Inertia–Gravity Waves Observed in the Lower Stratosphere over Macquarie Island

By F. Guest, M. Reeder, C. J. Marks, D. Karoly. 2000

170 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/02a4f1d2084d8577fcd63825966495d38ba64708

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Citations in the corpus

Inertia gravity wave generation by the tropospheric midlatitude jet as given by the Fronts and Atlantic Storm‐Track Experiment radio soundings (2003, methodology): “[34] Further information may be obtained from the above analysis by identifying the particular configurations of the flow corresponding to the radio soundings with highest values of A [cf. Guest et al., 2000].”
Inertia–Gravity Waves Spontaneously Generated by Jets and Fronts. Part I: Different Baroclinic Life Cycles (2007, background): “The first is studies based on observations, which have often emphasized the jet exit region upstream of a ridge as a key region of intense gravity wave activity (Uccellini and Koch 1987; Guest et al. 2000; Pavelin et al. 2001).”
An overview of the past, present and future of gravity‐wave drag parametrization for numerical climate and weather prediction models (2003, methodology): “In the absence of ducting by an unstable critical layer, these waves should propagate into the middle atmosphere, as has been verified by observation (Guest et al., 2000; Pavelin et al., 2001) and 3D modelling studies (Luo and Fritts, 1993; O’Sullivan and Dunkerton, 1995).”
Global Gravity Wave Variances from Aura MLS: Characteristics and Interpretation (2008, background): “Broader vortex enhancements are also seen in regions well away from significant mountains, which may result in part from GWs radiated from imbalances within baroclinic jet/front systems at these latitudes (e.g., Guest et al. 2000; see section 5).”
Numerical Modeling of Gravity Wave Generation by Deep Tropical Convection (2001, background): “Such nonorographic sources include midlatitude frontal systems (e.g., Reeder and Griffiths 1996), upper-level jets (e.g., Guest et al. 2000), and dry boundary layer convection (e.g., Clark et al. 1986; Kuettner et al. 1987; Hauf and Clark 1989).”
Balance and Spontaneous Wave Generation in Geophysical Flows (2013, result): “Numerical results such as these are in qualitative agreement with observations of IGWs thought to be generated spontaneously (e.g. Guest et al. 2000).”