Residence time in a semi-enclosed domain from the solution of an adjoint problem

The residence time measures the time spent by a water parcel or a pollutant in a given water body and is therefore a widely used concept in environmental studies. While many previous studies rely on severe hypotheses (assuming stationarity of the flow and/or neglecting diffusion) to evaluate the residence time, the paper introduces a general method for computing the residence time and/or the mean residence time without such simplifying hypotheses. The method is based on the resolution of an adjoint advection-diffusion problem and is therefore primarily meant to be used with numerical models. The method and its implications are first introduced using a simplified one-dimensional analytical model. The approach is then applied to the diagnostic of the three-dimensional circulation on the Northwest European Continental Shelf. (C) 2004 Elsevier Ltd. All rights reserved.

[1]  É. Deleersnijder,et al.  The concept of age in marine modelling II. Concentration distribution function in the English Channel and the North Sea , 2002 .

[2]  F. Kestner,et al.  Estuaries : a physical introduction , 1974 .

[3]  Bert Bolin,et al.  A note on the concepts of age distribution and transit time in natural reservoirs , 1973 .

[4]  P. Morse,et al.  Methods of theoretical physics , 1955 .

[5]  Timothy M. Hall,et al.  Transit-Time and Tracer-Age Distributions in Geophysical Flows , 2000 .

[6]  Eric Deleersnijder,et al.  The concept of age in marine modelling I. Theory and preliminary model results , 2001 .

[7]  J. Beckers,et al.  Dissection of the GHER turbulence closure scheme , 1999 .

[8]  Eric Deleersnijder,et al.  Toward a general theory of the age in ocean modelling , 1999 .

[9]  É. Delhez,et al.  Preliminary results of 3-D baroclinic numerical models of the mesoscale and macroscale circulations on the North-Western Europena Continental Shelf , 1992 .

[10]  John Marshall,et al.  Evaluating carbon sequestration efficiency in an ocean circulation model by adjoint sensitivity analysis , 2004 .

[11]  É. Delhez Reconnaissance of the general circulation of the North-Western European Continental Shelf by means of a three-dimensional turbulent closure model , 1996 .

[12]  J. Hobbie,et al.  Estuarine science: a synthetic approach to research and practice , 2000 .

[13]  U. Brinkman,et al.  Net fluxes of pesticides from the Scheldt Estuary into the North Sea: a model approach. , 2002, Environmental pollution.

[14]  R. Pingree Chapter 13 Physical Oceanography of the Celtic Sea and English Channel , 1980 .

[15]  P. Herman,et al.  Estimating estuarine residence times in the Westerschelde (The Netherlands) using a box model with fixed dispersion coefficients , 1995, Hydrobiologia.

[16]  F. Martins,et al.  A methodology to estimate renewal time scales in estuaries: the Tagus Estuary case , 2003 .

[17]  I. D. James,et al.  Advection schemes for shelf sea models , 1996 .

[18]  R. Vollenweider,et al.  Advances in defining critical loading levels for phosphorus in lake eutrophication. , 1976 .

[19]  J. Salomon,et al.  FLUXMANCHE radiotracers measurements: A contribution to the dynamics of the English Channel and North Sea , 1995 .

[20]  K. Ruddick,et al.  Haline stratification in the Rhine-Meuse freshwater plume: a three-dimensional model sensitivity analysis , 1995 .

[21]  D. McDowell,et al.  Hydrodynamics of estuaries , 1977 .

[22]  W. Boynton,et al.  The fate of nitrogen and phosphorus at the land-sea margin of the North Atlantic Ocean , 1996 .

[23]  H. Takeoka Fundamental concepts of exchange and transport time scales in a coastal sea , 1984 .

[24]  Nancy E. Monsen,et al.  A comment on the use of flushing time, residence time, and age as transport time scales , 2002 .

[25]  L. Arneborg Turnover times for the water above sill level in Gullmar Fjord , 2004 .