Internal gravity waves from atmospheric jets and fronts

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Internal wave coupling processes in Earth's atmosphere (2014, neutral): “ilities, but assumes that amplitudes of thus generated waves can be predicted within the linear theory. An excellent and insightful review of these theoretical developments has recently been given by Plougonven and Zhang (2014). 4.2. Numerical Modeling Techniques Numerical modeling allows for studyi”
GRACILE: a comprehensive climatology of atmospheric gravity wave parameters based on satellite limb soundings (2017, methodology): “The resulting altitude profiles of temperature residuals are analyzed with a two-step method introduced by Preusse et al. (2002). First, the whole altitude profile is analyzed by the maximum entropy method (MEM; Press et al.”
Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “, Blumen, 1972; Fritts and Luo, 1992; Fritts and Alexander, 2003], atmospheric jets and fronts [e.g., Mastrantonio et al., 1976; Chimonas and Grant, 1984; Plougonven and Zhang, 2014], or the spontaneous loss of balanced motions [e.”