441
the numerical model is explained by low-order vacillations. This applies
strictly to the barotropic components, the tests for baroclinic components
are overshadowed by the necessity to parameterize the momentum and
vorticity transports due to transient eddies by an extremely simplified representation in terms of a linear interfacial friction law in the low-order
image.
Bendat, J.S., and A.G. Piersol (1986): Random Data. Analysis and measurement procedures, 2nd ed. John Wiley and sons, New York
Benzi, R., Saltzman, B., and A. Wijn-Nielsen (1986): Anomalous atmospheric flows and blocking. Advances in Geophysics Bd. 29, Academic
Press, Orlando
Charney, J.G., and A. Eliassen (1949): A numerical method for predicting
the perturbations of the middle latitude westerlies. Tellus 1: 38 - 54
Charney, J.G., and J.G. DeVore (1979): Multiple flow equilibra in the
atmosphere and blocking. Journal of the Atmospheric Sciences 36:
1205 - 1216
Charney, J.G., and D.M. Straus (1980): Form drag instability, multiple
equilibra, and propagating planetary waves in baroclinic, orographically forced, planetary wave systems. Journal of the Atmospheric
Sciences 37: 1157 - 1176
Charney, J.G., Shukla, J., and K.C. Mo (1981): Comparison of a
barotropic blocking theory with observation. Journal of the Atmospheric Sciences 38: 762 - 779
De Swart, H.E., and J. Grassman (1987): Effect of stochastic perturbations on a low-order spectral model of the atmospheric circulation.
Tellus 39A: 10-24
Egger, J. (1978): Dynamics of blocking highs. Journal of the Atmospheric
Sciences 35: 1788-1801
Egger, J. (1981): Stochastically driven large-scale circulations with multiple equilibra. Journal of the Atmospheric Sciences 38: 2606 - 2618
The FRAM-Group (1991): An eddy-resolving model of the southern
ocean. EGS, Transactions of the American Geophysical Union 72:
169 - 175
the numerical model is explained by low-order vacillations. This applies
strictly to the barotropic components, the tests for baroclinic components
are overshadowed by the necessity to parameterize the momentum and
vorticity transports due to transient eddies by an extremely simplified representation in terms of a linear interfacial friction law in the low-order
image.
Bendat, J.S., and A.G. Piersol (1986): Random Data. Analysis and measurement procedures, 2nd ed. John Wiley and sons, New York
Benzi, R., Saltzman, B., and A. Wijn-Nielsen (1986): Anomalous atmospheric flows and blocking. Advances in Geophysics Bd. 29, Academic
Press, Orlando
Charney, J.G., and A. Eliassen (1949): A numerical method for predicting
the perturbations of the middle latitude westerlies. Tellus 1: 38 - 54
Charney, J.G., and J.G. DeVore (1979): Multiple flow equilibra in the
atmosphere and blocking. Journal of the Atmospheric Sciences 36:
1205 - 1216
Charney, J.G., and D.M. Straus (1980): Form drag instability, multiple
equilibra, and propagating planetary waves in baroclinic, orographically forced, planetary wave systems. Journal of the Atmospheric
Sciences 37: 1157 - 1176
Charney, J.G., Shukla, J., and K.C. Mo (1981): Comparison of a
barotropic blocking theory with observation. Journal of the Atmospheric Sciences 38: 762 - 779
De Swart, H.E., and J. Grassman (1987): Effect of stochastic perturbations on a low-order spectral model of the atmospheric circulation.
Tellus 39A: 10-24
Egger, J. (1978): Dynamics of blocking highs. Journal of the Atmospheric
Sciences 35: 1788-1801
Egger, J. (1981): Stochastically driven large-scale circulations with multiple equilibra. Journal of the Atmospheric Sciences 38: 2606 - 2618
The FRAM-Group (1991): An eddy-resolving model of the southern
ocean. EGS, Transactions of the American Geophysical Union 72:
169 - 175