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• W2950441567 endingPage "7718" @default.
• W2950441567 startingPage "7687" @default.
• W2950441567 abstract "We investigate the effects on the mesosphere and thermosphere from a strong mountain wave (MW) event over the wintertime Southern Andes using a gravity wave (GW)-resolving global circulation model. During this event, MWs break and attenuate at z∼50–80 km, thereby creating local body forces that generate large-scale secondary GWs having concentric ring structure with horizontal wavelengths λH=500–2,000 km, horizontal phase speeds cH=70–100 m/s, and periods τr∼3–10 hr. These secondary GWs dissipate in the upper mesosphere and thermosphere, thereby creating local body forces. These forces have horizontal sizes of 180–800 km, depending on the constructive/destructive interference between wave packets and the overall sizes of the wave packets. The largest body force is at z=80–130 km, has an amplitude of ∼2,400 m/s/day, and is located ∼1,000 km east of the Southern Andes. This force excites medium- and large-scale “tertiary GWs” having concentric ring structure, with λH increasing with radius from the centers of the rings. Near the Southern Andes, these tertiary GWs have cH=120–160 m/s, λH=350–2,000 km, and τr∼4–9 hr. Some of the larger-λH tertiary GWs propagate to the west coast of Africa with very large phase speeds of cH≃420 m/s. The GW potential energy density increases exponentially at z∼95–115 km, decreases at z∼115–125 km where most of the secondary GWs dissipate, and increases again at z>125 km from the tertiary GWs. Thus, strong MW events result in the generation of medium- to large-scale fast tertiary GWs in the mesosphere and thermosphere via this multistep vertical coupling mechanism." @default.
• W2950441567 created "2019-06-27" @default.
• W2950441567 creator A5043042883 @default.
• W2950441567 creator A5087078104 @default.
• W2950441567 date "2019-09-01" @default.
• W2950441567 modified "2023-10-16" @default.
• W2950441567 title "Numerical Modeling of the Generation of Tertiary Gravity Waves in the Mesosphere and Thermosphere During Strong Mountain Wave Events Over the Southern Andes" @default.
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• W2950441567 doi "https://doi.org/10.1029/2019ja026694" @default.
• W2950441567 hasPublicationYear "2019" @default.
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