| Ocean remote sensing requirements | |||||||||||
| OBSERVATIONS | OPTIMIZED REQUIREMENTS | THRESHOLD REQUIREMENTS | |||||||||
| Code | Application | Variable | Type | HR(km) | Cycle | Time | Acc | HR(km) | Cycle | Time | Acc |
| ALTIMETRY | |||||||||||
| A | Mesoscale Variability |
sea surface topography |
Input | 25 | 7d | 2d | 2cm | 100 | 30d | 15d | 10cm |
| B | Large scale Variability (seasonal, tides, gyres) |
sea surface topography |
Input | 100 | 10d | 2d | 1cm | 300 | 10d | 10d | 2cm |
| C | Mean sea level Variations |
sea surface topography |
Input | 200 | decades | 10d | 1mm/year | 1000 | decades | 10d | 5mm/year |
| D | Absolute Circulation heat transport |
sea surface topography |
Input | 100 | NA | NA | 1cm | 500 | NA | NA | 5-10cm |
| E | Geoid Estimation | Geoid | Base | 100 | NA | NA | 2 cm | 500 | NA | NA | ~ 1cm |
| SURFACE WIND VECTORS | |||||||||||
| F | Wind-forced circulation | Wind field | Input | 25 | 1d | 1d | 1-2m/sec 20° |
100 | 7d | 7d | 2m/sec 30° |
| SEA SURFACE RADIATIVE | |||||||||||
| G | Ocean/ Atmosphere coupling |
Sea surface temperature (radiometer) |
Input | 10 | 6h | 6h | 0.1°K (relative) |
300 | 30d | 30d | 1°K |
| H | Ocean forcing | Short-wave irradiance | Input | 200 km | 1d | 1d | 15 W/m2 | 500 km | 7d | 7d | 20-30 W/m2 |
| REMOTE SALINITY | |||||||||||
| I | Circulation and Water Transport |
Salinity | Input | 200 | 10d | 10d | 0.1PSU | 500 | 10d | 10d | 1PSU |
| SEA ICE | |||||||||||
| J | Ice Ocean coupling |
Sea ice cover | Input | 10 | 1d | 0.125d | 2% | 100 | 7d | 1d | 10% |
| OCEAN COLOR | |||||||||||
| K | Upwelling to recirculation | Ocean color signal | Input | 25 | 1d | 1d | 2% | 100 | 1d | 1d | 10% |
| SURFACE WAVES | |||||||||||
| L | Sea state prediction | Significant wave height | Input | 100 | 3h | 3h | 0.5 m | 250 | 7d | 12 h | 1 m |
| M | Sea state prediction | Period and direction | Input | 10 | 1h | 2h | 0.5 s 10° |
30 | 6h | 4h | 1 s 20° |
| Footnotes: | |||||||||||
| A requires | Wave height + wind (EM bias correction) measured from altimeter | ||||||||||
| Water vapor content / measured from on board radiometer | |||||||||||
| Ionospheric content / measured from 2 frequencies altimeter | |||||||||||
| B requires in addition | Precise positionning system = accuracy 1-2 cm for spatial resolution of 100 km; | ||||||||||
| need to address aliasing from solar tides with non-sunsynchronous orbits. | |||||||||||
| C requires in addition | Precise monitoring of transit time in the radar altimeter | ||||||||||
| A, B, C | Require repeat track at + 1 km = to filter out unknowns on geoid | ||||||||||
| A | Requires adequate sampling = at least 2 and better 3 satellites simultaneously | ||||||||||
| A, B, C | Requires long lifetime, continuity, cross calibration | ||||||||||
| D | Requires absolute calibration | ||||||||||
| E | Requires one-off missions with both high- and broad- resolution determination | ||||||||||
| F | Requirements on the wind field for sea state determination normally exceed | ||||||||||
| sampling requirements for wind forcing | |||||||||||
| G | High resolution SST: new geostationnary satellite + combination with low satellite | ||||||||||
| Table B. A table of ocean remote sensing requirements. The requirements include consideration of climate applications | |||||||||||
| as determined by the OOPC and ocean forecasting/estimation as determined by GODAE. | |||||||||||
| The requirements beyond the climate module have not be detailed here. | |||||||||||