No correlation between temperature and phase residuals, cold or warm weather. Strong (sometimes direct, sometimes inverse) correlation between temperature and pseudorange residuals during the winter months; shows some variation during summer months, but nowhere near as strong as wintertime.
January 2 and 3Hypothesis: When there is a large 'clock jump' between days at NRC2, below-zero temperatures somehow affected the equipment. The results of equipment sensitivity to changes in temperature resulted in a time-varying, non-zero behavior of the pseudorange residuals, which introduced enough 'noise' into the daily solutions to introduce a significant clock bias at midnight between days.
With respect to phase residuals, Elosegui found no correlation between residuals and time, and that holds true in the few phase examples I've examined so far. However, in the case of NRC1/2 that is not true for pseudorange residuals, which seem to show a heavily time-varying behavior in the winter. No trend/correlation seems to exist for between residuals and the elevation and azimuth angles.
The charts below attempt to establish a correlation between the
clock jumps at day boundaries and residual differences
(residual patterns and/or differences between daily average
residuals).
Plot descriptions:
| Julian date | Date/time of median | Clock jump (ps) | Daily residuals | Differences |
|---|---|---|---|---|
| 51911.0000000 | January 2, 00:00:00 | -1604.610 | January 2 to 4 | January 2-3, 3-4, and 4-5 differences |
| 51911.9982640 | January 2, 23:57:30 | 4131.262 | ||
| 51912.9982640 | January 3, 23:57:30 | 829.659 | ||
| 51913.9982640 | January 4, 23:57:30 | -3775.946 | ||
| 51914.9982640 | January 5, 23:57:30 | 3948.929 | January 5 to 7 | January 5-6 and 6-7 differences |
| 51915.9982640 | January 6, 23:57:30 | -273.220 | ||
| 51916.9982640 | January 7, 23:57:30 | 894.507 |
I took a brief look at Onsala's pseudorange residuals behavior, since the January to June plot of pseudorange residual sigmas was so steady. As expected, there is no time-varying behavior to the residuals for a random wintertime week at ONSA. ONSA is in Sweden and therefore should be pretty cold, but the temperatures may be moderated by a coastal setting, or a significant equipment difference.
| Date | Daily residuals |
|---|---|
| January 20 | January 20 to 22 |
| January 21 | |
| January 22 | |
| January 23 | January 23 to 25 |
| January 24 | |
| January 25 |
| Julian date | Date/time of median | Clock jump (ps) | Daily residuals | Differences |
|---|---|---|---|---|
| 52043.9982640 | May 14, 23:57:30 | 175.069 | May 14 to 16 | May 14-15, 15-16, and 16-17 differences |
| 52044.9982640 | May 15, 23:57:30 | 48.362 | ||
| 52045.9982640 | May 16, 23:57:30 | -77.530 | ||
| 52046.9982640 | May 17, 23:57:30 | 82.742 | May 17 to 19 | May 17-18 and 18-19 differences |
| 52047.9982640 | May 18, 23:57:30 | 268.261 | ||
| 52048.9982640 | May 19, 23:57:30 | 97.514 | ||
| 52049.9982640 | May 20, 23:57:30 | -184.671 |