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scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

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STP12 Abstracts<br />

Berlin, 12 - 16 July <strong>2010</strong><br />

SCOSTEP Symposium <strong>2010</strong><br />

The 11-years solar cycle in tr<strong>an</strong>sient WACCM-3 simulations<br />

Chiodo Gabriel 1 , García-Herrera Ricardo 1 , Calvo Natalia 2<br />

1 Universidad Complutense de Madrid, 2 National Center for Atmospheric Research<br />

The whole atmospheric response to the 11-years Schwabe cycle was <strong>an</strong>alysed in <strong>an</strong> ensemble<br />

of four WACCM-3.5 simulations covering 45 years (1965-2005, neglecting the initial five<br />

years for model spin-up). These experiments were carried out within the CCMVal-2 initiative<br />

to reproduce the past. The simulations were driven with the following forcings: (1) a timevarying<br />

solar cycle, (2) nudged QBO, (3) observed SSTs, (4) <strong>an</strong>thropogenic carbon <strong>an</strong>d ODS<br />

emissions. All ensemble members show a statistically signific<strong>an</strong>t <strong>an</strong>nual me<strong>an</strong> warming<br />

throughout the middle <strong>an</strong>d upper tropical stratosphere, with a radiatively-driven maximum in<br />

the upper stratosphere, a relative minimum in the middle stratosphere <strong>an</strong>d a secondary<br />

dynamically-driven strong maximum in the tropical lower stratospheric temperature <strong>an</strong>d<br />

ozone response. The nudged QBO <strong>an</strong>d the observed SSTs play <strong>an</strong> import<strong>an</strong>t role in<br />

amplifying the solar signal in the lower stratosphere. Moreover, a downward propagation of<br />

zonal wind <strong>an</strong>omalies from the stratosphere to the troposphere in the extra-tropics is found<br />

during the Northern Hemispheric winter, which appears to be a robust feature of the model<br />

simulations. On the other h<strong>an</strong>d, the QBO modulation of the extra-tropical solar signal in late<br />

NH-winter (i), <strong>an</strong>d the solar-cycle modulation of the Holton-T<strong>an</strong> relationship (ii) are only<br />

evident in two of the four ensemble members, thus indicating that the two-way QBO-solar<br />

cycle dynamical interaction is not signific<strong>an</strong>t. Some features of these results are shown to be<br />

closer to observations th<strong>an</strong> in previous WACCM modeling studies, thus certifying <strong>an</strong><br />

improvement in the modeled whole atmospheric solar response in WACCM-3.5, which is<br />

brought by the implementation of a new GW-source parameterization.

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