camilla.compton/Documents/sqz/templates/dtt/20250904_SRCLSQZdata.xml
and
attached.Type | Time (UTC) | SRCL Offset | Angle | DTT Ref |
FIS SQZ | 21:09:30 - 21:12:30 | -382 | (-)125.4 | ref 1 |
FIS SQZ | 21:14:45 - 21:17:45 | -200 | (-)151.0 | ref 2 |
FIS SQZ | 21:19:30 - 21:22:30 | 0 | (-)211.7 | ref 3 |
Took above data at NLG of 24.0, measaured a few hours ago 86729.
Type | Time (UTC) | SRCL Offset | Angle | DTT Ref |
FIS SQZ | 21:44:00 - 21:47:00 | -235 | (-)143.4 | ref 4 |
FIS Mid + SQZ (tuned to no sqz) | 21:48:00 - 21:51:00 | -235 | (-)151.0 | ref 5 |
FIS Mid - SQZ (tuned to no sqz) | 21:51:45 - 21:54:45 | -235 | (-)122.6 | ref 6 |
Mean SQZ (ADF off) | 21:56:00 - 21:59:00 | -235 | N/A | ref 7 |
I used this data and the no sqz data from here to run the so-called "brontosaurus" plot.
The results indicate that the SRCL offset is significantly decreased. The fit gives an offset of -235 ct for the hot OM2, compared to our current -382 ct offset.