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  List of Accepted Contributions - AS1.08 The quasi-biennial oscillation and its role in the cllimate system (co-listed in CL)

Please, click Abstract Number to find the corresponding abstract as PDF file; if necessary, download Adobe Acrobat Reader 4.0 first to open the file. Any abstract may be freely reproduced for non-commercial, scientific purposes; however, the moral right of the author(s) to be identified as the author(s) of such abstracts is asserted.

EGU06-A-01223
Calvo, N.; Giorgetta, M.A.
QBO influence on the boreal winter vortex in MAECHAM5 GCM

EGU06-A-01370
Sitnov, S.
The QBO effects in solar maximum and in solar minimum conditions over Europe. (withdrawn)

EGU06-A-01417
Sitnov, S.
The extratropical QBO effects in total ozone: dependence on solar cycle and season. (withdrawn)

EGU06-A-01484
Shibata, K.; Deushi, M.
Ozone Radiative Effects on the Quasi-Biennial Oscillation in the Equatorial Stratosphere

EGU06-A-02442
Matthes, K.
Modeling the influence of the 11-year solar cycle and the QBO on the atmosphere (withdrawn)

EGU06-A-03023
Kuttippurath, J; Lott, F
Tropical waves in the LMDz stratospheric model and in the ERA40 reanalysis

EGU06-A-03141
Wedi, N.; Smolarkiewicz, P.K.
Direct numerical simulation of the Plumb-McEwan laboratory analogue of the QBO (withdrawn)

EGU06-A-07207
Manzini, E. ; Giorgetta, M. A.
Tropospheric tropical variability and the Quasi Biennial Oscillation

EGU06-A-08403
Pascoe, C L ; Gray, L J
Equatorial Winds and Sudden Stratospheric Warmings

EGU06-A-08679
Peņa-Ortiz, C.; Ribera, P.; Giorgetta, M.; Garcia-Herrera, R.
MTMSVD analysis of the seasonal variation of the QBO signal at low and middle latitudes

EGU06-A-08700
Giorgetta, M. A.; Manzini, E.; Roeckner, E.; Esch, M.; Bengtsson, L.
Climatology and forcing of the quasi-biennial oscillation in the MAECHAM5 model

EGU06-A-08811
Peņa-Ortiz, C.; Ribera, P.; Giorgetta, M.; Gracia-Herrera, R.
QBO modulation of the high latitude circulation in ERA40 and MAECHAM5 simulations

EGU06-A-08882
Gabis, I.P.; Troshichev, O.A.
QBO cycle identified by changes in height profile of the zonal winds: new regularities and relation to variations in the solar UV flux


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