Home > Publications database > Dynamical Coupling between Hurricane Matthew and the Middle to Upper Atmosphere via Gravity Waves |
Journal Article | FZJ-2019-02709 |
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2019
Wiley
Hoboken, NJ
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Please use a persistent id in citations: http://hdl.handle.net/2128/22347 doi:10.1029/2018JA026453
Abstract: During 30 September to 9 October 2016, Hurricane Matthew traversed the Caribbean Sea to the east coast of the United States. During its period of greatest intensity, in the central Caribbean, Matthew excited a large number of concentric gravity waves (GWs, or CGWs). In this paper, we report on hurricane‐generated CGWs observed in both the stratosphere and mesosphere from space‐borne satellites and in the ionosphere by ground Global Positioning System (GPS) receivers. We found CGWs with horizontal wavelengths of ~200–300 km in the stratosphere (height of ~30–40 km) and in the airglow layer of the mesopause (height of ~85–90 km), and we found concentric traveling ionospheric disturbances (TIDs, or CTIDs) with horizontal wavelengths of ~250–350 km in the ionosphere (height of ~100–400 km). The observed TIDs lasted for more than several hours on 1, 2 and 7 October 2016. We also briefly discuss the vertical and horizontal propagation of the Hurricane Matthew‐induced GWs and TIDs. This study shows that Hurricane Matthew induced significant dynamical coupling between the troposphere and the entire middle and upper atmosphere via GWs. It is the first comprehensive satellite analysis of gravity wave propagation generated by hurricane event from the troposphere through the stratosphere and mesosphere into the ionosphere.
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