diff options
author | Joe Hunkeler <jhunkeler@gmail.com> | 2015-08-11 16:51:37 -0400 |
---|---|---|
committer | Joe Hunkeler <jhunkeler@gmail.com> | 2015-08-11 16:51:37 -0400 |
commit | 40e5a5811c6ffce9b0974e93cdd927cbcf60c157 (patch) | |
tree | 4464880c571602d54f6ae114729bf62a89518057 /noao/onedspec/doc/sys/sensfunc.ms | |
download | iraf-osx-40e5a5811c6ffce9b0974e93cdd927cbcf60c157.tar.gz |
Repatch (from linux) of OSX IRAF
Diffstat (limited to 'noao/onedspec/doc/sys/sensfunc.ms')
-rw-r--r-- | noao/onedspec/doc/sys/sensfunc.ms | 83 |
1 files changed, 83 insertions, 0 deletions
diff --git a/noao/onedspec/doc/sys/sensfunc.ms b/noao/onedspec/doc/sys/sensfunc.ms new file mode 100644 index 00000000..67b6532d --- /dev/null +++ b/noao/onedspec/doc/sys/sensfunc.ms @@ -0,0 +1,83 @@ +.EQ +delim $$ +.EN +.OM +.TO +IRAF ONEDSPEC Users +.FR +Frank Valdes +.SU +SENSFUNC Corrections +.LP +This memorandum describes the meaning of the corrections +computed by the \fBonedspec\fR task \fBsensfunc\fR. +The basic equation is + +.EQ (1) +I( lambda )~=~I sub obs ( lambda )~10 sup {0.4~(s( lambda )~+ +~A~e( lambda )~+~roman {fudge~terms})} +.EN + +where $I sub obs$ is the observed spectrum corrected to counts per second, +$I$ is the flux calibrated spectrum, $s( lambda )$ is the sensitivity +correction needed to produce +flux calibrated intensities, $A$ is the air mass at the time of the +observation, $e( lambda )$ is a standard extinction function, and, +finally, additional terms appropriately called \fIfudge\fR terms. Expressed +as a magnitude correction this equation is + +.EQ (2) +DELTA m( lambda )~=s( lambda )~+~A~e( lambda )~+~roman {fudge~terms} +.EN + +In \fBsensfunc\fR the standard extinction function is applied so that ideally +the $DELTA m$ curves (defining the sensitivity function) obtained from +observations of different stars and at different air masses are identical. +However, at times this is not the case because the observations were taken +through non-constant or nonstandard extinction. + +There are two types of fudge terms used in \fBsensfunc\fR, called \fIfudge\fR +and \fIgrey\fR. The \fIfudge\fR correction is a separate constant, +independent of wavelength or air mass, applied to each observation to shift +the sensitivity curves to the same level on average. This is done to +determine the shape of the sensitivity curve only. +The fudge correction for each observation is obtained by determining +the average magnitude shift over all wavelenths relative to the observation +with the smallest sensitivity correction. A composite sensitivity curve +is then determined from the average of all the fudged observations. +The fudge terms are not incorporated in the sensitivity or extinction +corrections applied to calibrate the spectra. Thus, after applying the +sensitivity and extinction corrections to the standard star spectra there +will be absolute flux scale errors due to the observing conditions. + +If the observer believes that there is an actual calibratible error in +the standard extinction then \fBsensfunc\fR can be used to determine a +correction which is a linear function of the air mass. This is done by +relating the fudge values (the magnitude shifts needed to bring observations +to the same sensitivity level) to the air mass of the observations. +The \fIgrey\fR term is obtained by the least square fit to + +.EQ (3) +f sub i~=~G~DELTA A sub i~=~G~A sub i~+~C +.EN + +where the $f sub i$ are the fudge values relative to the observation with +the smallest sensitivity correction and the $DELTA A sub i$ are the +air mass differences relative to this same observation. The slope constant +$G$ is what is refered to as the \fIgrey\fR term. The constant term, +related to the air mass of the reference observation to which the other +spectra are shifted, is absorbed in the sensitivity function. +The modified equation (2) is + +.EQ (4) +DELTA m( lambda )~=~s ( lambda ) + A~(e( lambda )~+~G) +.EN + +It is important to realize that equation (3) can lead to erroneous results +if there is no real relation to the air mass or the air mass range is +too small. In other words applying the grey term correction will produce +some number for $G$ but it may be worse than no correction. A plot of +the individual fudge constants, $f sub i$, and the air mass or +air mass differences would be useful to evaluate the validity of the +grey correction. The actual magnitude of the correction is not $G$ +but $DELTA A~G$ where $DELTA A$ is the range of observed air mass. |