Astronomy grows an airmass page. Relative air mass is Kasten and Young 1989, m = [sin γ + 0.50572 (γ + 6.07995)^(−1.6364)]^(−1), with the apparent elevation in degrees. Their Table II lists 1.0000 at 90°, 1.9939 at 30°, 5.5841 at 10°, and 38.0868 at the horizon, and prints a relative error of +0.432% on that horizon row. This page evaluates the formula: 0.9997 at 90°, 1.9943 at 30°, 5.5860 at 10°, and 37.92 at 0°. Plane-parallel sec(z) is exactly 2 at 30° and has no finite value at 0°. Extinction in magnitudes is k times that air mass. Krisciunas et al. 1987 summit medians at 4200 m are B 0.19 and V 0.11. Krisciunas 1990, Table 2, a hazy night at Keaau, 75 m, on 19 December 1989, is V 0.341 ± 0.020. Bennett 1982 at apparent altitude 0°, 1010 hPa, and 10°C is 34.5′. NOAA’s sunrise altitude is −0.833°, about 34′ of refraction plus about 16′ of solar semi-diameter. The setting-Sun button puts the lower limb on the apparent horizon, and Bennett’s vertical diameter is shorter than 32′. Not a forecast.