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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 />

References<br />

Anderson, C. J., and R. W. Arritt, An alternative mass flux<br />

profile in the Kain-Fritsch convective parameterization<br />

and its effect on seasonal precipitation. J. Hydrometeor.,<br />

Vol. 8, No. 5, pp. 1128-1140, 2007.<br />

Anderson, C. J., and R. W. Arritt, Mesoscale convective<br />

complexes and persistent elongated convective systems<br />

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2003.<br />

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2004.<br />

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II reanalysis (R-2), Bull. Amer. Meteor. Soc., Vol. 83,<br />

pp. 1631—1643, 2002.<br />

Markowski, P. M., and D. J. Stensrud, Mean monthly<br />

diurnal cycles observed with PRE-STORM surface data,<br />

J. Climate, Vol. 11, No. 11, pp. 2995—3009, 1998.<br />

Pandya, R. E., D. R. Durran, M. L. Weisman, The influence<br />

of convective thermal forcing on the three-dimensional<br />

mesoscale circulation around squall lines, J. Atmos. Sci.,<br />

Vol. 57, No. 1, 29—45, 2000.

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