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Photometry Atmosphere & Standardization ASTR 3010 Lecture 13 Textbook 10.6 & 10.7
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Extinction by Atmosphere Observing the incoming radiation at depth H in the atmosphere. Observing the incoming radiation at depth H in the atmosphere. Measured spectrum φ A (λ) where optical depth τ where optical depth τ and X is air mass. and X is air mass.
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Different notations
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Bouguer’s Law Take multiple measurements of non-varying object at several different airmasses! one can get a mean extinction coeff from the slope with known airmass, one can recover m λ for any other stars! X 0123 slope = k
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Sources of extinction 1.Rayleigh scattering 2.Absorption by Ozone 3.Scattering by Aerosols 4.Molecular-band absorption stable over long time variable due to a weather system
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Photometric Condition To be able to use Bouguer’s Law, we need two conditions 1.k is stationary 2.k is isotropic when these two conditions are met, the night is called “photometric” X 0123 slope = k Example of non-stationary extinction during the obs.
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Measuring monochromatic extinction 1.Assume use observatory’s value 2.Use a reference observe a star with known m λ 3.From the Bouguer line of your measurements 4.Variable extinction / multi-night data o measure two standard stars at a given time at different airmass o repeat the pair observation several times per night 5.Use all data X 0123
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Heterochromatic extinction Apparent magnitudes versus airmass different slopes for different colors Apparent magnitudes versus airmass different slopes for different colors Forbes Effect = spectrum of a star changes with airmass
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2 nd order extinction coefficients Taylor Expand k P (or parameterize k P ) Taylor Expand k P (or parameterize k P ) For example, (B-V) color can be used to indicate the spectral shape. For example, (B-V) color can be used to indicate the spectral shape. This color-dependent term is not changing rapidly and takes many data to measure one can use observatory’s value This color-dependent term is not changing rapidly and takes many data to measure one can use observatory’s value
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Transformation to a standard system instrumental (outside the atmosphere) magnitudes measured with two filters at λ 1 and λ 2 where standard wavelengths are λ S1 and λ S2. instrumental (outside the atmosphere) magnitudes measured with two filters at λ 1 and λ 2 where standard wavelengths are λ S1 and λ S2.From we get Then, color term color coefficient efficiency term zero-point constant
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Transformation to a standard system In practice, you measure m λ1 and (color index) 12 or m λ1 and m λ2 In practice, you measure m λ1 and (color index) 12 or m λ1 and m λ2 then plot X = Color Index 0+1+2
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Example (Homework) An observer used B and V filters to obtain four exposures of the same field at different air masses: two B exposures at air masses 1.05 and 2.13, and two V exposures at airmasses 1.10 and 2.48. Four stars in this field are photometric standards. Their measured magnitudes are given below. (B-V)Vb(1)b(2)v(1)v(2) Airmass1.052.131.102.48 Star A-0.0712.019.85310.6878.7789.427 Star B0.3612.4410.69311.4799.1609.739 Star C0.6912.1910.75911.4628.8739.425 Star D1.1512.8911.89812.5479.52210.001
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Example (Homework) 1.Calculate extinction coefficients for the instrumental system for B and V bands. 2.Compute the standard transformation coefficients α V and α B-V (or α B ) 3.Calculate standard magnitudes of Obj1 (i.e., V and B-V) whose instrumental magnitudes are v=9.850 and b=10.899 taken at airmass=1.50 (B-V)Vb(1)b(2)v(1)v(2) Airmass1.052.131.102.48 Star A-0.0712.019.85310.6878.7789.427 Star B0.3612.4410.69311.4799.1609.739 Star C0.6912.1910.75911.4628.8739.425 Star D1.1512.8911.89812.5479.52210.001
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Example (Homework) 1.Calculate extinction coefficients for the instrumental system for B and V bands. (B-V)Vb(1)b(2)v(1)v(2) Airmass1.052.131.102.48 Star A-0.0712.019.85310.6878.7789.427 Star B0.3612.4410.69311.4799.1609.739 Star C0.6912.1910.75911.4628.8739.425 Star D1.1512.8911.89812.5479.52210.001 unknown Plot b(2)-b(1)/(X 2 -X 1 ) and measure the slope for k 1 (B-V)
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Example (Homework) 2.Compute the standard transformation coefficients α V and α B-V (or α B ) (B-V)Vb(1)b(2)v(1)v(2) Airmass1.052.131.102.48 Star A-0.0712.019.85310.6878.7789.427 Star B0.3612.4410.69311.4799.1609.739 Star C0.6912.1910.75911.4628.8739.425 Star D1.1512.8911.89812.5479.52210.001 Plot as a function of color index (e.g., B-V) Slope = α 12 y-intercept= α 1
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Example (Homework) 3.Calculate standard magnitudes of Obj1 (i.e., V and B-V) whose instrumental magnitudes are v=9.850 and b=10.899 taken at airmass=1.50
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In summary… Important Concepts Bouguer’s Law Photometric condition Standard Transformation Important Terms Extinction coefficient Forbes effect Chapter/sections covered in this lecture : 10.6 & 10.7
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