A Generalized Transport Theory: Water-Mass Composition and Age
Open Access
- 1 June 2002
- journal article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 32 (6) , 1932-1946
- https://doi.org/10.1175/1520-0485(2002)032<1932:agttwm>2.0.co;2
Abstract
A general theory to describe and understand advective and diffusive ocean transport is reported. It allows any passive tracer field with an atmospheric source to be constructed by superposing sea surface contributions with a generalized Green's function called the boundary propagator of the passive tracer equation. The boundary propagator has the interpretation of the joint water-mass and transit-time distribution from the sea surface. The theory thus includes the classical oceanographic idea of water-mass analysis and extends it to allow for a distribution of transit times from the sea surface. The joint water-mass and transit-time distribution contains complete information about the transport processes in the flow. It captures this information in a more accessible way than using velocity and diffusivity fields, however, at least for the case of sequestration and transport of dissolved material by the ocean circulation. The boundary propagator is thus the natural quantity to consider when discus... Abstract A general theory to describe and understand advective and diffusive ocean transport is reported. It allows any passive tracer field with an atmospheric source to be constructed by superposing sea surface contributions with a generalized Green's function called the boundary propagator of the passive tracer equation. The boundary propagator has the interpretation of the joint water-mass and transit-time distribution from the sea surface. The theory thus includes the classical oceanographic idea of water-mass analysis and extends it to allow for a distribution of transit times from the sea surface. The joint water-mass and transit-time distribution contains complete information about the transport processes in the flow. It captures this information in a more accessible way than using velocity and diffusivity fields, however, at least for the case of sequestration and transport of dissolved material by the ocean circulation. The boundary propagator is thus the natural quantity to consider when discus...Keywords
This publication has 40 references indexed in Scilit:
- The concept of age in marine modellingJournal of Marine Systems, 2001
- Toward a general theory of the age in ocean modellingOcean Modelling, 1999
- A comparison of ocean tracer dating techniques on a meridional section in the eastern North AtlanticDeep Sea Research Part I: Oceanographic Research Papers, 1997
- Temporal evolution of CFC 11 and CFC 12 concentrations in the ocean interiorJournal of Geophysical Research: Oceans, 1996
- Examining a coupled climate model using CFC‐11 as an ocean tracerGeophysical Research Letters, 1996
- The Age of Water and Ventilation Timescales in a Global Ocean ModelJournal of Physical Oceanography, 1995
- Solubility of chlorofluorocarbon 113 in water and seawaterDeep Sea Research Part I: Oceanographic Research Papers, 1995
- A chlorofluorocarbon section in the eastern North AtlanticDeep Sea Research Part A. Oceanographic Research Papers, 1992
- Chlorofluorocarbons as Time Dependent Tracers in the OceanOceanography, 1989
- The effect of boundary conditions on tracer estimates of thermocline ventilation ratesJournal of Marine Research, 1988