Editing Sverdrup (section)

== Examples ==
The water transport in the [[Gulf Stream]] gradually increases from {{val|30|u=Sv}} in the [[Florida Current]] to a maximum of {{val|150|u=Sv}} south of Newfoundland at 55°&nbsp;W [[longitude]].<ref>{{Cite web |url=http://oceancurrents.rsmas.miami.edu/atlantic/gulf-stream.html |title=The Gulf Stream |website=Ocean Surface Currents |publisher=[[University of Miami]] [[Rosenstiel School of Marine, Atmospheric, and Earth Science]] |access-date=12 August 2017}}</ref>

The [[Antarctic Circumpolar Current]], at approximately {{val|125|u=Sv}}, is the largest ocean current.<ref>{{Cite web |url=http://oceancurrents.rsmas.miami.edu/southern/antarctic-cp.html |title=The Antarctic Circumpolar Current |website=Ocean Surface Currents |publisher=[[University of Miami]] [[Rosenstiel School of Marine, Atmospheric, and Earth Science]] |access-date=12 August 2017}}</ref>

The entire global input of [[fresh water]] from rivers to the ocean is approximately {{val|1.2|u=Sv}}.<ref>{{Cite journal |last1=Lagerloef |first1=Gary |last2=Schmitt |first2=Raymond |last3=Schanze |first3=Julian |last4=Kao |first4=Hsun-Ying |date=2010-12-01 |title=The Ocean and the Global Water Cycle |url=https://tos.org/oceanography/article/the-ocean-and-the-global-water-cycle |journal=Oceanography |volume=23 |issue=4 |pages=82–93 |doi=10.5670/oceanog.2010.07|doi-access=free }}</ref>