EUCLIPSE First Period Report
EUCLIPSE First Period Report
EUCLIPSE First Period Report
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Figure. 23. Zonal mean temperature assimilation increments in April 2011, for a control and<br />
an experiment with reduced entrainment rate in the parameterization of deep convection<br />
(top). On the bottom the difference in temperature assimilation increments between the two<br />
experiments is shown (left) and the mean difference in temperature tendencies accumulated<br />
over the first six forecast hours due convection, explaining most of the model differences.<br />
References<br />
Rodwell, M. J., and T. N. Palmer, 2007: Using numerical weather prediction to assess<br />
climate models. Quart. J. Roy. Meteor. Soc., 133, 129-146.<br />
Phillips, T. J. , G. L. Potter, D. L. Williamson, R. T. Cederwall, J. S. Boyle, M.<br />
Fiorino, J. J. Hnilo, J. G. Olson, S. Xie, and J. John Yio, 2004: Evaluating<br />
parameterizations in General Circulation Models: Climate simulation meets weather<br />
prediction. Bull. Am. Met. Soc., 85, 1903-1915.<br />
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