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92<br />
The absence of the very shallow, near surface negative KF<br />
theta change when using the altered KF scheme is due to the<br />
severe reduction in precipitation produced by the KF<br />
scheme. The downdraft model uses a fraction of the<br />
precipitation to generate an evaporatively cooled downdraft<br />
that detrains in the lowest model layer. In the altered<br />
version of the KF scheme, precipitation is nearly absent and<br />
the water vapor is partitioned into cloud material so that the<br />
downdraft model produces very little cooling.<br />
Skamarock, W. C., J. B. Klemp, and J. Dudhia, Prototypes<br />
for the WRF (Weather Research and Forecasting)<br />
model, Preprints, Ninth Conf. on Mesoscale Processes,<br />
Fort Lauderdale, FL, Amer. Meteor. Soc., J11—J15,<br />
2001.<br />
4. Summary<br />
An altered version of the KF scheme in which water vapor<br />
flux is converted into cloud material rather than precipitation<br />
is examined. The results from simulations of a two-month<br />
period in which large propagating MCSs were frequent<br />
showed dramatic differences in diabatic heating profiles.<br />
At the workshop, additional results will be discussed that<br />
show just as dramatic differences in precipitation<br />
characteristics. In particular, the phase of the diurnal cycle<br />
of precipitation is significantly delayed and more accurate in<br />
when using the altered KF scheme, and with this modified<br />
scheme the eastward, nocturnal propagation of precipitation<br />
is more pronounced. The sensitivity to microphysics<br />
parameterization and grid point spacing will be discussed as<br />
well.<br />
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