Changeset 5938
- Timestamp:
- Jan 6, 2006, 5:10:54 PM (20 years ago)
- File:
-
- 1 edited
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trunk/doc/pslib/psLibSDRS.tex (modified) (2 diffs)
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trunk/doc/pslib/psLibSDRS.tex
r5915 r5938 1 %%% $Id: psLibSDRS.tex,v 1.37 2 2006-01-06 02:39:46 jhoblittExp $1 %%% $Id: psLibSDRS.tex,v 1.373 2006-01-07 03:10:54 price Exp $ 2 2 \documentclass[panstarrs,spec]{panstarrs} 3 3 … … 6954 6954 typedef enum { 6955 6955 PS_PRECESS_ROUGH, 6956 PS_PRECESS_COMPLETE,6957 6956 PS_PRECESS_IAU2000A, 6957 PS_PRECESS_COMPLETE_A, 6958 PS_PRECESS_COMPLETE_B 6958 6959 } psPrecessMethod; 6959 6960 \end{datatype} 6961 6962 \code{PS_PRECESS_ROUGH} indicates that an approximate precession 6963 rotation is determined from a cubic polynomial in the time difference 6964 (ADD 3.4.3). \code{PS_PRECESS_IAU2000A} indicates that the precession 6965 rotation is determined from differencing the two rotations obtained 6966 from applying the IAU 2000A model (\code{psEOC_PrecessionModel}, 6967 followed by \code{psSphereRot_CEOtoGCRS}) at each epoch. 6968 \code{PS_PRECESS_COMPLETE_A} and \code{PS_PRECESS_COMPLETE_B} 6969 indicates that the precession rotation is the same as for 6970 \code{PS_PRECESS_IAU2000A}, except that the earth pole correction 6971 published by the IERS is included (using the appropriate bulletin in 6972 \code{psEOC_PrecessionCorr} --- \code{PS_IERS_A} for 6973 \code{PS_PRECESS_COMPLETE_A}, and \code{PS_IERS_B} for 6974 \code{PS_PRECESS_COMPLETE_B}). 6960 6975 6961 6976 \subsection{Atmospheric Effects}
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