437
Evensen, G., 1994b: Sequential data assimilation with a nonlinear
quasi_geostrophic model using Monte Carlo methods to forecast error statistics, J. Geophys. Res., 99(C5), 10,143-10,162.
Evensen, G. and N. Fario, 1997: A weak constrain variational inverse for the
Lorenz equations using substitutional methods. J. Meteor. Soc. Japan, 7(IB),
229-243.
Evensen, G., 1997: Advanced data assimilation for strongly nonlinear dynamics,
Mon. Weather Rev., 125, 1342-1354.
Evensen, G., and P. J. van Leeuwen, 1996: Assimilation of Geosat altimeter data
for the Agulhas current using the ensemble Kalman filter with a quasi~eostrophic model, Mon. Weather Rev., 124, 85--96.
Ezer, T. and GL Mellor, 2000: Sensitivity studies with the North Atlantic sigma
coordinate Princeton Ocean Model. In: Ocean Circulation Model Evalutation
Experiments for the North Atlantic Basin, E.P. Chassignet and P. MalanotteRizzoli (Eds.), Dyn. Atmos. Ocean, 32,185-208.
Ezer, T., 1999: Decadal variabilities ofthe upper layers ofthe subtropical North
Atlantic: An ocean model study. J. Phys. Oceanogr., 29(12), 3111-3124.
Ezer, T., and G. L. Mellor, 1994: Continuous assimilation of Geosat altimeter
data into a three dimensional primitive equation Gulf stream model, J. Phys.
Oceanogr., 24, 832-847.
Ezer, T., and G. L. Mellor, 1997: Simulations ofthe Atlantic Ocean with a free
surface sigma coordinate ocean model. J. Geophys. Res., 102, 15,647-15,657.
Falkowski, P.G. and lA.Raven ,1997: Aquatic photosynthesis. Oxford, Blackwe1l375pp.
Farrell, B. F, 1985: Transient growth of damped baroclinic waves, J. Atmos Sci.,
42,2718-2727.
Farrell, B. F., 1988: Optimal excitation ofneutral Rossby waves, J. Atmos.Sci.,
45,163-172.
Farrell, B. F., 1989: Optimal excitation of baroc1inic waves, J. Atmos.Sci., 46,
1193-1206.
Farrell, B. F., 1990: Small error dynamics and the predictability of atmospheric
flows, J. Atmos. Sci., 47, 2409-2416.
Farrell, B., and A.M.Moore, 1992: An adjoint method for obtaining the most
rapidly growing perturbation to oceanic flows. J. Phys. Ocean., 22(4), 338349.
Fasham, M.J.R., H.W.Ducklow and S.M.McKelvie, 1990: A nitrogen based
model of plankton dynamics in the oceanic mixed layer. J. Mar. Res., 48,
591-639.
Fasham, M.J.R., 1978: The statistical and mathematical analysis of plankton
patchiness. Oceanography and Marine Biology. An Annual Review, 16,4379.
Fasham, M. J. R., 1993: Ecosystem behavior at Bermuda station "S" and ocean
weather station "India": a general circulation model and observational analysis. Global Biogeochemical Cycles, 7(2): 379-415.
Evensen, G., 1994b: Sequential data assimilation with a nonlinear
quasi_geostrophic model using Monte Carlo methods to forecast error statistics, J. Geophys. Res., 99(C5), 10,143-10,162.
Evensen, G. and N. Fario, 1997: A weak constrain variational inverse for the
Lorenz equations using substitutional methods. J. Meteor. Soc. Japan, 7(IB),
229-243.
Evensen, G., 1997: Advanced data assimilation for strongly nonlinear dynamics,
Mon. Weather Rev., 125, 1342-1354.
Evensen, G., and P. J. van Leeuwen, 1996: Assimilation of Geosat altimeter data
for the Agulhas current using the ensemble Kalman filter with a quasi~eostrophic model, Mon. Weather Rev., 124, 85--96.
Ezer, T. and GL Mellor, 2000: Sensitivity studies with the North Atlantic sigma
coordinate Princeton Ocean Model. In: Ocean Circulation Model Evalutation
Experiments for the North Atlantic Basin, E.P. Chassignet and P. MalanotteRizzoli (Eds.), Dyn. Atmos. Ocean, 32,185-208.
Ezer, T., 1999: Decadal variabilities ofthe upper layers ofthe subtropical North
Atlantic: An ocean model study. J. Phys. Oceanogr., 29(12), 3111-3124.
Ezer, T., and G. L. Mellor, 1994: Continuous assimilation of Geosat altimeter
data into a three dimensional primitive equation Gulf stream model, J. Phys.
Oceanogr., 24, 832-847.
Ezer, T., and G. L. Mellor, 1997: Simulations ofthe Atlantic Ocean with a free
surface sigma coordinate ocean model. J. Geophys. Res., 102, 15,647-15,657.
Falkowski, P.G. and lA.Raven ,1997: Aquatic photosynthesis. Oxford, Blackwe1l375pp.
Farrell, B. F, 1985: Transient growth of damped baroclinic waves, J. Atmos Sci.,
42,2718-2727.
Farrell, B. F., 1988: Optimal excitation ofneutral Rossby waves, J. Atmos.Sci.,
45,163-172.
Farrell, B. F., 1989: Optimal excitation of baroc1inic waves, J. Atmos.Sci., 46,
1193-1206.
Farrell, B. F., 1990: Small error dynamics and the predictability of atmospheric
flows, J. Atmos. Sci., 47, 2409-2416.
Farrell, B., and A.M.Moore, 1992: An adjoint method for obtaining the most
rapidly growing perturbation to oceanic flows. J. Phys. Ocean., 22(4), 338349.
Fasham, M.J.R., H.W.Ducklow and S.M.McKelvie, 1990: A nitrogen based
model of plankton dynamics in the oceanic mixed layer. J. Mar. Res., 48,
591-639.
Fasham, M.J.R., 1978: The statistical and mathematical analysis of plankton
patchiness. Oceanography and Marine Biology. An Annual Review, 16,4379.
Fasham, M. J. R., 1993: Ecosystem behavior at Bermuda station "S" and ocean
weather station "India": a general circulation model and observational analysis. Global Biogeochemical Cycles, 7(2): 379-415.