Abstract
Mechanisms of internal gravity wave generation have been intensively studied because of the role of gravity waves in the large-scale atmospheric circulation. One source of gravity waves that is poorly understood is spontaneous wave generation by the low frequency mesoscale and large scale motions in the atmosphere. In this work, we study the interaction among potential vorticity perturbations and gravity waves in a stably stratified, horizontally sheared zonal flow, with the goal of clarifying the role of these interactions in the process of spontaneous wave generation. We find that vorticity perturbations amplify in energy due to downgradient Reynolds stress when their phase lines tilt towards the west with increasing latitude for a northward increasing shear flow. For a Froude number of order one, there is strong coupling between the vorticity perturbations and the gravity wave manifold. As a result, the large growth attained by vorticity perturbations is transferred to propagating gravity waves. When the flow geometry permits wave propagation, significant gravity wave emission occurs.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Bakas NA, Farrell BF (2009a) Gravity waves in a barotropic shear flow. Part I: growth mechanisms in the absence of potential vorticity perturbations. J Phys Oceanogr 39:481–496. doi:10.1175/2008JPO3836.1
Bakas NA, Farrell BF (2009b) Gravity waves in a barotropic shear flow. Part II: interaction between gravity waves and potential vorticity perturbations. J Phys Oceanogr 39:497–511. doi:10.1175/2008JPO3836.1
Farrell BF, Ioannou PJ (1996) Generalized stability theory. Part I: autonomous operators. J Atmos Sci 53:2025–2040. doi:10.1175/1520-0469(1996) 053<2025:GSTPIA>2.0.CO;2
Ford R, McIntyre ME, Norton WA (2000) Balance and the slow quasi-manifold: some explicit results. J Atmos Sci 57:1236–1254. doi:10.1175/15200469(2000) 057<1236:BATSQS>2.0. CO;2
Hakim V (1998) Asymptotic techniques in nonlinear problems: some illustrative examples. In: Godreche C, Manneville P (eds) Hydrodynamics and nonlinear instabilities. Cambridge University Press, Cambridge, pp 295–386
Kalashnik MV, Mamatsashvili GR, Chagelishvili GD, Lominadze JG (2006) Linear dynamics of non-symmetric perturbations in geostrophic horizontal shear flows. Q J R Meteor Soc 132:505–518. doi:10.1256/qj.04.105
O’Sullivan D, Dunkerton TJ (1995) Generation of inertia-gravity waves in a simulated life cycle of baroclinic instability. J Atmos Sci 52:3695–3716. doi:10.1175/1520-0469(1995) 052<3695: GOIWIA>2.0.CO;2
Olver FWJ (1974) Asymptotics and special functions. Academic Press, New York, p 572
Orr WMF (1907) The stability or instability of the steady motions of a perfect liquid and of a viscous liquid. Proc R Irish Acad Ser A 27:9
Plougonven R, Snyder C (2007) Inertia-gravity waves spontaneously generated by jets and fronts. Part I: different baroclinic life cycles. J Atmos Sci 64:2502–2520. doi:10.1175/JAS3953.1
Vanneste J, Yavneh I (2004) Exponentially small inertia-gravity waves and the breakdown of quasigeostrophic balance. J Atmos Sci 61:211–223. doi:10.1175/1520-0469(2004) 061< 0211:ESIWAT>2.0.CO;2
Acknowledgments
This research was supported by the NSF ATM-0736022 grant.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2013 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
Bakas, N.A., Farrell, B.F. (2013). On the Role of Potential Vorticity Perturbations in the Spontaneous Generation of Gravity Waves. In: Helmis, C., Nastos, P. (eds) Advances in Meteorology, Climatology and Atmospheric Physics. Springer Atmospheric Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-29172-2_3
Download citation
DOI: https://doi.org/10.1007/978-3-642-29172-2_3
Published:
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-29171-5
Online ISBN: 978-3-642-29172-2
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)