Saral validation report, cycle 134
Cycle date | 2019-10-07 - 2019-11-11 |
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Cycle quality | Mispointing levels during this cycle are close to what was observed during the previous cycle. These levels of mispointing are due to attitude deviation, and explains the higher percentage of rejected data during the validation process. Please note that the percentage of missing measurements is nominal during this cycle. Data quality is punctually impacted by these events, so that around 10.96 % of the data rejected during the validation process are mainly due to mispointing (see section ). |
Missing data | Cycle 134 has no missing pass but, track 628 is partially missing due to the calibration that occurred on 29/10/2019 between 15:31:00 to 15:58:45 (35.8% of missing data but only 5.0% are over ocean). |
5.35 cm | |
9.50 cm |
(*)When using a selection to remove shallow waters (1000 m), areas of high ocean variability and high latitudes (> |50| deg)
(**) relative to a 7-year mean (cycles <= 33) or 20-year mean (cycles >=34)
Missing measurements |
Edited measurements |
Percentage of valid measurements |
Maps for cycle 134
View the maps for cycle 134 by clicking on the thumbnail, or see previous maps and animate them (click on the legend)
SLA |
Wind |
Waves |
Long-term monitoring
Long-term crossover standard deviation |
Cyclic monitoring of differences of (Saral - Jason-2) mean SLA |
For a more complete assessment of data quality, see the Validation report for cycle 134 (pdf)