Farrell, Brian F. - School of Engineering and Applied Sciences, Harvard University

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Farrell, Brian F. - School of Engineering and Applied Sciences, Harvard University

1 SEPTEMBER 2003 2101F A R R E L L A N D I O A N N O U 2003 American Meteorological Society
The Stochastic Parametric Mechanism for Growth of Wind-Driven Surface Water Waves
P1: FYX/FGC P2: FXS 0521848822c08.xml CUUK341B-Palmer February 14, 2006 9:36
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 134: 16271633 (2008)
1 SEPTEMBER 2003 2083H E I F E T Z A N D F A R R E L L 2003 American Meteorological Society
Gravity Waves in a Horizontal Shear Flow. Part I: Growth Mechanisms in the Absence of Potential Vorticity Perturbations
Pliocene equatorial temperature: Lessons from atmospheric superrotation
Momentum and Energy Transport by Gravity Waves in Stochastically Driven Stratified Flows. Part II: Radiation of Gravity Waves from a Gaussian Jet
Distributed Forcing of Forecast and Assimilation Error Systems BRIAN F. FARRELL
Roll/streak dynamics in turbulent shear flow Brian F. Farrell1, a)
The Role of Nonnormality in Overreflection Theory NIKOLAOS A. BAKAS AND BRIAN F. FARRELL
The role of non-normality in overreflection Nikolaos A. Bakas
A stochastic structural stability theory model of the drift wavezonal flow system
Emergence of Jets from Turbulence in the Shallow-Water Equations on an Equatorial Beta Plane
Structure and Spacing of Jets in Barotropic Turbulence BRIAN F. FARRELL
Generalized Stability of Nongeostrophic Baroclinic Shear Flow. Part II: Intermediate Richardson Number Regime
P1: FYX/FGC P2: FXS 0521848822c05.xml CUUK341B-Palmer February 14, 2006 9:11
Formation of Jets by Baroclinic Turbulence BRIAN F. FARRELL
2644 VOLUME 61J O U R N A L O F T H E A T M O S P H E R I C S C I E N C E S 2004 American Meteorological Society
Nonnormal Frontal Dynamics YIZHAK FELIKS
Gravity Waves in a Horizontal Shear Flow. Part II: Interaction between Gravity Waves and Potential Vorticity Perturbations
METEOROLOGICAL Journal of the Atmospheric Sciences
Abrupt Transition to Strong Superrotation Driven by Equatorial Wave Resonance in an Idealized GCM