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Lidar observations of stratospheric gravity waves from 2011 to 2015 at McMurdo (77.84°S, 166.69°E), Antarctica: 1. Vertical wavelengths, periods, and frequency and vertical wave number spectra
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2017
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Source: Journal of Geophysical Research: Atmospheres, 122(10), 5041-5062
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Journal Title:Journal of Geophysical Research: Atmospheres
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Description:Five years of atmospheric temperature data, collected with an Fe Boltzmann lidar by the University of Colorado group from 2011 to 2015 at Arrival Heights, are used to characterize the vertical wavelengths, periods, vertical phase speeds, frequency spectra, and vertical wave number spectra ofstratospheric gravity waves from 30 to 50 km altitudes. Over 1000 dominant gravity wave events are identi fied from the data. The seasonal spectral distributions of vertical wavelengths, periods, and vertical phase speeds in summer, winter, and spring/fall are found obeying a lognormal distribution. Both thedownward and upward phase progression gravity waves are observed by the lidar, and the fractions of gravity waves with downward phase progression increase from summer ~59% to winter ~70%. The seasonal and monthly mean vertical wavelengths and periods exhibit clear seasonal cycles with vertical wavelengthgrowing from summer ~5.5 km to winter ~8.5 km, and period increasing from summer ~4.5 h to winter ~6 h.
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Source:Journal of Geophysical Research: Atmospheres, 122(10), 5041-5062
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ISSN:2169-897X;2169-8996;
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Rights Information:Other
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