scholarly journals Climatic features of summertime baroclinic wave packets over Eurasia and the associated possible impacts on precipitation in southern China

2019 ◽  
Vol 20 (4) ◽  
pp. e889 ◽  
Author(s):  
Dechao Ye ◽  
Zhaoyong Guan ◽  
Dachao Jin
Keyword(s):  
Southern China ◽  
Wave Packets ◽  
Baroclinic Wave ◽  
Climatic Features

Interaction of North Atlantic baroclinic wave packets and the Mediterranean storm track

2013 ◽  
Vol 140 (680) ◽  
pp. 754-765 ◽  
Author(s):  
F. Ahmadi-Givi ◽  
M. Nasr-Esfahany ◽  
A. R. Mohebalhojeh
Keyword(s):  
North Atlantic ◽  
Wave Packets ◽  
Storm Track ◽  
Baroclinic Wave ◽  
The Mediterranean

Baroclinic Wave Packets in Models and Observations

1993 ◽  
Vol 50 (10) ◽  
pp. 1413-1428 ◽  
Author(s):  
Sukyoung Lee ◽  
Isaac M. Held
Keyword(s):  
Wave Packets ◽  
Baroclinic Wave

scholarly journals Baroclinic wave packets in an extended quasigeostrophic two-layer model

2007 ◽  
Vol 34 (5) ◽  
Author(s):  
Wenchang Yang ◽  
Ji Nie ◽  
Pu Lin ◽  
Benkui Tan
Keyword(s):  
Wave Packets ◽  
Baroclinic Wave ◽  
Layer Model ◽  
Two Layer Model

Baroclinic wave packets described by spatially varying Lorenz equations

1982 ◽  
Vol 87 (5) ◽  
pp. 240-244
Author(s):  
M.E. Alexander ◽  
J. Brindley ◽  
I.M. Moroz
Keyword(s):  
Wave Packets ◽  
Baroclinic Wave ◽  
Lorenz Equations ◽  
Spatially Varying

Aperiodic behaviour of baroclinic wave packets

1981 ◽  
Vol 83 (6) ◽  
pp. 259-262 ◽  
Author(s):  
J. Brindley ◽  
I.M. Moroz
Keyword(s):  
Wave Packets ◽  
Baroclinic Wave

Evolution of baroclinic wave packets in a flow with continuous shear and stratification

1981 ◽  
Vol 377 (1771) ◽  
pp. 379-404 ◽  
Keyword(s):  
Evolution Equations ◽  
Gordon Equation ◽  
Wave Packets ◽  
Baroclinic Instability ◽  
Wave Dispersion ◽  
Baroclinic Wave ◽  
Sine Gordon Equation ◽  
Weakly Nonlinear ◽  
Boundary Slope ◽  
Continuous Shear

Evolution equations are developed for weakly nonlinear baroclinic wave packets in a flow with continuous shear and stratification. When wave dispersion is forced by using sloping upper and lower boundaries it is shown that, for boundary slope equal to isothermal slope in the basic state, these evolution equations are transformable to the sine-Gordon equation. The relation between behaviour in this model and that in the discretelayer models of baroclinic instability is discussed, and finally solutions of the sine-Gordon equation appropriate to a periodic domain are presented and compared with experimental results.

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