Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Sea surface temperature
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
{{Short description|Water temperature close to the ocean's surface}} {{good article}} [[File:1979- Daily sea surface temperatures 60S-60N latitudes.png|thumb|upright=1.4|Sea surface temperature since 1979 in the extrapolar region (between 60 degrees south and 60 degrees north latitude).<ref>{{Cite web |title=Copernicus: March 2024 is the tenth month in a row to be the hottest on record {{!}} Copernicus |url=https://climate.copernicus.eu/copernicus-march-2024-tenth-month-row-be-hottest-record |access-date=2024-08-15 |website=climate.copernicus.eu}}</ref>]] '''Sea surface temperature''' (or '''ocean surface temperature''') is the [[ocean temperature|temperature of ocean water]] close to the surface. The exact meaning of ''surface'' varies in the literature and in practice. It is usually between {{convert|1|mm|in|sigfig=1}} and {{convert|20|m|ft|sigfig=1}} below the [[sea]] surface. Sea surface temperatures greatly modify [[air mass]]es in the [[Atmosphere of Earth|Earth's atmosphere]] within a short distance of the shore. The [[thermohaline circulation]] has a major impact on average sea surface temperature throughout most of the world's oceans.<ref name="Rahmstorf2003">{{cite journal |last=Rahmstorf |first=S |year=2003 |title=The concept of the thermohaline circulation |url=http://www.pik-potsdam.de/~stefan/Publications/Nature/nature_concept_03.pdf |journal=Nature |volume=421 |issue=6924 |page=699 |bibcode=2003Natur.421..699R |doi=10.1038/421699a |pmid=12610602 |s2cid=4414604 |doi-access=free}}</ref> Warm sea surface temperatures can develop and [[Tropical cyclogenesis|strengthen cyclones over the ocean]]. Tropical cyclones can also cause a cool wake. This is due to turbulent mixing of the upper {{convert|30|m|ft|sigfig=1}} of the ocean. Sea surface temperature changes during the day. This is like the air above it, but to a lesser degree. There is less variation in sea surface temperature on breezy days than on calm days. Coastal sea surface temperatures can cause offshore winds to generate [[upwelling]], which can significantly cool or warm nearby landmasses, but shallower waters over a [[continental shelf]] are often warmer. Onshore winds can cause a considerable warm-up even in areas where upwelling is fairly constant, such as the northwest coast of [[South America]]. The values are important within [[numerical weather prediction]] as the sea surface temperature influences the atmosphere above, such as in the formation of [[sea breeze]]s and [[advection fog#Types|sea fog]]. It is very likely that global mean sea surface temperature increased by 0.88 °C between 1850–1900 and 2011–2020 due to [[Climate change|global warming]], with most of that warming (0.60 °C) occurring between 1980 and 2020.<ref name="AR6_WG1_Chapter9">Fox-Kemper, B., H.T. Hewitt, C. Xiao, G. Aðalgeirsdóttir, S.S. Drijfhout, T.L. Edwards, N.R. Golledge, M. Hemer, R.E. Kopp, G. Krinner, A. Mix, D. Notz, S. Nowicki, I.S. Nurhati, L. Ruiz, J.-B. Sallée, A.B.A. Slangen, and Y. Yu, 2021: [https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_Chapter09.pdf Chapter 9: Ocean, Cryosphere and Sea Level Change]. In [https://www.ipcc.ch/report/ar6/wg1/ Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change] [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, New York, USA, pages 1211–1362, doi:10.1017/9781009157896.011.</ref>{{rp|1228}} The temperatures over land are rising faster than [[Ocean temperature|ocean temperatures]]. This is because the [[Ocean heat content|ocean absorbs]] about 90% of [[Earth's energy budget|excess heat]] generated by [[climate change]].<ref name="ocean heat 92">{{cite web |title=The Oceans Are Heating Up Faster Than Expected |url=https://www.scientificamerican.com/article/the-oceans-are-heating-up-faster-than-expected/ |access-date=3 March 2020 |publisher=scientific american}}</ref> {{TOC limit|3}}
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)