Differential Atmospheric Refraction at an Altitude of 2KM relative to a reference wavelength of 5000A
Sec Z | 3000A | 3500A | 4000A | 4500A | 5000A | 5500A | 6000A | 6500A |
1.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 |
1.05 | 0.68 | 0.38 | 0.20 | 0.08 | 0.00 | -0.06 | -0.11 | -0.14 |
1.10 | 0.97 | 0.55 | 0.29 | 0.12 | 0.00 | -0.09 | -0.15 | -0.20 |
1.15 | 1.20 | 0.68 | 0.36 | 0.15 | 0.00 | -0.11 | -0.19 | -0.25 |
1.20 | 1.40 | 0.80 | 0.42 | 0.17 | 0.00 | -0.13 | -0.22 | -0.30 |
1.25 | 1.59 | 0.90 | 0.48 | 0.20 | 0.00 | -0.14 | -0.25 | -0.33 |
1.30 | 1.76 | 1.00 | 0.53 | 0.22 | 0.00 | -0.16 | -0.28 | -0.37 |
1.35 | 1.92 | 1.09 | 0.58 | 0.24 | 0.00 | -0.17 | -0.30 | -0.40 |
1.40 | 2.07 | 1.18 | 0.62 | 0.26 | 0.00 | -0.19 | -0.33 | -0.44 |
1.45 | 2.22 | 1.26 | 0.67 | 0.28 | 0.00 | -0.20 | -0.35 | -0.47 |
1.50 | 2.37 | 1.34 | 0.71 | 0.29 | 0.00 | -0.21 | -0.37 | -0.50 |
1.55 | 2.51 | 1.42 | 0.75 | 0.31 | 0.00 | -0.23 | -0.40 | -0.53 |
1.60 | 2.64 | 1.50 | 0.80 | 0.33 | 0.00 | -0.24 | -0.42 | -0.56 |
1.65 | 2.78 | 1.58 | 0.84 | 0.34 | 0.00 | -0.25 | -0.44 | -0.59 |
1.70 | 2.91 | 1.65 | 0.88 | 0.36 | 0.00 | -0.26 | -0.46 | -0.61 |
1.75 | 3.04 | 1.73 | 0.92 | 0.38 | 0.00 | -0.27 | -0.48 | -0.64 |
1.80 | 3.17 | 1.80 | 0.95 | 0.39 | 0.00 | -0.29 | -0.50 | -0.67 |
1.85 | 3.29 | 1.87 | 0.99 | 0.41 | 0.00 | -0.30 | -0.52 | -0.69 |
1.90 | 3.42 | 1.94 | 1.03 | 0.42 | 0.00 | -0.31 | -0.54 | -0.72 |
2.00 | 3.54 | 2.01 | 1.07 | 0.44 | 0.00 | -0.32 | -0.56 | -0.75 |
2.05 | 3.67 | 2.08 | 1.10 | 0.45 | 0.00 | -0.33 | -0.58 | -0.77 |
2.10 | 3.91 | 2.22 | 1.18 | 0.48 | 0.00 | -0.35 | -0.62 | -0.82 |
2.20 | 4.15 | 2.36 | 1.25 | 0.51 | 0.00 | -0.37 | -0.66 | -0.87 |
2.30 | 4.38 | 2.49 | 1.32 | 0.54 | 0.00 | -0.40 | -0.69 | -0.92 |
2.40 | 4.62 | 2.62 | 1.39 | 0.57 | 0.00 | -0.42 | -0.73 | -0.97 |
Sec Z | 7000A | 7500A | 8000A | 8500A | 9000A | 9500A | 10000A |
1.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 | 0.00 |
1.05 | -0.17 | -0.19 | -0.21 | -0.23 | -0.24 | -0.25 | -0.26 |
1.10 | -0.24 | -0.28 | -0.30 | -0.32 | -0.34 | -0.36 | -0.37 |
1.15 | -0.30 | -0.34 | -0.38 | -0.40 | -0.42 | -0.44 | -0.46 |
1.20 | -0.35 | -0.40 | -0.44 | -0.47 | -0.50 | -0.52 | -0.54 |
1.25 | -0.40 | -0.45 | -0.50 | -0.53 | -0.56 | -0.59 | -0.61 |
1.30 | -0.44 | -0.50 | -0.66 | -0.59 | -0.62 | -0.65 | -0.67 |
1.35 | -0.48 | -0.55 | -0.60 | -0.64 | -0.68 | -0.71 | -0.73 |
1.40 | -0.52 | -0.59 | -0.65 | -0.69 | -0.73 | -0.77 | -0.79 |
1.45 | -0.56 | -0.63 | -0.69 | -0.74 | -0.79 | -0.82 | -0.85 |
1.50 | -0.60 | -0.68 | -0.74 | -0.79 | -0.84 | -0.87 | -0.91 |
1.55 | -0.63 | -0.72 | -0.78 | -0.84 | -0.89 | -0.93 | -0.96 |
1.60 | -0.67 | -0.75 | -0.83 | -0.88 | -0.93 | -0.98 | -1.01 |
1.65 | -0.70 | -0.79 | -0.87 | -0.93 | -0.98 | -1.03 | -1.06 |
1.70 | -0.73 | -0.83 | -0.91 | -0.97 | -1.03 | -1.07 | -1.11 |
1.75 | -0.77 | -0.87 | -0.95 | -1.02 | -1.07 | -1.12 | -1.16 |
1.80 | -0.80 | -0.90 | -0.99 | -1.06 | -1.12 | -1.17 | -1.21 |
1.85 | -0.83 | -0.94 | -1.03 | -1.10 | -1.16 | -1.22 | -1.26 |
1.90 | -0.86 | -0.98 | -1.07 | -1.14 | -1.21 | -1.26 | -1.31 |
2.00 | -0.89 | -1.01 | -1.11 | -1.19 | -1.25 | -1.31 | -1.36 |
2.05 | -0.92 | -1.05 | -1.15 | -1.23 | -1.30 | -1.35 | -1.40 |
2.10 | -0.99 | -1.12 | -1.22 | -1.31 | -1.38 | -1.44 | -1.50 |
2.20 | -1.05 | -1.18 | -1.30 | -1.39 | -1.47 | -1.53 | -1.59 |
2.30 | -1.11 | -1.25 | -1.37 | -1.47 | -1.55 | -1.62 | -1.68 |
2.40 | -1.16 | -1.32 | -1.44 | -1.55 | -1.63 | -1.70 | -1.77 |
Notes:
1. Sec Z is essentially equal to air mass over this range.
2. The CFADC can correct for atmospheric dispersion up to Sec Z=2.4 (65 degrees zenith angle)
3. The useful short wavelength limit of the Hydra corrector is 3350A
4. Source of this table: ESO