Stratospheric Mountain Waves over the South Andes: Observations and Application of Linear Theory.
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| Title: | Stratospheric Mountain Waves over the South Andes: Observations and Application of Linear Theory. |
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| Authors: | Valentini, Thomas1 (AUTHOR) valentini.t@unimelb.edu.au, Kitsios, Vassili2,3 (AUTHOR), Klewicki, Joseph1 (AUTHOR), Philip, Jimmy1 (AUTHOR) |
| Source: | Journal of the Atmospheric Sciences. Feb2026, Vol. 83 Issue 2, p265-280. 16p. |
| Subjects: | Gravity waves, Coriolis force, Theory of wave motion, Differential equations |
| Geographic Terms: | Andes |
| Abstract: | The South Andes Mountain range is a global hotspot for stratospheric gravity waves. Here, we identify two selected case study flows over the South Andes, using data from the fifth generation ECMWF atmospheric reanalysis (ERA5) reanalysis, one featuring extensive vertical and downstream wave propagation with a characteristic cellular pattern and the other with little to no wave propagation. Core features of these two flow fields are identified and shown to correspond to different analytical solutions to the linear Taylor–Goldstein equation: one with vertical wave propagation (with and without rotation) and one with trapped waves propagating downstream. The importance of rotation is emphasized for its ability to suppress mountain waves at low altitudes, and wave trapping is identified as potentially contributing to the downstream propagation of waves in the stratosphere for one of the flow snapshots. The dimensionless number γ, the ratio of the height scale of the Scorer parameter and the mountain's horizontal length scale, is highlighted as playing a critical role in the behavior of trapped waves in multiple analytical models. [ABSTRACT FROM AUTHOR] |
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| Database: | Engineering Source |
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| Abstract: | The South Andes Mountain range is a global hotspot for stratospheric gravity waves. Here, we identify two selected case study flows over the South Andes, using data from the fifth generation ECMWF atmospheric reanalysis (ERA5) reanalysis, one featuring extensive vertical and downstream wave propagation with a characteristic cellular pattern and the other with little to no wave propagation. Core features of these two flow fields are identified and shown to correspond to different analytical solutions to the linear Taylor–Goldstein equation: one with vertical wave propagation (with and without rotation) and one with trapped waves propagating downstream. The importance of rotation is emphasized for its ability to suppress mountain waves at low altitudes, and wave trapping is identified as potentially contributing to the downstream propagation of waves in the stratosphere for one of the flow snapshots. The dimensionless number γ, the ratio of the height scale of the Scorer parameter and the mountain's horizontal length scale, is highlighted as playing a critical role in the behavior of trapped waves in multiple analytical models. [ABSTRACT FROM AUTHOR] |
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| ISSN: | 00224928 |
| DOI: | 10.1175/JAS-D-25-0046.1 |
