2
  • Rank the images in order of the quality of seeing
    on the work sheet.
  • 1 Best Seeing to 6 Worst Seeing.
  • Record the reasons for choosing the rank of each
    image.
  • Record which part of the image has been used to
    identify bad seeing.
  • Compare the best and worst image. What are the
    differences?

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15
Discussion After the Experiment
  • Is bad seeing easier to identify on some objects
    more than others?
  • What are the best methods for identifying bad
    seeing on an astronomical image?
  • Pick the image with the worst seeing, what kind
    of weather might you have expected on that day?
  • Are there any images which have artifacts that
    cannot be attributed to seeing?

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16
Questions, Exercises and Tasks
  • What methods are there for overcoming
    astronomical seeing?
  • Are some parts of the world affected more than
    others? Where is the best place to locate a
    telescope?
  • Are small telescopes affected more than large
    telescopes?
  • Will observations of more distance objects such
    as galaxies be more prone to seeing effects?

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