Energy transports by ocean and atmosphere based on an entropy extremum principle. I - Zonal averaged transports

• Main Authors: Sohn, Byung-Ju, Smith, Eric A.
• Format: Other/Unknown Material
• Language: unknown
• Published: 1993
• Subjects: 47; Southern Ocean
• Online Access: http://ntrs.nasa.gov/search.jsp?R=19930056761

The maximum entropy production principle suggested by Paltridge (1975) is applied to separating the satellite-determined required total transports into atmospheric and oceanic components. Instead of using the excessively restrictive equal energy dissipation hypothesis as a deterministic tool for separating transports between the atmosphere and ocean fluids, the satellite-inferred required 2D energy transports are imposed on Paltridge's energy balance model, which is then solved as a variational problem using the equal energy dissipation hypothesis only to provide an initial guess field. It is suggested that Southern Ocean transports are weaker than previously reported. It is argued that a maximum entropy production principle can serve as a governing rule on macroscale global climate, and, in conjunction with conventional satellite measurements of the net radiation balance, provides a means to decompose atmosphere and ocean transports from the total transport field.