R.M.S Values of Auxiliary Corrections |
IPF Baseline: | Phase: |
The surface height measurements provided in Cryosat L2 data are corrected for atmospheric propogation delays and geophysical surface variations. In this tool the r.m.s value and spatial distribution of each correction is monitored for each 30-day data take:
| Show Correction Availability |
| 30-day Data take: | <<104 (4/4/19 ..) | 105 (4/5/19 ..) | 106 (3/6/19 ..) | 107 (3/7/19 ..) | Trend |
| Dry Tropospheric | 2219.8 | - | - | - | View |
| Wet Tropospheric | 140.399 | - | - | - | View |
| Inv. Barometric | 157.119 | - | - | - | View |
| Dynamic Atmos. | 137.656 | - | - | - | View |
| Ionospheric | 20.6186 | - | - | - | View |
| Sea State Bias | 165.305 | - | - | - | View |
| Ocean Tide | 357.84 | - | - | - | View |
| Long Period Tide | 18.1557 | - | - | - | View |
| Ocean Loading Tide | 13.9553 | - | - | - | View |
| Solid Earth Tide | 79.6064 | - | - | - | View |
| Geocentric Polar Tide | 3.29929 | - | - | - | View |
Click on a rms value to view a map of the corresponding correction rms values