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Numerical Weather Prediction Models
Prepared by C. Tubbs, P. Davies, Met Office UK Revised, delivered by P. Chen, WMO Secretariat
SWFDP-Eastern Africa Training Workshop Bujumbura, Burundi, 11-22 November 2013
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NWP Model Formulation
1. Different types of model
2. Model Characteristics
3. General strengths and weaknesses of NWP models
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Types of atmospheric model
• Climatological• Global Climate Models (GCM’s)• Hindcasts and forecasts• Climate change – global warming• Non-operational weather forecasting models
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Types of atmospheric model
• Long-term and seasonal • Coupled ocean-atmosphere models• Aims to infer climate from indicators such as
Sea Surface Temperature (El Nino)• Forecasts issued by ECMWF every month • Typically based on ensemble methods
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Types of atmospheric model
• Global NWP models• Operational forecasting models• Run twice to four times daily• Generally short- to medium-range (typically
t+144h)• Global output coverage (datasets) • Hi-res “deterministic” vs EPS
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Types of atmospheric model
• Limited Area Models (mesoscale/LAMs)• Add local detail to broad picture from global
model• Take boundary conditions from global• Higher resolution, so better representation of
small scale events• Shorter forecast range (typically t+48h) • Careful (especially if approaching cloud-
scale!): kinematic effects vs dynamical processes
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Types of atmospheric model
• Very-short-range (<12h) incl. Nowcasting• Nowcasting aims to give best forecast for time
period of <4-6h hours lead-time • Blend of model and observational data • e.g. UK Met Office uses the NIMROD system
• Specific applications• Atmospheric Dispersion• Air quality • Lee-wave forecasting models
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Models
« Anticipated advances in NWP, and thegrowing technology gap in weather forecasting »
(2013)
http://www.wmo.int/pages/prog/www/swfdp/Meetings/documents/Advances_NWP.pdf
See Annex II for NWP systems
? T574L64 ~27km ? ? EPS 50 members +1 control ?
? forecast range / max. lead-time ?
t+144h ? ? domain ?
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ECMWFGlobal High-Res. IFS • Horizontal resolution of T1279 (16km),
91 vertical levels• 240h forecast range (10 days ahead)• 4-D VAR
Global EPS – Ensemble Prediction System
• 50 members, T319 (65km), 62 levels
T= spectral truncation
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NCEPNational Centers for Environmental
Prediction (Washington, USA)
• GFS (Global Forecasting System) model – T574 L64 (27km, 2010), T1148 (18km, planned 2013), and
• GEPS ensemble model – 42 members, T190 (70km)
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Met Office UK
Global model “UM”• Horizontal resolution of 25 km and L70
vertical levels• 4 times daily • Run out to t+144h• 4DVar MOGREPS-15 (UM) Global 23 members, 60km, L70
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UK Met Office
• Africa LAM – retired October 2013
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UK Met Office
Lake Victoria LAM
• 4 km horizontal resolution, 70 vertical levels
• Available via password protected website http://www.metoffice.gov.uk/weather/africa/lam/
• Username is afr_nms and password is uk_alam• Intermittent data assimilation• Run to t+48h
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Strengths & Weaknesses of NWP models
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Strengths & Weaknesses
• There are generic problems common to most NWP
• If we know about these we can account for them in our initial verification
• Most problems are related to resolution
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NWP Strengths
• Convection• General area of convection is well captured
• Extra-tropical latitudes• Model is much better here• Frontal systems are well represented• Orographically enhanced rainfall better
than Global Model
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Generic Problems
• Inaccurate Initial Conditions• Lack of data• Imperfect data assimilation
• Resolution• Horizontal resolution may cause small scale
features to be missed• Vertical profile may not capture full detail e.g.
inversions, localised temperature advection
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Generic Problems
• Orography• Generally flattened – less steep and less high• Some features completely omitted• Orography in LAMs is better than in global
models but still not perfect
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Generic Problems
• Lateral Boundary Conditions• Only a problem for LAM’s• Spin up problems when transposing low
resolution data onto a high resolution grid• Potential problems at edge of domain
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NWP Weaknesses
• Tropical Convection• Representation of diurnal cycle is poor• Convection initiated too early and is too
widespread• 0600-1200 ppn accumulation frames
contain much spurious ppn but can indicate areas of activity
• Fails to develop large scale, long-lived mesoscale convective systems
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NWP convection switched on….
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NWP convection switched off….
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Questions & Answers