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Urban Modelling 1 03/2003 © Crown copyright Urban Scale NWP with the Met Office's Unified Model Peter Clark Mesoscale Modelling Group Met Office Joint Centre for Mesoscale Meteorology University of Reading
Urban Modelling 2 03/2003 © Crown copyright Why Mesoscale Models? Mesoscale variation of boundary layer structure due to: –Changes in surface characteristics. »Urban/rural »Land/sea »Soil moisture/surface temperature –Orography. Mesoscale flows induced by above. –Land/sea breeze. –Drainage flows. Mesoscale structure in synoptic meteorology –Fronts –Convective storms Air Quality Weather Forecasting
Urban Modelling 3 03/2003 © Crown copyright Why the Unified Model (UM)? Non-hydrostatic, fully compressible, deep atmosphere. Suitable for use at very high spatial resolution. The UM surface exchange scheme treats urban areas and is being improved. Data assimilation is a powerful tool; makes UM data a major resource. UM availability and improvements. –Available to and adopted by NERC community. –Portable UM 5 released VERY soon. –SLICE: A Semi-Lagrangian Inherently Conserving and Efficient scheme for transport problems Operational Plans: –UK ~4 km 2005. –1 km ~2008-10 for v short range.
Urban Modelling 4 03/2003 © Crown copyright Example results from High Resolution Trial Model Visibility (m) 12 km 4 km1 km
Urban Modelling 5 03/2003 © Crown copyright Blending Height Surface UM Tile surface exchange Treats heterogeneous surfaces using blending height techniques. Nine surface types, –Broad Leaf Trees –Needle Leaf Trees –C3 Grass –C4 Grass –Shrub –Urban –Water –Soil –Ice Each tile has fixed characteristics. 4 layer soil temperature and moisture.
Urban Modelling 6 03/2003 © Crown copyright s T s 4 g T g 4 H E s T s 4 G RNRN Urban Tiles Each tile has a full surface energy balance. This includes a radiatively coupled canopy. In the urban case this has high thermal inertia to simulate wall effects. Work in progress (Reading) to improve representaion, especially of radiative effects.
Urban Modelling 7 03/2003 © Crown copyright 12 km 4 km 1 km Model Configuration Met Office non-hydrostatic semi- implicit, semi-Lagrangian Unified Model, 38 levels on stretched height based terrain following grid. One-way nested –Global (~60km) 20 min timestep –~12 km (146X182) 5 min timestep –~4 km (300x300) 2 min timestep –~1 km (300x300) 0.5 min timestep 12 km down to 1 km run from operational 3D VAR mesoscale analysis at 12Z 10th May 2001 Tiled land surface scheme using CEH 25 m Landsat based land-use including urban fraction. Model ignores man-made heat sources
Urban Modelling 8 03/2003 © Crown copyright Example 1 km domain Orography Urban Fraction in Land Use Grass Fraction in Land Use
Urban Modelling 9 03/2003 © Crown copyright Formation of the night time urban heat island Light Wind 00Z 11/05/2001 Urban-No-Urban Near surface temperature difference
Urban Modelling 10 03/2003 © Crown copyright Urban fraction Point 1: 1 % Point 2: 97 % Point 3: 50 % Point 4: 1 % Urban Fraction and contours of Urban Impact on 20 m Temperature 1 2 3 4 0.5 1.0 1.5 00Z 11/05/2001
Urban Modelling 11 03/2003 © Crown copyright Point 2 Point 3 Point 1 Point 4 Point 1: Upstream Point 2: Central London Point 3: Downstream Suburbs Point 4: Downstream Rural Evolution of vertical structure over London
Urban Modelling 12 03/2003 © Crown copyright Impact on vertical mixing. Urban Area produces 200 m near neutral boundary layer Central London
Urban Modelling 13 03/2003 © Crown copyright Tracer release broadly reflecting smoothed emissions Afternoon deep convection brings down clean air Night time stabilization Blocking of flow by North Downs Arbitrary Units Predictable? Unpredictable!
Urban Modelling 14 03/2003 © Crown copyright Regional tropospheric data assimilation of tracers/chemistry? Ambitious, but shouldnt we be? 3D VAR stratospheric chemistry, tropospheric 'aerosol' already a reality. DA discipline forces objective analysis of model error, observation error and representativity/covariance. 4D VAR of tracers has potential to improve model transport as well as provide concentration fields. Tracer assimilation straightforward using model dynamics. Conceivable using alternative dispersion if incorporated into UM. DARC
Urban Modelling 15 03/2003 © Crown copyright Towards a Modelling Strategy Based on the Unified Model Provision of higher resolution UM output to drive offline transport/dispersion (NAME + Others). Use of UM in NERC community to validate/improve meteorology. –Benefits of using operational analyses including sub-surface. Closer coupling of transport/chemistry with UM. –Using UM transport OR alternative (NAME, parcel, Eulerian) –Consistent physics –Shorter updating interval for winds Start thinking in a data assimilation framework –Model error covariances –Observation representativity defined with respect to model. Eventual implementation of multiscale DA of quasi-conserved species.
1 Rachel Capon 04/2004 © Crown copyright Met Office Unified Model NIMROD Nowcasting Rachel Capon Met Office JCMM.
Evolution and Performance of the Urban Scheme in the Unified Model Aurore Porson, Ian Harman, Pete Clark, Martin Best, Stephen Belcher University of Reading.
The University of Reading Helen Dacre AMS 2010 Air Quality Forecasting using a Numerical Weather Prediction Model ETEX Surface Measurement Sites.
The University of Reading Helen Dacre UM user 2009 Forecasting the transport of pollution using a NWP model ETEX Surface Measurement Sites.
The University of Reading Helen Dacre AGU Dec 2008 Boundary Layer Ventilation by Convection and Coastal Processes Helen Dacre, Sue Gray, Stephen Belcher.
Page 1© Crown copyright Modelling the stable boundary layer and the role of land surface heterogeneity Anne McCabe, Bob Beare, Andy Brown EMS 2005.
Regional Modelling Prepared by C. Tubbs, P. Davies, Met Office UK Revised, delivered by P. Chen, WMO Secretariat SWFDP-Eastern Africa Training Workshop.
1 00/XXXX © Crown copyright URBAN ATMOSPHERIC CHEMISTRY MODELLING AT THE METEOROLOGICAL OFFICE Dick Derwent Climate Research Urban Air Quality Modelling.
Trials of a 1km Version of the Unified Model for Short Range Forecasting of Convective Events Humphrey Lean, Susan Ballard, Peter Clark, Mark Dixon, Zhihong.
Page 1© Crown copyright 2006 NWP in the Met Office.
Laura Davies, University of Reading, UK. Supervisors: Bob Plant, Steve Derbyshire (Met Office)
1 NGGPS Dynamic Core Requirements Workshop NCEP Future Global Model Requirements and Discussion Mark Iredell, Global Modeling and EMC August 4, 2014.
Page 1© Crown copyright 2006SRNWP 9-12 October 2006, Zurich Variable resolution or lateral boundary conditions Terry Davies Dynamics Research Yongming.
A numerical simulation of urban and regional meteorology and assessment of its impact on pollution transport A. Starchenko Tomsk State University.
Introduction to data assimilation in meteorology Pierre Brousseau, Ludovic Auger ATMO 08,Alghero, september 2008.
© Crown copyright Met Office Experiences with a 100m version of the Unified Model over an Urban Area Humphrey Lean Reading, UK WWOSC.
From Rain into Water Peter Ewins Chief Executive Met Office.
1 00/XXXX © Crown copyright Carol Roadnight, Peter Clark Met Office, JCMM Halliwell Representing convection in convective scale NWP models : An idealised.
JMA Takayuki MATSUMURA (Forecast Department, JMA) C Asia Air Survey co., ltd New Forecast Technologies for Disaster Prevention and Mitigation 1.
Next Gen AQ model Need AQ modeling at Global to Continental to Regional to Urban scales – Current systems using cascading nests is cumbersome – Duplicative.
Page 1 NAE 4DVAR Oct 2006 © Crown copyright 2006 Mark Naylor Data Assimilation, NWP NAE 4D-Var – Testing and Issues EWGLAM/SRNWP meeting Zurich 9 th -12.
Martin G. Schultz, MPI Meteorology, Hamburg GEMS proposal preparation meeting, Reading, Dec 2003 GEMS RG Global reactive gases monitoring and forecast.
08/20031 Volcanic Ash Detection and Prediction at the Met Office Helen Champion, Sarah Watkin Derrick Ryall Responsibilities Tools Etna 2002 Future.
Page 1© Crown copyright 2004 SRNWP Lead Centre Report on Data Assimilation 2005 for EWGLAM/SRNWP Annual Meeting October 2005, Ljubljana, Slovenia.
1/29 Parametrization of the planetary boundary layer (PBL) Irina Sandu & Anton Beljaars Introduction Irina Surface layer and surface fluxes Anton Outer.
Dispersion conditions in complex terrain - a case study of the January 2010 air pollution episode in Norway Viel Ødegaard Norwegian Meteorological.
Non-hydrostatic Numerical Model Study on Tropical Mesoscale System During SCOUT DARWIN Campaign Wuhu Feng 1 and M.P. Chipperfield 1 IAS, School of Earth.
For more information about this poster please contact Gerard Devine, School of Earth and Environment, Environment, University of Leeds, Leeds, LS2 9JT.
Page 1 Developments in regional DA Oct 2007 © Crown copyright 2007 Mark Naylor, Bruce Macpherson, Richard Renshaw, Gareth Dow Data Assimilation and Ensembles,
Meteorology meets Astronomy : open discussion 1.Usefullness of atmospheric mesoscale modelling for astrophysical applications - to forecast astrophysical.
INTERCONTINENTAL TRANSPORT OF OZONE AND ITS SEASONAL VARIATIONS IN EUROPE Dick Derwent rdscientific 2 nd ICAP Workshop Chapel Hill, North Carolina October.
KMD Consortium for Small-Scale Modeling (COSMO) Strengths and Weaknesses Vincent N. Sakwa RSMC, Nairobi.
DYMECS: Dynamical and Microphysical Evolution of Convective Storms (NERC Standard Grant) University of Reading: Robin Hogan, Bob Plant, Thorwald Stein,
© European Centre for Medium-Range Weather Forecasts Operational and research activities at ECMWF now and in the future Sarah Keeley Education Officer.
© University of Reading 2007www.reading.ac.uk RMetS Student Conference, Manchester September 2008 Boundary layer ventilation by mid-latitude cyclones Victoria.
03/06/2015 Modelling of regional CO2 balance Tiina Markkanen with Tuula Aalto, Tea Thum, Jouni Susiluoto and Niina Puttonen.
Accounting for Uncertainties in NWPs using the Ensemble Approach for Inputs to ATD Models Dave Stauffer The Pennsylvania State University Office of the.
CMAQ (Community Multiscale Air Quality) pollutant Concentration change horizontal advection vertical advection horizontal dispersion vertical diffusion.
Earth Science Division National Aeronautics and Space Administration 18 January 2007 Paper 5A.4: Slide 1 American Meteorological Society 21 st Conference.
ESF- MedCLIVAR Workshop Climate Change Modeling for the Mediterranean region, ICTP, Trieste, Italy, Oct 2008 Regional air quality decadal simulations.
A NUMERICAL PREDICTION OF LOCAL ATMOSPHERIC PROCESSES A.V.Starchenko Tomsk State University.
Weather Research & Forecasting Model (WRF) Stacey Pensgen ESC 452 – Spring ’06.
Ross Bannister Balance & Data Assimilation, ECMI, 30th June 2008 page 1 of 15 Balance and Data Assimilation Ross Bannister High Resolution Atmospheric.
© Crown copyright Met Office Regional climate model formulation PRECIS Workshop, Reading University, 23 rd – 27 th April 2012.
GEMS Kick- off MPI -Hamburg CTM - IFS interfaces GEMS- GRG Review of meeting in January and more recent thoughts Johannes Flemming.
Mesoscale Modeling Review the tutorial at: –In class.
Chapter 13 – Weather Analysis and Forecasting. The National Weather Service The National Weather Service (NWS) is responsible for forecasts several times.
© Crown copyright Met Office Downscaling ability of the HadRM3P model over North America Wilfran Moufouma-Okia and Richard Jones.
Météo-France / CNRM – T. Bergot 1) Introduction 2) The methodology of the inter-comparison 3) Phase 1 : cases study Inter-comparison of numerical models.
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