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Plougonven, Riwal - Laboratoire de Meteorologie Dynamique, Ecole Normale Supérieure
Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 136: 13711377, July 2010 Part A Notes and Correspondence
J. Fluid Mech. (2009), vol. 638, pp. 2747. c Cambridge University Press 2009 doi:10.1017/S0022112009990796
Observations and simulations of a large-amplitude mountain wave breaking over the Antarctic Peninsula
Gravity waves excited by jets: Propagation versus generation R. Plougonven
CORRIGENDUM RIWAL PLOUGONVEN
2692 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
Inertia gravity wave generation by the tropospheric midlatitude jet as given by the
Physics Letters A 314 (2003) 140149 www.elsevier.com/locate/pla
J. Fluid Mech. (2003), vol. 481, pp. 269290. c 2003 Cambridge University Press DOI: 10.1017/S0022112003003896 Printed in the United Kingdom
18 me Congrs Franais de Mcanique Grenoble, 27-31 aot 2007 Ageostrophic instabilities of a front in a stratified rotating fluid
Inertia -gravity wave generation by the tropospheric mid-latitude jet as given by the FASTEX radiosoundings
Universite Pierre et Marie Curie Paris 6 Ecole doctorale 129 Sciences de l'Environnement
Licence-Master Sciences de la plan`ete Terre Licence (L3)
Licence-Master Sciences de la plan`ete Terre Licence (L3)
Licence-Master Sciences de la plan`ete Terre Licence (L3)
Licence-Master Sciences de la plan`ete Terre Licence (L3)
Licence-Master Sciences de la plan`ete Terre Licence (L3)
Licence-Master Sciences de la plan`ete Terre Licence (L3)
On the spontaneous generation of gravity waves by vortical motions
InertiaGravity Waves Spontaneously Generated by Jets and Fronts. Part I: Different Baroclinic Life Cycles
Internal gravity wave emission from a pancake vortex: An example of wavevortex interaction in strongly stratified flows
SPECIALITE OCEAN-ATMOSPHERE-CLIMAT-TELEDETECTION Universit Pierre et Marie Curie/ Ecole Polytechnique
Announcement: Session AS1.06 on
Nonlinear development of inertial instability in a barotropic shear Riwal Plougonven1,a
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2 1.4
Comparison of a large-scale inertia-gravity wave as seen in the ECMWF analyses and from radiosondes
J. Fluid Mech. (2009), vol. 627, pp. 485507. c 2009 Cambridge University Press doi:10.1017/S0022112009006508 Printed in the United Kingdom
Quasigeostrophic Dynamics of a Finite-Thickness Tropopause R. PLOUGONVEN
