P72 Upgrading from WRF
3.1.1 to WRF 3.4.1 operationally at Metservice: Comparison of the two versions for
eleven significant weather events
Davis,
Cory,
Dominikus Heinzeller,
Graham Rye, Paul Shucksmith, Peter Kreft, John Crouch, Heath Gullery,
Paul Mallinson, Chris Noble, Liz Walsh, Brooke
Lockhart, and Chelsea Russ, Metservice
At
Metservice we run 24 WRF models over New Zealand,
Australia, UK, Europe and
Asia,
at various horizontal resolutions, using GFS, ECMWF, and UKMO NWP
data for initial and boundary conditions. Since 2009, we
have been using a
slightly modified version of WRF 3.1.1. To benefit from
recent improvements in
the WRF system, and to enable more effective research
on improving our
implementation of WRF, we upgraded to version 3.4.1
operationally in May 2013.
A
critical application of our WRF output is its use as guidance by all
forecasting desks (severe weather, public, marine, and aviation) in our
National Weather Service. It was necessary to get forecaster feedback and
acceptance before making the upgrade operational. This was
done by running the new and old versions over 11 historical cases that were
selected by forecasters. To ease the transition to
the new version, no changes were made to physics
options. The historical cases
included severe air mass convection and embedded convection
events, broad scale
wind, rain, and snow events, marginal wind and rain
events, and a major fog
event. A customized imagery viewer was created, allowing
easy comparison, and
forecasters from all desks were invited to comment on an
internal wiki page. Overall the new version was found to better represent the
cases considered, although in an airmass convection
case, the low level wind field was significantly
different in the new version, misplacing an area of convergence, and removing
the signal of a severe convection event. Differences in the low
level wind field were noticeable in several other cases.
This
poster describes the historical cases, the configuration of WRF, and the
relative performance of versions 3.1.1 and 3.4.1.