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• W2018485931 abstract "[1] In November 2001, the Equatorial Atmosphere Radar (0.20°S, 100.32°E) observed a continuous strong eastward wind shear (10–50 m s−1 km−1), westward wind (2–27 m s−1), and the radar echo layer tilted downward to the west in the region 0–1 km above the tropopause. During the same period, the Richardson number calculated with hourly-averaged horizontal wind and radiosonde temperature data was almost continuously <0.5 and sometimes <0.25, which seems to indicate that the Kelvin-Helmholtz instability (KHI) frequently occurs in that region. The existence of the tilted radar echo layer can be explained by KHI billows. A spurious updraft caused by the KHI-induced tilted echo layer and by the strong westward wind was also observed in the region." @default.
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• W2018485931 date "2003-01-01" @default.
• W2018485931 modified "2023-10-18" @default.
• W2018485931 title "Kelvin-Helmholtz instability around the tropical tropopause observed with the Equatorial Atmosphere Radar" @default.
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• W2018485931 doi "https://doi.org/10.1029/2002gl016685" @default.
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