page 1 developments in regional da oct 2007 © crown copyright 2007 mark naylor, bruce macpherson,...
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Page 3 Developments in regional DA Oct 2007 © Crown copyright 2007 Impact of LS subsidence (similar to first ECMWF scheme) positive impact on moisture field Cape closure perturbations (main term) positive impact on virtually all fields PF convection parametrisation in 4DVAR (Olaf Stiller) Two contributions: Unsteady/noisy UM convection scheme motivated statistical approach with time smoothing of input fields from nonlinear modelTRANSCRIPT
Developments in regional DA Oct 2007 © Crown copyright 2007 Page 1
Mark Naylor, Bruce Macpherson, Richard Renshaw, Gareth DowData Assimilation and Ensembles , Met R & D
Developments in regional data assimilation
at the Met OfficeEWGLAM / SRNWP 2007
new NAEUK4
Developments in regional DA Oct 2007 © Crown copyright 2007 Page 2
NAE Data Assimilation changes 2007
GPS IWV introduced (1 per 6 hr) aerosol background error reduced AIRS over land introduced (above 400hPa) More frequent ATOVS data (+ thinning 40 80km)
More frequent GPS IWV data (1 per hr) PF-Model Convection cease soil temperature increments under snow
introduce IASI introduce ASCAT
Mar 07
Aug 07
Nov 07
Developments in regional DA Oct 2007 © Crown copyright 2007 Page 3
Impact of LS subsidence (similar to first ECMWF scheme)positive impact on moisture field
Cape closure perturbations(main term)positive impact on virtually all fields
PF convection parametrisation in 4DVAR (Olaf Stiller)
Two contributions:
Unsteady/noisy UM convection scheme motivated statistical approachwith time smoothing of input fields from nonlinear model
Developments in regional DA Oct 2007 © Crown copyright 2007 Page 4
PF convection – linearisation test (Olaf Stiller)
after 6 hours
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PF convection - trial results
Summer 2006 NAE trial Generally beneficial in most variables +1% on UK Index (skill score for T2m, v10m, rain, cloud, visibility)
rms PMSL rms T2m
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soil temperature increments
ΔT (soil level 1) = ΔT (atmosphere level 1) in NAE helps retain benefit of screen temperature assimilation (no screen level assimilation or ΔT (soil) in global model)
CNTL
no ΔT(soil)
mean
T2m
rms
T2m
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soil temperature increments …..under snow
ΔT (soil level 1) = ΔT (atmosphere level 1) not sensible when snow insulates the soil Feb 07 night-time T2m errors in Finland ~10-15K
soil temp difference (NAE-GLOBAL) snow cover
20K !
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Ground GPS IWV (operational since March 07)
Operational coverage
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Ground GPS IWV
● Pre-operational trials gave slight benefit in screen temperature, rain, cloud and visibility. (~0.5% on UK Index)
● Obs frequency increased to hourly (Aug 07) with neutral impact / slight benefit
● Further trials to optimise assimilation underway- adjusting obs errors and forward model
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IASI trial
1-month trial – May 2007 Global trials gave benefit in PMSL & upper-level winds NAE trial showed small benefit in UK pmsl
mean rms CNTL
IASI
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ASCAT
ASCAT data – implementation due Nov 07 in NAE 10-day NAE trial May 2007(impact neutral), following longer
global trials ASCAT observations for QY18, with ERS2 and Seawinds
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Weather radar – VAD winds
Currently assimilated 61 rejected 26
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VAD wind impact experiment
3-week 24km NAE 4DVAR test, autumn 2006
CNTL
noVAD
mean
pmsl
rms
pmsl
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VAD wind impact experiment - 2
Pmsl benefit statistically significant when error bars computed for mean difference in CNTL / noVAD errors
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Part 2
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4km UK model assimilation
3DVARnudging scheme for cloud & rainfall assimilationeight 3-hourly cycles per day forecasts to t+36 from 03, 09, 15, 21 UTC lateral boundaries from hh-3 run of 12km NAE
Developments in regional DA Oct 2007 © Crown copyright 2007 Page 17
UK model – increased vertical resolution
38 70 levels same top at ~40km 7 16 levels in bottom 1km lowest theta level at 5m lowest wind level at 2.5m
due for implementation Nov 2007
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UK model – 70 level forecast error covariances
variant of laggedNMC method
74 forecast pairs t+12 – t+24
horizontal scales psi 130km chi 180km Ap 130km mu 90km log m 90km
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UK model – 70 level case study trial – pmsl (17 cases)
mean rms
L38
L70
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UK model – 70 level case study trial – T2m
mean rms
L38
L70
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UK model – 70 level case study trial – RH2m
mean rms
L38
L70
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UK model – 70 level case study trial – v10m
rms
vector
mean
speed
L38
L70
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UK model – 70 level case study trial – cloud cover
rmsmean
L38
L70
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UK model – 70 level case study trial – 6-hourly rainfall
0.2mm /6 hr
1mm /6 hr
4mm /6 hr
solid L38
dashed L70
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Future work
Upgrade NAE (and global) to 70 levels (Feb 08). Initial 1-month trial in NAE completed Physics package still under development
MOPS cloud data in 4DVAR to replace nudging PF model boundary layer scheme (autumn 08) ensemble-based covariances ? replace NAE continuous assimilation with single
cycle spin-up from previous global ‘update’ analysis
2009: new computer retain 12km NAE when global 25km nest 1.5km UK model with variable resolution perimeter into
12km NAE
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OPERA composite
NAE impact experiment is planned with OPERA composite (Spring 08) promote benefits to NWP of radar data exchange within Europe clarify requirements from NWP for operational radar data hub prepare for eventual operational assimilation
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Questions?
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Visibility/Aerosol tuning
3-week package trial consisting of:- Reduced visibility background error Climatological aerosol in radiation (not prognostic aerosol) Maximum aerosol concentration reduced (200µg/kg) Relaxation to climatological aerosol increased (20days)
Significant benefit seen in Screen temperature