;+
; NAME:
; CO_REFRACT()
;
; PURPOSE:
; Calculate correction to altitude due to atmospheric refraction.
;
; DESCRIPTION:
; CO_REFRACT can calculate both apparent altitude from observed altitude and
; vice-versa.
;
; CALLING SEQUENCE:
; new_alt = CO_REFRACT(old_alt, [ ALTITUDE= , PRESSURE= , $
; TEMPERATURE= , /TO_OBSERVED , EPSILON= ])
;
; INPUT:
; old_alt - Observed (apparent) altitude, in DEGREES. (apparent if keyword
; /TO_OBSERVED set). May be scalar or vector.
;
; OUTPUT:
; Function returns apparent (observed) altitude, in DEGREES. (observed if
; keyword /TO_OBSERVED set). Will be of same type as input
; altitude(s).
;
; OPTIONAL KEYWORD INPUTS:
; ALTITUDE : The 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 : The pressure at the observing location, in millibars.
; TEMPERATURE: The temperature at the observing location, in Kelvin.
; EPSILON: When keyword /TO_OBSERVED has been set, this is the accuracy
; to obtain via the iteration, in arcseconds [default = 0.25
; arcseconds].
; /TO_OBSERVED: Set this keyword to go from Apparent->Observed altitude,
; using the iterative technique.
;
; Note, if altitude is set, but temperature or pressure are not, the
; program will make an intelligent guess for the temperature and pressure.
;
; DESCRIPTION:
;
; 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.
;
; EXAMPLE:
; The lower limb of the Sun is observed to have altitude of 0d 30'.
; Calculate the the true (=apparent) altitude of the Sun's lower limb using
; mean conditions of air pressure and temperature
;
; IDL> print, co_refract(0.5) ===> 0.025degrees (1.55')
; 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.
;
; REFERENCES:
; 1. Meeus, Astronomical Algorithms, Chapter 15.
; 2. Explanatory Supplement to the Astronomical Almanac, 1992.
; 3. Methods of Experimental Physics, Vol 12 Part B, Astrophysics,
; Radio Telescopes, Chapter 2.5, "Refraction Effects in the Neutral
; Atmosphere", by R.K. Crane.
;
;
; DEPENDENCIES:
; CO_REFRACT_FORWARD (contained in this file and automatically compiled).
;
; AUTHOR:
; Chris O'Dell
; Assistant Professor of Atmospheric Science
; Colorado State University
; Email: odell@atmos.colostate.edu
;
; REVISION HISTORY:
; version 1 (May 31, 2002)
; Update iteration formula, W. Landsman June 2002
; Corrected slight bug associated with scalar vs. vector temperature and
; pressure inputs. 6/10/2002
; Fixed problem with vector input when /TO_OBSERVED set W. Landsman Dec 2005
; Allow arrays with more than 32767 elements W.Landsman/C.Dickinson Feb 2010
;-
function co_refract_forward, a, P=P, T=T
; INPUTS
; a = The observed (apparent) altitude, in DEGREES.
; May be scalar or vector.
;
; INPUT KEYWORDS
; P: Pressure [in millibars]. Default is 1010 millibars. [scalar or vector]
; T: Ground Temp [in Celsius]. Default is 0 Celsius. [scalar or vector]
compile_opt idl2
d2r = !dpi/180.
if n_elements(P) eq 0 then P = 1010.
if n_elements(T) eq 0 then T = 283.
; you have observed the altitude a, and would like to know what the "apparent"
; altitude is (the one behind the atmosphere).
w = where(a LT 15.)
R = 0.0166667/tan((a + 7.31/(a+4.4))*d2r)
;R = 1.02/tan((a + 10.3/(a+5.11))*d2r)/60.
; this formula goes the other direction!
if w[0] ne -1 then R[w] = 3.569*(0.1594 + .0196*a[w] + $
.00002*a[w]^2)/(1.+.505*a[w]+.0845*a[w]^2)
tpcor = P/1010. * 283/T
R = tpcor * R
return, R
END
function co_refract, a, altitude=altitude, pressure=pressure, $
temperature=temperature, To_observed=To_observed, epsilon=epsilon
; This is the main window. Calls co_refract_forward either iteratively or a
; single time depending on the direction we are going for refraction.
compile_opt idl2
o = keyword_set(To_observed)
alpha = 0.0065 ; temp lapse rate [deg C per meter]
if n_elements(altitude) eq 0 then altitude = 0.
if n_elements(temperature) eq 0 then begin
if altitude GT 11000 then temperature = 211.5 $
else temperature = 283.0 - alpha*altitude
endif
; estimate Pressure based on altitude, using U.S. Standard Atmosphere formula.
if n_elements(pressure) eq 0 then $
pressure = 1010.*(1-6.5/288000*altitude)^5.255
if n_elements(epsilon) eq 0 then $
epsilon = 0.25 ; accuracy of iteration for observed=1 case, in arcseconds
if not o then begin
aout = a - co_refract_forward(a,P=pressure,T=temperature)
endif else begin
aout = a*0.
na = n_elements(a)
; if there are multiple elevations but only one temp and pressure entered,
; expand those to be arrays of the same size.
P = pressure + a*0. & T = temperature + a*0.
for i=0L,na-1 do begin
;calculate initial refraction guess
dr = co_refract_forward(a[i],P=P[i],T=T[i])
cur = a[i] + dr ; guess of observed location
repeat begin
last = cur
dr = co_refract_forward(cur,P=P[i],T=T[i])
cur= a[i] + dr
endrep until abs(last-cur)*3600. LT epsilon
aout[i] = cur
endfor
endelse
if N_elements(aout) GT 1 then return, reform(aout) else return, aout
END