Changeset 41181 for trunk/doc/release.2015/ps1.calibration/calibration.tex
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- Nov 29, 2019, 11:21:52 AM (7 years ago)
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trunk/doc/release.2015/ps1.calibration/calibration.tex
r41180 r41181 1038 1038 1039 1039 As described above, the instrumental magnitude and the calibrated magnitude 1040 are related by arithmeticmagnitude offsets which account for effects1040 are related by \textmod{additive} magnitude offsets which account for effects 1041 1041 such as the instrumental variations and atmospheric attenuation (Eqn~\ref{eqn:Mrel}). 1042 1042 %% \begin{equation} … … 1089 1089 rejections do not catch all cases of bad measurements. 1090 1090 1091 \note{justify this outlier rejection process}1092 1091 After the initial iterations, we also perform outlier rejections based 1093 1092 on the consistency of the measurements. For each star, we use a two … … 1097 1096 \& standard deviation (weighted by the inverse error) are 1098 1097 recalculated. We then reject detections which are more than 3$\sigma$ 1099 from the recalculated mean. 1098 from the recalculated mean. 1100 1099 1101 1100 Suspicious stars are also excluded from the analysis. We exclude stars … … 1115 1114 calibrated based on their overlaps with other images. 1116 1115 1117 \note{justify the choice of a factor of 10} 1116 \textadd{We note that the goal of these rejections is to avoid biasing 1117 the zero points by including clearly inconsistent or poor quality 1118 measurements. The criteria have been chosen by inspection of the 1119 dataset to avoid rejecting too many valid measurements, but the 1120 specific numbers are admittedly ad-hoc. However, as long as the 1121 exclusions do not bias the results, the exact choices are not 1122 critical. The only exclusion we make which is not symmetric with 1123 respect to the average values is the choice to reject images with 1124 substantial extinction. However, we believe this choice is 1125 justified since we know real images with clouds will often have 1126 significant extinction variations across the field and will thus be 1127 poorly represented with a single exposure zero point.} 1128 1118 1129 We overweight the ubercal measurements in order to tie the relative 1119 1130 photometry system to the ubercal zero points. Ubercal images and 1120 1131 measurements from those images are not allowed to float in the 1121 1132 relative photometry analysis. Detections from the Ubercal images are 1122 assigned weights of 10x their default (inverse-variance) weight. The 1123 calculation of the formal error on the mean magnitudes propagates this 1124 additional weight, so that the errors on the Ubercal observations 1125 dominates where they are present. 1133 assigned weights of 10x their default (inverse-variance) weight. 1134 \textadd{The choice of 10, while somewhat arbitrary, is chosen to 1135 ensure that the ubercal data will dominate the result unless it 1136 represents much less than 10\% of the measurements. Since most 1137 areas of the sky have at least a few epochs of ubercal data per 1138 filter, only for rare regions will the non-ubercal data drive the 1139 results.} The calculation of the formal error on the mean 1140 magnitudes propagates this additional weight, so that the errors on 1141 the Ubercal observations dominates where they are present. 1126 1142 1127 1143 \begin{equation} … … 1368 1384 \code{http://users.stat.umn.edu/~sandy/courses/8053/handouts/robust.pdf} 1369 1385 \code{https://arxiv.org/pdf/0807.0575.pdf} 1386 \code{https://www.redalyc.org/pdf/3939/393933924009.pdf} 1387 \code{Street, J. O., Carrol, R. J., \& Ruppert D. 1988, Am. Stat, 42, 152} 1388 \code{Green, P. J., 1984, J. R. Statist. Soc B, 42, 149} 1370 1389 1371 1390 \subsubsection{Selection of Measurements}
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