HR: 0800h
AN: SA41A-1054    [Abstracts]
TI: Coordinated Ground and Space Based Observations of the Quasi Two-Day Wave in January 2004
AU: * Palo, S E
EM: Scott.Palo@colorado.edu
AF: University of Colorado, Department of Aerospace Engineering Sciences, Boulder, CO 80309
AU: Zhang, X
EM: Xiaoli.Zhang@colorado.edu
AF: University of Colorado, Department of Aerospace Engineering Sciences, Boulder, CO 80309
AU: Forbes, J M
EM: Jeffrey.Forbes@colorado.edu
AF: University of Colorado, Department of Aerospace Engineering Sciences, Boulder, CO 80309
AU: Russell, J
EM: James.Russell@hampton.edu
AF: Hampton University, Center for Atmospheric Sciences, Hampton, VA 23668
AU: Mlynczak, M
EM: M.G.Mlynczak@nasa.gov
AF: NASA Langley Research Center, Atmospheric Sciences Division 21 Langley Blvd., Hampton, VA 23681
AU: Mertens, C
EM: c.j.mertens@larc.nasa.gov
AF: NASA Langley Research Center, Atmospheric Sciences Division 21 Langley Blvd., Hampton, VA 23681
AU: Killeen, T
EM: killeen@ucar.edu
AF: National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307
AU: Solomon, S
EM: stans@ucar.edu
AF: National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307
AU: Wu, Q
EM: qwu@ucar.edu
AF: National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307
AU: Vincent, R
EM: Robert.Vincent@adelaide.edu.au
AF: University of Adelaide, Department of Physics, Adelaide, 5005 Australia
AU: Murphy, D
EM: Damian.Murphy@aad.gov.au
AF: Australian Antarctic Division, Channel Highway, Kingston, 7050 Australia
AU: Riggin, D
EM: Riggin@cora.nwra.com
AF: Colorado Research Associates, 3380 Mitchell Ln., Boulder, CO 80301
AU: Nakamura, T
EM: Nakamura@kurasc.kyoto-u.ac.jp
AF: Kyoto University, Research Institute for Sustainable Humanosphere, Uji, 611-0011 Japan
AU: Tsuda, T
EM: Tsuda@kurasc.kyoto-u.ac.jp
AF: Kyoto University, Research Institute for Sustainable Humanosphere, Uji, 611-0011 Japan
AB: The quasi two-day wave is a predominant feature of the mesosphere and lower thermosphere during January and early February each year with horizontal wind speeds exceeding 50 m/s and temperature perturbations on the order of 14K. Theoretical and modeling results indicate the quasi two-day wave is initiated through a baroclinic instability of the summer westward mesospheric jet. The global quasi two-day wave response is repeatable from year to year and is the result of the 3,0 Rossby normal mode being forced by the instability. Observations from the TIMED spacecraft in January 2004 have provided the first opportunity to study the global structure and evolution of the quasi two-day with measurements of both the temperature and horizontal wind field. These measurements from the mesosphere into the lower-thermosphere are provided from the SABER and TIDI instruments on TIMED. These observations will be combined with observations from the global network of ground-based meteor and medium frequency radars to provide a comprehensive view of the quasi two-day wave observed during January 2004.
DE: 3332 Mesospheric dynamics
DE: 3334 Middle atmosphere dynamics (0341, 0342)
DE: 3384 Waves and tides
SC: SPA-Aeronomy [SA]
MN: 2004 AGU Fall Meeting