Latitudinal and longitudinal variability of mesospheric winds and temperatures during stratospheric warming events
By P. Hoffmann, W. Singer, D. Keuer, W. Hocking, Markus Kunze, Y. Murayama. 2007
193 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/db2ef86d1f921d22c50ff6dbaceab9ee9c8dbefb
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In Astronomy and Astrophysics
In Atmospheric Science
- Jorge L. Chau
- Han-Li Liu
- L. P. Goncharenko
- B. Fejer
- M. Ern
- M. Mlynczak
- J. Russell
- Stephen D. Eckermann
Citations in the corpus
- Ionospheric signatures of sudden stratospheric warming: Ion temperature at middle latitude (2008, background): “Cooling in the mesosphere reportedly precedes warming in the stratosphere and is also associated with large dynamical changes in the mesosphere, which include zonal wind reversal, increase in planetary wave activity and changes in the gravity wave activity [i.e., Hoffmann et al., 2007].”
- Implications for atmospheric dynamics derived from global observations of gravity wave momentum flux in stratosphere and mesosphere (2011, background): “This effect can also be seen in the northern hemisphere, however during winter in the northern hemisphere GW squared amplitudes and momentum fluxes are more dominated by enhancements that are likely connected with major stratospheric warmings [see also Hoffmann et al., 2007; Manney et al., 2008].”
- Case studies of the mesospheric response to recent minor, major, and extended stratospheric warmings (2010, background): “consistent with results fromHoffman et al. [2007], who found enhanced turbulent energy dissipation rates from their radar data during this period of intensified westerly winds.”
- Equatorial and Low Latitude Ionospheric Effects During Sudden Stratospheric Warming Events (2011, background): “While several studies reveal that mesospheric changes occur prior to SSW events (Azeem et al. 2005; Hoffmann et al. 2007), maximum ionospheric disturbances are reported within several days after the peak in SSW (e.g., Anderson and Araujo-Pradere 2010; Chau et al. 2009, 2010; Goncharenko et al.…”