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Proceedings - C-SRNWP Project

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Cycle Date Model change and impact<br />

U4.03 11 Oct 2005 UM version upgraded to UM6.1<br />

Targeted moisture diffusion instead of horizontal<br />

moisture diffusion. (change reversed in cycle U4.04)<br />

Empirically adjusted cloud fraction introduced - removes<br />

negative cloud bias.<br />

Convection upgrade to 4A - improves precipitation<br />

Microphysics upgrade to 3D & revised autoconversion<br />

coefficients: reduces excessive light precipitation.<br />

Change in orography blending weights: Improve<br />

consistency of orography in LBC rim area.<br />

U4.04 13 Dec 2005 Introduce 3D-Var and an Analysis Correction scheme<br />

for cloud and precipitation<br />

4 main runs at 03, 09, 15 and 21 UTC<br />

Introduce gravity wave drag<br />

Replace targeted diffusion with horizontal diffusion<br />

Add water loading term as the specific humidity based<br />

dynamics does not consider the weight of precipitation<br />

products in the density.<br />

U4.05 14 Mar 2006 Mixing ratio replaces specific humidity in dynamics<br />

Include anthropogenic urban heat source<br />

U4.06 14 Jun 2006 Extension of domain to cover Shetlands<br />

Correction of MOPS cloud height<br />

U4.07 26 Sep 2006 Two small changes to the assimilation of radar data by<br />

Latent Heat Nudging (LHN):<br />

1) The scale for horizontal filtering of temperature<br />

increments reduced from 21km to 6km.<br />

2) The derivation of increments from sections of the<br />

model profile below cloud base, where evaporation is<br />

taking place is removed.<br />

The northward extension of the model domain allows a better representation of showers<br />

around Scotland in a northerly airstream as shown in Figure 7.<br />

55

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