From fa080de7afc95aa1c19a6e6fc0e0708ced2eadc4 Mon Sep 17 00:00:00 2001 From: Joseph Hunkeler Date: Wed, 8 Jul 2015 20:46:52 -0400 Subject: Initial commit --- math/slalib/doc/refz.hlp | 78 ++++++++++++++++++++++++++++++++++++++++++++++++ 1 file changed, 78 insertions(+) create mode 100644 math/slalib/doc/refz.hlp (limited to 'math/slalib/doc/refz.hlp') diff --git a/math/slalib/doc/refz.hlp b/math/slalib/doc/refz.hlp new file mode 100644 index 00000000..5c91ab03 --- /dev/null +++ b/math/slalib/doc/refz.hlp @@ -0,0 +1,78 @@ +.help refz Jun99 "Slalib Package" +.nf + + SUBROUTINE slREFZ (ZU, REFA, REFB, ZR) + + - - - - - + R E F Z + - - - - - + + Adjust an unrefracted zenith distance to include the effect of + atmospheric refraction, using the simple A tan Z + B tan**3 Z + model (plus special handling for large ZDs). + + Given: + ZU dp unrefracted zenith distance of the source (radian) + REFA dp tan Z coefficient (radian) + REFB dp tan**3 Z coefficient (radian) + + Returned: + ZR dp refracted zenith distance (radian) + + Notes: + + 1 This routine applies the adjustment for refraction in the + opposite sense to the usual one - it takes an unrefracted + (in vacuo) position and produces an observed (refracted) + position, whereas the A tan Z + B tan**3 Z model strictly + applies to the case where an observed position is to have the + refraction removed. The unrefracted to refracted case is + harder, and requires an inverted form of the text-book + refraction models; the formula used here is based on the + Newton-Raphson method. For the utmost numerical consistency + with the refracted to unrefracted model, two iterations are + carried out, achieving agreement at the 1D-11 arcseconds level + for a ZD of 80 degrees. The inherent accuracy of the model + is, of course, far worse than this - see the documentation for + slRFCO for more information. + + 2 At ZD 83 degrees, the rapidly-worsening A tan Z + B tan**3 Z + model is abandoned and an empirical formula takes over. Over a + wide range of observer heights and corresponding temperatures and + pressures, the following levels of accuracy (arcsec) are + typically achieved, relative to numerical integration through a + model atmosphere: + + ZR error + + 80 0.4 + 81 0.8 + 82 1.5 + 83 3.2 + 84 4.9 + 85 5.8 + 86 6.1 + 87 7.1 + 88 10 + 89 20 + 90 40 + 91 100 } relevant only to + 92 200 } high-elevation sites + + The high-ZD model is scaled to match the normal model at the + transition point; there is no glitch. + + 3 Beyond 93 deg zenith distance, the refraction is held at its + 93 deg value. + + 4 See also the routine slREFV, which performs the adjustment in + Cartesian Az/El coordinates, and with the emphasis on speed + rather than numerical accuracy. + + P.T.Wallace Starlink 19 September 1995 + + Copyright (C) 1995 Rutherford Appleton Laboratory + Copyright (C) 1995 Association of Universities for Research in Astronomy Inc. + +.fi +.endhelp -- cgit