Search
Skip to Search Results- 2Atlantic Meridional Overturning Circulation
- 1Air-sea interface
- 1Atlantic Ocean
- 1Buoyancy loss
- 1Critical review
- 1Deep Convection
-
Fall 2021
The Labrador Sea experiences deep convection, a process where the oceans’ surface cools to the point where it may become more dense than the water at depth, promoting sinking and vertical mixing. This mixing can exceed 2000m in depth, producing a large volume of deep water, a crucial component in...
-
2020-01-01
Hirschi, Joel J. M., Barier, Bernard, Boning, Claus, Biastoch, Arne, Blaker, Adam T., Coward, Andrew, Danilov, Sergey, Drijfhout, Sybren, Gezlaff, Klaus, Griffies, Stephen M., Hasumi, Hiroyasu, Hewitt, Helene, Iovino, Doroteaciro, Kawasaki, Takao, Kiss, Andrew E., Koldunov, Nikolay, Marzocchi, Alice, Mecking, Jennifer V., Moat, Ben, Molines, Jean-Marc, Myers, Paul G., Penduff, Thierry, Robert, Malcolm, Treguier, Anne-Marie, Sein, Dmitry V., Sidorenko, Dmitry, Small, Justin, Spence, Paul, Thompson, LuAnne, Weijer, Wilbert, Xu, Xiaobiao
The Atlantic meridional overturning circulation (AMOC) represents the zonally integrated stream function of meridional volume transport in the Atlantic Basin. The AMOC plays an important role in transporting heat meridionally in the climate system. Observations suggest a heat transport by the...