Sea State is the characterization of wave and swell, typically in terms of height, wavelength, period, and directional wave energy flux. Waves generated by ocean surface stress evolve from wind waves to swell through nonlinear dynamical processes.. Wave characteristics are modified by bathymetry when the depth of the water is comparable to the wavelength, and by surface currents. Sea state is most well known for its impacts on marine safety, marine transport and damage to structures. It is also a substantial modifier of air-sea exchanges of momentum, moisture and CO2. Waves also impact beach erosion, storm-related water damage (wave set-up contributes to storm surge), surface albedo, and transport of larva. Waves can also modify the growth or decay of sea ice.
Map of Wave Height
ECV Products and Requirements
These products and requirements reflect the Implementation Plan 2022 (GCOS-244).
The requirements are found in the complete 2022 ECVs Requirements document as well: ECV Sea State.
Products | | Wave Height |
| (*) | Unit | Values |
Horizontal Resolution | G | km | 1 |
B | 25 |
T | 100 |
Vertical Resolution | G | | - |
B | - |
T | - |
Temporal Resolution | G | h | 1 |
B | 3 |
T | 24 |
Timeliness | G | d | 7 |
B | 30 |
T | 365 |
Required Measurement Uncertainty (2-sigma) | G | % | 5 |
B | |
T | |
Stability | G | cm/ decade | 1 |
B | |
T | 10 |
(*) Goal (G): an ideal requirement above which further improvements are not necessary. Breakthrough (B): an intermediate level between threshold and goal which, if achieved, would result in a significant improvement for the targeted application. The breakthrough value may also indicate the level at which specified uses within climate monitoring become possible. It may be appropriate to have different breakthrough values for different uses. Threshold (T): the minimum requirement to be met to ensure that data are useful