{{Short description|General condition of the free surface on a large body of water}} {{Redirect|State of the sea|the Venetian Empire|Stato da Màr}} [[File:Wea00810.jpg|thumb|NOAA ship ''Delaware II'' in foul weather on Georges Bank.]] thumb|Sea State 5 and 8 range In oceanography, '''sea state''' is the general condition of the free surface on a large body of water—with respect to wind waves and swell—at a certain location and moment. A sea state is characterized by statistics, including the wave height, period, and spectrum. The sea state varies with time, as the wind and swell conditions change. The sea state can be assessed either by an experienced observer (like a trained mariner) or by using instruments like weather buoys, wave radar, or Earth observation satellites.<ref name=":0">{{Cite book |last=Holthuijsen |first=Leo H. |title=Waves in oceanic and coastal waters |date=2007 |publisher=Cambridge University Press |isbn=978-0-511-27021-5 |location=Cambridge}}</ref>

The short-term statistics describing the sea state are determined for a time interval in which the sea state is considered to be constant. This duration has to be much longer than the individual wave period, but shorter than the period in which the wind and swell conditions can be expected to vary significantly. Typically, the sea state is assumed to be constant for 15-30 minutes.<ref name=":0" />

The large number of variables involved in creating and describing the sea state cannot be quickly and easily summarized, so simpler scales are used to give an approximate but concise description of conditions for reporting in a ship's log or similar record.{{Citation needed|date=October 2025}}

== WMO sea state code== thumb|Winter, North Atlantic – Water over deck and hatches, storm with huge waves (1958) The World Meteorological Organization (WMO) sea state code largely adopts the 'wind sea' definition of the Douglas Sea Scale.{{Citation needed|date=October 2025}} The direction from which the swell is coming should be recorded.{{Citation needed|date=October 2025}}

thumb|graphic of WMO sea state codes, descriptions, and wave heights in meters

{| class=wikitable ! WMO Sea State Code !! Wave height !! Characteristics |- | 0 || {{convert|0|m}} || Calm (glassy) |- | 1 || {{convert|0|to|0.1|m|in}} || Calm (rippled) |- | 2 || {{convert|0.1|to|0.5|m}} || Smooth (wavelets) |- | 3 || {{convert|0.5|to|1.25|m}} || Slight |- | 4 ||{{convert| 1.25|to|2.5|m}} || Moderate |- | 5 || {{convert|2.5|to|4|m}} || Rough |- | 6 || {{convert|4|to|6|m}} || Very rough |- | 7 || {{convert|6|to|9|m}} || High |- | 8 || {{convert|9|to|14|m}} || Very high |- | 9 || Over {{convert|14|m}} || Phenomenal |} {| class="wikitable" |+ Character of the sea swell |- | &nbsp; || 0. None |- | '''Low''' || 1. Short or average<br /> 2. Long |- | '''Moderate''' || 3. Short<br />4. Average<br />5. Long |- | '''High''' || 6. Short<br />7. Average<br />8. Long |- | &nbsp; || 9. Confused |} == Sea states in marine engineering == In engineering applications, sea states are often characterized by the following two parameters:

* The ''significant wave height'' ''H''<sub>1/3</sub> — the mean wave height of the highest third of the waves.<ref>{{cite book |last=Munk |first=W.H. |title=Proposed uniform procedure for observing waves and interpreting instrument records |publisher=Wave Project at the Scripps Institution of Oceanography |year=1944 |location=La Jolla, California}}</ref> * The mean ''wave period'', ''T''<sub>1</sub>.

In addition to the short-term wave statistics presented above, long-term sea state statistics are often given as a joint frequency table of the significant wave height and the mean wave period. From the long and short-term statistical distributions, it is possible to find the extreme values expected over a given number of years by fitting an extreme value distribution.<ref>{{Cite journal |last=Aarnes |first=Ole Johan |last2=Breivik |first2=Øyvind |last3=Reistad |first3=Magnar |date=2012 |title=Wave Extremes in the Northeast Atlantic |url=https://journals.ametsoc.org/doi/10.1175/JCLI-D-11-00132.1 |journal=Journal of Climate |language=en |volume=25 |issue=5 |pages=1529–1543 |doi=10.1175/JCLI-D-11-00132.1 |issn=0894-8755|hdl=1956/9253 |hdl-access=free }}</ref> The extreme value distribution can then inform an engineer about the most extreme significant wave height to be expected during a lifetime of a ship or offshore structure. Using the response amplitude operators of the ship, the engineer can then use the extremes in significant wave height and wave period to calculate the most extreme loads that the ship should be able to withstand. Withstanding significant wave heights that happen on average once in 100 years or once in 1000 years is a common demand for design of ships and offshore structures.<ref>{{Cite journal |last=Jonathan |first=Philip |last2=Ewans |first2=Kevin |date=2013 |title=Statistical modelling of extreme ocean environments for marine design: A review |url=https://linkinghub.elsevier.com/retrieve/pii/S002980181300019X |journal=Ocean Engineering |language=en |volume=62 |pages=91–109 |doi=10.1016/j.oceaneng.2013.01.004|url-access=subscription }}</ref>

== CCI Sea State == The "Sea State" project within the ESA's Climate Change Initiative (CCI) program created an 18-year data set (2002–2020) covering various sea state-related Essential Climate Variables as measured by the Jason satellite series, other ocean-focused Earth observation satellites, and ''in situ'' sources.<ref>{{Cite web |title=Sea State |url=https://climate.esa.int/en/projects/sea-state/ |access-date=2025-10-11 |website=ESA Climate Office |language=en}}</ref><ref>{{Cite web |title=CCI Sea State |url=https://www.umr-lops.fr/en/Projects/Active-projects/CCI-Sea-State |access-date=2025-10-11 |website=Laboratory for Ocean Physics and Satellite remote sensing |language=en-GB}}</ref><ref>{{Cite web |last=Laboratory |first=Plymouth Marine |title=Sea State CCI |url=https://pml.ac.uk/projects/sea-state-cci/ |access-date=2025-10-11 |website=Plymouth Marine Laboratory}}</ref><ref>{{Cite web |title=CCI+ Sea State |url=https://www.dlr.de/en/eoc/research-transfer/projects-missions/cci-sea-state |access-date=2025-10-11 |website=www.dlr.de |language=en}}</ref> In 2025, data from CCI Sea State, combined with the new SWOT satellite measurements, were used to describe a new record wave height of nearly 20&nbsp;m in the open ocean.<ref>{{Cite web |title=Satellites reveal the power of ocean swell |url=https://www.esa.int/Applications/Observing_the_Earth/Space_for_our_climate/Satellites_reveal_the_power_of_ocean_swell |access-date=2025-10-11 |website=www.esa.int |language=en}}</ref><ref>{{Cite journal |last=Ardhuin |first=Fabrice |last2=Postec |first2=Taina |last3=Accensi |first3=Mickael |last4=Piolle |first4=Jean-François |last5=Dodet |first5=Guillaume |last6=Passaro |first6=Marcello |last7=De Carlo |first7=Marine |last8=Husson |first8=Romain |last9=Guitton |first9=Gilles |last10=Collard |first10=Fabrice |date=2025-09-23 |title=Sizing the largest ocean waves using the SWOT mission |url=https://www.pnas.org/doi/10.1073/pnas.2513381122 |journal=Proceedings of the National Academy of Sciences |volume=122 |issue=38 |article-number=e2513381122 |doi=10.1073/pnas.2513381122 |pmc=12478040 |pmid=40956893}}</ref>

== See also == * Beaufort scale * Cross sea * Douglas sea scale

== Citations == {{Reflist}}

== General and cited references == * {{citation | last = Bowditch | first = Nathaniel | author-link = Nathaniel Bowditch | series = H.O. publication No. 9 | title = American Practical Navigator | edition = revised | year = 1938 | publisher = United States Hydrographic Office | oclc = 31033357 }} * {{Citation | last = Faltinsen | first = O. M. | title = Sea Loads on Ships and Offshore Structures | publisher = [Cambridge University Press] | year = 1990 | isbn = 0-521-45870-6 }}

{{Physical oceanography}} {{Authority control}}

Category:Marine meteorology Category:Meteorological phenomena Category:Oceanography