Oceanic Frontogenesis
2021 ◽
Vol 13
(1)
◽
pp. 227-253
Keyword(s):
Frontogenesis is the fluid-dynamical processes that rapidly sharpen horizontal density gradients and their associated horizontal velocity shears. It is a positive feedback process where the ageostrophic, overturning secondary circulation in the cross-front plane accelerates the frontal sharpening until an arrest occurs through frontal instability and other forms of turbulent mixing. Several well-known types of oceanic frontal phenomena are surveyed, their impacts on oceanic system functioning are assessed, and future research is envisioned.
Keyword(s):
2017 ◽
Vol 122
(23)
◽
Keyword(s):
2015 ◽
Vol 13
(3)
◽
pp. 1-24
◽
Keyword(s):
Keyword(s):
Keyword(s):
2011 ◽
Vol 23
(2)
◽
pp. 703-721
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