Abstract The global ocean is so heavily density-stratified that forcing is mostly restricted to lie at or near its top and bottom boundaries. The general circulation is determined by mass, heat and momentum exchange with the atmosphere and the solid Earth. The primary ...
CITATION STYLE
Hallberg, R., & Rhines, P. B. (2000). Boundary Sources of Potential Vorticity in Geophysical Circulations (pp. 51–65). https://doi.org/10.1007/978-94-010-0928-7_5
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