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Le comportement des ondes internes de gravite proches du niveau critique de Jones est etudie theoretiquement en vue de l'etude de l'origine possible de la turbulence dans la moyenne atmosphere. On tient compte de l'effet inertiel de la rotation de l'atmosphere et on suppose la constante de coriolis et le cisaillement vertical constant. L'epaisseur des couches de turbulence calculee est comparee pour la stratosphere, mesosphere et thermosphere

Propagation and Breakdown of Internal Inertio-Gravity Waves Near Critical Levels in the Middle Atmosphere