co_refract: Calculate correction to altitude due to atmospheric...

Description Usage Arguments Details Value Author(s) References See Also Examples

Description

Calculate correction to altitude due to atmospheric refraction

Usage

1
co_refract(a, altitude, pressure, temperature, to_observed, epsilon)

Arguments

a

observed (apparent) altitude, in degrees (scalar or vector)

altitude

height of the observing location, in meters. This is only used to determine an approximate temperature and pressure, if these are not specified separately. (default=0, i.e. sea level)

pressure

pressure at the observing location, in millibars (default = 1010)

temperature

temperature at the observation location, in Kelvin (default = 283)

to_observed

Flag to calculate from Apparent->Observed altitude, using the iterative technique (default = omitted gives a single estimate of the refraction correction)

epsilon

iteration accuracy (default = 0.25 arcseconds)

Details

Because the index of refraction of air is not precisely 1.0, the atmosphere bends all incoming light, making a star or other celestial object appear at a slightly different altitude (or elevation) than it really is. It is important to understand the following definitions:

Observed Altitude: The altitude that a star is SEEN to BE, with a telescope. This is where it appears in the sky. This is always GREATER than the apparent altitude.

Apparent Altitude: The altitude that a star would be at, if *there were no atmosphere* (sometimes called "true" altitude). This is usually calculated from an object's celestial coordinates. Apparent altitude is always LOWER than the observed altitude.

Thus, for example, the Sun's apparent altitude when you see it right on the horizon is actually -34 arcminutes.

This program uses couple simple formulae to estimate the effect for most optical and radio wavelengths. Typically, you know your observed altitude (from an observation), and want the apparent altitude. To go the other way, this program uses an iterative approach.

WAVELENGTH DEPENDENCE: This correction is 0 at zenith, about 1 arcminute at 45 degrees, and 34 arcminutes at the horizon FOR OPTICAL WAVELENGTHS. The correction is NON-NEGLIGIBLE at all wavelengths, but is not very easily calculable. These formulae assume a wavelength of 550 nm, and will be accurate to about 4 arcseconds for all visible wavelengths, for elevations of 10 degrees and higher. Amazingly, they are also ACCURATE FOR RADIO FREQUENCIES LESS THAN ~ 100 GHz.

It is important to understand that these formulae really can't do better than about 30 arcseconds of accuracy very close to the horizon, as variable atmospheric effects become very important.

Value

aout

observed (apparent) altitude, in degrees

Author(s)

Written Chris O'Dell

R adaptation by Arnab Chakraborty (June 2013)

References

Meeus, J., Astronomical Algorithms, Chapter 15.

Explanatory Supplement to the Astronomical Almanac, 1992.

Methods of Experimental Physics, Vol 12 Part B, Astrophysics, Radio Telescopes, Chapter 2.5, "Refraction Effects in the Neutral Atmosphere", by R.K. Crane.

See Also

co_refract_forward co_aberration

Examples

1

astrolibR documentation built on May 2, 2019, 3:26 a.m.