The 4-Day Wave and Transport ofUARSTracers in the Austral Polar Vortex
- 1 December 1998
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 55 (23) , 3456-3470
- https://doi.org/10.1175/1520-0469(1998)055<3456:tdwato>2.0.co;2
Abstract
Upper Atmosphere Research Satellite tracer data and isentropic transport calculations using U.K. Meteorological Office winds initialized with these data show evidence of eastward-traveling waves in the polar upper stratosphere in late austral winter 1992. Microwave Limb Sounder (MLS) H2O from prototype iterative retrievals shows a 4-day wave signal at levels from ∼1.5 to 0.1 hPa; a 4-day wave signal was not obvious in production retrievals of MLS H2O. At 1800 K, the 4-day wave signal in MLS H2O has a double-peaked structure in latitude, which is reproduced in isentropic transport calculations. The time evolution, amplitude, and phase of the 4-day wave in the transport calculations agree well with observations at high latitudes; the position and shape of the polar vortex and of H2O drawn up around the vortex are reproduced by the transport calculations. Spectral analyses of the Cryogen Limb Array Etalon Spectrometer (CLAES) CH4 are dominated by more slowly eastward-moving waves (∼6–10 days), but a... Abstract Upper Atmosphere Research Satellite tracer data and isentropic transport calculations using U.K. Meteorological Office winds initialized with these data show evidence of eastward-traveling waves in the polar upper stratosphere in late austral winter 1992. Microwave Limb Sounder (MLS) H2O from prototype iterative retrievals shows a 4-day wave signal at levels from ∼1.5 to 0.1 hPa; a 4-day wave signal was not obvious in production retrievals of MLS H2O. At 1800 K, the 4-day wave signal in MLS H2O has a double-peaked structure in latitude, which is reproduced in isentropic transport calculations. The time evolution, amplitude, and phase of the 4-day wave in the transport calculations agree well with observations at high latitudes; the position and shape of the polar vortex and of H2O drawn up around the vortex are reproduced by the transport calculations. Spectral analyses of the Cryogen Limb Array Etalon Spectrometer (CLAES) CH4 are dominated by more slowly eastward-moving waves (∼6–10 days), but a...Keywords
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