A statistical study of gravity waves in the polar regions based on operational radiosonde data
By M. Yoshiki, Kaoru Sato. 2000
144 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/7e7d92e79e3d566ca2c6f6b0c25361630d96d822
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Citations in the corpus
- Global Gravity Wave Variances from Aura MLS: Characteristics and Interpretation (2008, methodology): “Above 20–25 km, the peak GW variances in these studies tend to occur in midwinter (Yoshiki and Sato 2000; Baumgaertner and McDonald 2007), also in agreement with the MLS GW variances in Fig.”
- Gravity Wave Characteristics in the Southern Hemisphere Revealed by a High-Resolution Middle-Atmosphere General Circulation Model (2012, methodology): “By analyzing vertical energy propagation of gravity waves observed by operational and campaign observations using radiosondes, Yoshiki and Sato (2000), Yoshiki et al. (2004), and Sato and Yoshiki (2008) suggested that gravity wave sources are present in the stratosphere in the polar region and that…”
- Estimation of Gravity Wave Momentum Flux and Phase Speeds from Quasi-Lagrangian Stratospheric Balloon Flights. Part II: Results from the Vorcore Campaign in Antarctica (2008, methodology): “Based on the results obtained by Allen and Vincent (1995) and Yoshiki and Sato (2000) in the lower stratosphere, we made the assumption that the observed waves were propagating upward so that this flux is always a positive quantity.”
- Evaluation of Polar MM5 Simulations of Antarctic Atmospheric Circulation (2003, background): “The spatial distribution of the surface pressure biases suggests that gravity waves generated around the steep coastal slopes and in the stratosphere play an important role in the redistribution of momentum in Antarctica (Yoshiki and Sato 2000).”
- General aspects of a T213L256 middle atmosphere general circulation model (2008, background): “The existence of gravity waves propagating energy downward in the stratosphere was also later confirmed by radiosonde observations [Yoshiki and Sato, 2000; Sato, 2000; Yoshiki et al., 2004; Sato and Yoshiki, 2008].”
- Gravity Wave Generation around the Polar Vortex in the Stratosphere Revealed by 3-Hourly Radiosonde Observations at Syowa Station (2008, methodology): “According to the climatological study for the Antarctic by Yoshiki and Sato (2000), it appears that the seasonal variation of gravity wave activity is related to the polar vortex evolution: the maximum of gravity wave energy is observed in spring when the polar vortex breaking occurs.”