Mesoscale model experience with UM at met.no

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Mesoscale model experience with UM at met.no. HIRLAM-ALADIN-MF miniworkshop 12/12/05 Dag Bjørge. NWP collaboration in Europe. Short version of UM history at met.no. 2002: Met Office–met.no NWP collaboration 2003: UM 3km, S-Norway grid, forced by Met Office 20km and Hirlam 10km - PowerPoint PPT Presentation

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Mesoscale model experience with UM at met.no

HIRLAM-ALADIN-MF miniworkshop 12/12/05Dag Bjørge

Norwegian Meteorological Institute met.no

NWP collaboration in Europe

Norwegian Meteorological Institute met.no

Short version of UM history at met.no

• 2002: Met Office–met.no NWP collaboration• 2003: UM 3km, S-Norway grid, forced by Met

Office 20km and Hirlam 10km• 2004: UM 4km, Norway grid, forced by HL

10km• 2005: ”UM4XL”, Norway/Sweden grid• Nov2005: UM 1km, 3 small grids nested into

UM4XL

Norwegian Meteorological Institute met.no

How does it perform ?

Norwegian Meteorological Institute met.no

Temperature

Norwegian Meteorological Institute met.no

Norwegian Meteorological Institute met.no

Norwegian Meteorological Institute met.no

How is the UM model set up ?

• Climate and parameter files from Met Office ”ancil generation” software

• LBC’s from Hirlam 10km, interpolation with ”hl2um” ( a met.no mixture of subroutines from UM and Hirlam )

• Some surface fields from Hirlam …• Some fields from previous +12h

forecast …

Norwegian Meteorological Institute met.no

• 300 * 500 * 38 gridpoints, • 4km resolution, 100s timestep• Hourly postprocessing of surface fields, 3

hourly pressure levels, 6 hourly model levels

• Boundary fields written out every 20 minutes for +8h to +21h, for nesting of 3 UM 1km grids

• Runs on 280 CPUs, at 00UTC and 12UTC• 48h forecast in ~1h45min• SGI Origin 3800 ( to be replaced next

year )

Norwegian Meteorological Institute met.no

What does it look like ?

• Quasi operational runs• Different experiments• Temperature problem solved (last

week)

Norwegian Meteorological Institute met.no

The model chain at met.no

• The ”turbulence project” is used to describe the different models we now have available for forecasting at global to local ( airport ) scale.

Norwegian Meteorological Institute met.no

Why a turbulence project ?

”På grunn av variable og vanskelige vindforhold bestemte kapteinen seg for å avbryte landinga. Da kom det et kraftig vindkast, og flyet smalt i bakken.”

Norwegian Meteorological Institute met.no

• Orography and resolution ( ”Seven sisters” )

Norwegian Meteorological Institute met.no

LBCs (~50km) for Hirlam20 and Hirlam10 at 3 hour intervals ( usually 6 hours old )

Norwegian Meteorological Institute met.no

Hirlam10

• Starts from interpolated Hirlam20-analysis

• Boundaries ( frames ) from ECMWF• Writes ”model dumps” / ”history files”

every hour for nesting of Met Office Unified Model ( UM4 )

Norwegian Meteorological Institute met.no

Hirlam10 and UM4

Norwegian Meteorological Institute met.no

UM 4km with three UM 1km grids

Norwegian Meteorological Institute met.no

The ”lifetime” of LBCs in a small grid

•30min intervals

Norwegian Meteorological Institute met.no

UM1

• Starts for all airports as soon as UM4 has reached it’s +21 hour forecast

• UM1 starts at UM4 +8h forecast, spins up for one hour

• Writes full model dumps at +9, +12, +15, +18 and +21

• The turbulence model called ”Simra” is then run for each of these instances

Norwegian Meteorological Institute met.no

Operational cycles

• The model system as described is run twice a day at 00UTC and 12UTC

• Results are continously updated through the run, and can be studied as the forecast is produced

Norwegian Meteorological Institute met.no

UM1, Sandnessjøen

Norwegian Meteorological Institute met.no

Example of product, inflight cone

Norwegian Meteorological Institute met.no

Example of product, inflight turbulence in cross section

Norwegian Meteorological Institute met.no

Some examples of different treatment of precipitation in the different models

Norwegian Meteorological Institute met.no

”Precipitation shaddow”, Hirlam / UM

Norwegian Meteorological Institute met.no

Tromsø-area, Hirlam10 and UM4

Norwegian Meteorological Institute met.no

Structure of precipitation, HL20/10, UM4, radar

Norwegian Meteorological Institute met.no

Ad hoc setup of UM for the Barents sea

• Example showing a ”polar low”

Norwegian Meteorological Institute met.no

Polar low in UM 4km

Norwegian Meteorological Institute met.no

Hirlam10 og UM4

Norwegian Meteorological Institute met.no

UM4 +23h, mslp and wind

Norwegian Meteorological Institute met.no

Temperature problem ( solved last week )

• um505_thetamono_no.mf77 • A fix for the valley cooling problem.

It is an active area of investigation and we may come up with alternative/better solutions, but this will hopefully work in the short term.

Norwegian Meteorological Institute met.no

Norwegian Meteorological Institute met.no

Norwegian Meteorological Institute met.no

Norwegian Meteorological Institute met.no

Comparing Hirlam and UM

• Hirlam has been set up on exactly the same ( horizontal ) grid as UM4XL

• Hirlam version 6.4.1+• H04 runs started in November on the

met.no Linux cluster• Some technical difficulties …• Computer resources (SGI) : UM = 3 *

HL

Norwegian Meteorological Institute met.no

Heavy precipitation and flooding at the western coast of Norway in November

Norwegian Meteorological Institute met.no

Norwegian Meteorological Institute met.no

Hirlam 4km UM 4km

Norwegian Meteorological Institute met.no

Hirlam 4km, 12h accumulated precip

Norwegian Meteorological Institute met.no

UM 4km, 12h accumulated precip

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