446
Bibliography
Durran, D. R. (1991). The third-order Adams-Bashforth method: an attractive
alternative to leapfrog time differencing. Mon . Wea. Rev. 119,702-720.
Durran, D. R. and J. B. Klemp (1983). A compressible model for the simulation
ofmoist mountain waves. Mon. Wea. Rev. 111,2341-2361.
Durran, D. R., M.-J. Yang, D. N. Slinn, and R. G. Brown (1993). Toward more
accurate wave-permeable boundary conditions. Mon. Wea. Rev. 121, 604620.
Eliasen, E., B. Machenhauer, and E. Rasmussen (1970). On a numerical
method for integration of the hydrodynamical equations with a spectral
representation of the horizontal fields. Report no. 2, Institut for Teoretisk
Meteorologi, University of Copenhagen.
Engquist, B. and A. Majda (1977). Absorbing boundary conditions for the numerical simulation of waves. Math . Comp . 31, 629-651 .
Engquist, B. and A. Majda (1979). Radiation boundary conditions for acoustic
and elastic wave calculations. Comm. Pure Appl. Math. 32, 313-357.
Ferziger, J. H. and M. Periö (1997). Computational Methodsfor Fluid Dynamics. Berlin: Springer-Verlag .
Fjsrtoft, R. (1953). On the changes in the spectral distribution ofkinetic energy
for two-dimensional nondivergent flow. Tellus 5, 225-230.
Foreman, M. and R. Thomson (1997). Three-dimensional model simulations
of tides and buoyancy currents along the west coast of Vancouver Island.
J. Phys. Oceanogr. 27, 1300-1325.
Fornberg, B. (1973). On the instability of leap-frog and Crank-Nicolson approximations to a nonlinear partial differential equation. Math. Comp. 27,
45-57.
Fornberg, B. (1996). A Practical Guide to Pseudospectral Methods. Cambridge: Cambridge University Press.
Gal-Chen, T. and R. C. J. Somerville (1975). On the use of a coordinate
transformation for the solution of the Navier-Stokes equations. J. Comp.
Phys . 17,209-228.
Gamer, S. (1986). A radiative upper boundary condition for f -plane models .
Mon. Wea. Rev. 114, 1570-1577.
Gary, J. (1979). Nonlinear instability. In Numerical Methods Used in Atmospheric Models, Volume II of GARP Publication Series No . 17, pp. 476499. Geneva: World Meteorological Organization.
Gary, J. M. (1973). Estimate of truncation error in transformed coordinate,
primitive equation atmospheric models . J. Atmos. Sei. 30, 223-233.
Gear, C. W. (1971). Numerical Initial Value Problems in Ordinary Differential
Equations. Englewood Cliffs: Prentice-Hall.
GiII, A. E. (1982). Atmosphere-Ocean Dynamics. Orlando: Academic Press.
Bibliography
Durran, D. R. (1991). The third-order Adams-Bashforth method: an attractive
alternative to leapfrog time differencing. Mon . Wea. Rev. 119,702-720.
Durran, D. R. and J. B. Klemp (1983). A compressible model for the simulation
ofmoist mountain waves. Mon. Wea. Rev. 111,2341-2361.
Durran, D. R., M.-J. Yang, D. N. Slinn, and R. G. Brown (1993). Toward more
accurate wave-permeable boundary conditions. Mon. Wea. Rev. 121, 604620.
Eliasen, E., B. Machenhauer, and E. Rasmussen (1970). On a numerical
method for integration of the hydrodynamical equations with a spectral
representation of the horizontal fields. Report no. 2, Institut for Teoretisk
Meteorologi, University of Copenhagen.
Engquist, B. and A. Majda (1977). Absorbing boundary conditions for the numerical simulation of waves. Math . Comp . 31, 629-651 .
Engquist, B. and A. Majda (1979). Radiation boundary conditions for acoustic
and elastic wave calculations. Comm. Pure Appl. Math. 32, 313-357.
Ferziger, J. H. and M. Periö (1997). Computational Methodsfor Fluid Dynamics. Berlin: Springer-Verlag .
Fjsrtoft, R. (1953). On the changes in the spectral distribution ofkinetic energy
for two-dimensional nondivergent flow. Tellus 5, 225-230.
Foreman, M. and R. Thomson (1997). Three-dimensional model simulations
of tides and buoyancy currents along the west coast of Vancouver Island.
J. Phys. Oceanogr. 27, 1300-1325.
Fornberg, B. (1973). On the instability of leap-frog and Crank-Nicolson approximations to a nonlinear partial differential equation. Math. Comp. 27,
45-57.
Fornberg, B. (1996). A Practical Guide to Pseudospectral Methods. Cambridge: Cambridge University Press.
Gal-Chen, T. and R. C. J. Somerville (1975). On the use of a coordinate
transformation for the solution of the Navier-Stokes equations. J. Comp.
Phys . 17,209-228.
Gamer, S. (1986). A radiative upper boundary condition for f -plane models .
Mon. Wea. Rev. 114, 1570-1577.
Gary, J. (1979). Nonlinear instability. In Numerical Methods Used in Atmospheric Models, Volume II of GARP Publication Series No . 17, pp. 476499. Geneva: World Meteorological Organization.
Gary, J. M. (1973). Estimate of truncation error in transformed coordinate,
primitive equation atmospheric models . J. Atmos. Sei. 30, 223-233.
Gear, C. W. (1971). Numerical Initial Value Problems in Ordinary Differential
Equations. Englewood Cliffs: Prentice-Hall.
GiII, A. E. (1982). Atmosphere-Ocean Dynamics. Orlando: Academic Press.