The origin of nonlinear signatures of planetary wave dynamics: Mean phase space tendencies and contributions from non-Gaussianity

被引:31
作者
Franzke, Christian
Majda, Andrew J.
Branstator, Grant
机构
[1] NYU, Ctr Atmospher Ocean Sci, Courant Inst Math Sci, New York, NY USA
[2] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
关键词
D O I
10.1175/2006JAS2221.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Mean phase space tendencies are investigated to systematically identify the origin of nonlinear signatures and the dynamical significance of small deviations from Gaussianity of planetary low-frequency waves. A general framework for the systematic investigation of mean phase space tendencies in complex geophysical systems is derived. In the special case of purely Gaussian statistics, this theory predicts that the interactions among the planetary waves themselves are the source of the nonlinear signatures in phase space, whereas the unresolved waves contribute only an amplitude-independent forcing, and cannot contribute to any nonlinear signature. The predictions of the general framework are studied for a simple stochastic climate model. This toy model has statistics that are very close to being Gaussian and a strong nonlinear signature in the form of a double swirl in the mean phase space tendencies of its low-frequency variables, much like recently identified signatures of nonlinear planetary wave dynamics in prototype and comprehensive atmospheric general circulation models (GCMs). As predicted by the general framework for the Gaussian case, the double swirl results from nonlinear interactions of the low-frequency variables. Mean phase space tendencies in a reduced space of a prototype atmospheric GCM are also investigated. Analysis of the dynamics producing nonlinear signatures in these mean tendencies shows a complex interplay between waves resolved in the subspace and unresolved waves. The interactions among the resolved planetary waves themselves do not produce the nonlinear signature. It is the interaction with the unresolved waves that is responsible for the nonlinear dynamics. Comparing this result with the predictions of the general framework for the Gaussian case shows that the impact of the unresolved waves is due to their small deviations from Gaussianity. This suggests that the observed deviations from Gaussianity, even though small, are dynamically relevant.
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收藏
页码:3987 / 4003
页数:17
相关论文
共 79 条
[1]   Linking nonlinearity and non-Gaussianity of planetary wave behavior by the Fokker-Planck equation [J].
Berner, J .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2005, 62 (07) :2098-2117
[2]  
BERNER J, 2003, THESIS METEOROLOGICA
[3]   Linear and Nonlinear signatures in the planetary wave dynamics of an AGM probability density functions [J].
Berner, Judith ;
Branstator, Grant .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2007, 64 (01) :117-136
[4]   Linear and nonlinear signatures in the planetary wave dynamics of an AGCM: Phase space tendencies [J].
Branstator, G ;
Berner, J .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2005, 62 (06) :1792-1811
[5]  
BRANSTATOR G, 1990, J ATMOS SCI, V47, P629, DOI 10.1175/1520-0469(1990)047<0629:LFPIBS>2.0.CO
[6]  
2
[7]   The seasonal cycle of interannual variability and the dynamical imprint of the seasonally varying mean state [J].
Branstator, G ;
Frederiksen, J .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2003, 60 (13) :1577-1592
[8]  
Branstator G, 1998, J CLIMATE, V11, P2645, DOI 10.1175/1520-0442(1998)011<2645:AEMOBA>2.0.CO
[9]  
2
[10]   NONLINEAR STABILITY AND STATISTICAL-MECHANICS OF FLOW OVER TOPOGRAPHY [J].
CARNEVALE, GF ;
FREDERIKSEN, JS .
JOURNAL OF FLUID MECHANICS, 1987, 175 :157-181