Met Office dust forecasting Using the Met Office

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Met Office dust forecasting Using the Met Office Unified Model™ David Walters: Manager Global

Met Office dust forecasting Using the Met Office Unified Model™ David Walters: Manager Global Atmospheric Model Development, Met Office. (with M. E. Brooks, B. Ingleby, B. Johnson, J. Mulcahy, Y. Pradhan) © Crown copyright Met Office

Dust forecasting with the Met. UM © Crown copyright Met Office

Dust forecasting with the Met. UM © Crown copyright Met Office

Met Office Unified Model™ (Met. UM) A 'seamless' model used across all time and

Met Office Unified Model™ (Met. UM) A 'seamless' model used across all time and space scales. Met. UM framework includes: OPS, VAR, VER … © Crown copyright Met Office

Met Office Unified Model™ Atmospheric model components Dynamics: Physics: • Regular lat/lon grid. •

Met Office Unified Model™ Atmospheric model components Dynamics: Physics: • Regular lat/lon grid. • Spectral band radiation • Non-hydrostatic dynamics with a deep atmosphere. • Diagnostic or prognostic cloud • Semi-implicit time integration with 3 D semi-Lagrangian advection. • Mass flux convection • Atmospheric tracer advection • Mixed-phase ppn • Boundary layer • Gravity wave schemes • JULES land-surface model Aerosols/chemistry: • CLASSIC: SO 4, Soot, Biomass smoke, OCFF, x. NO 3, seasalt, dust • United Kingdom Chemistry Aerosol (UKCA) community model © Crown copyright Met Office

Dust in the Met. UM Woodward (2001, 2011) Friction velocity scheme using explicit U*

Dust in the Met. UM Woodward (2001, 2011) Friction velocity scheme using explicit U* over bare soil only: Horizontal flux: Kawamura (1951) Dry Ut* prescribed for each bin Iverson and White (1982) Soil moisture contribution to Ut* from top soil layer Fecan et al. (1999) Horizontal flux calculated for 9 size divisions Size division 1 2 3 4 5 6 7 8 9 Lower lim (mm) 0. 0316 0. 1 0. 316 1. 0 3. 16 10 31. 6 100 316 Upper lim (mm) 0. 1 0. 316 1. 0 3. 16 10 31. 6 100 316 1000 Horizontal and vertical flux © Crown copyright Met Office Saltation only

Dust in the Met. UM Crisis Area Model implementation Mrel, sand/silt/clay & soil properties

Dust in the Met. UM Crisis Area Model implementation Mrel, sand/silt/clay & soil properties from HWSD Nachtergaele et al (2008) e. g. grid-box clay fraction Vertical flux: © Crown copyright Met Office Gillette (1979)

Dust in the Met. UM Mapping from horizontal to vertical flux Using 6 size

Dust in the Met. UM Mapping from horizontal to vertical flux Using 6 size divisions: • Dynamically diagnosed from horizontal flux distribution: Currently used in climate research or • Prescribed following a fixed size distribution: Currently used in limited area NWP © Crown copyright Met Office

Dust in the Met. UM Mapping from horizontal to vertical flux Using 2 size

Dust in the Met. UM Mapping from horizontal to vertical flux Using 2 size divisions: Size division 1 2 3 4 5 6 7 8 9 Lower lim (mm) 0. 0316 0. 1 0. 316 1. 0 3. 16 10 31. 6 100 316 Upper lim (mm) 0. 1 0. 316 1. 0 3. 16 10 31. 6 100 316 1000 Horizontal saltation flux • Uses prescribed size distribution only Size division 1 2 Lower lim (mm) 0. 1 2 Upper lim (mm) 2 10 Vertical flux © Crown copyright Met Office Currently used in global NWP

Dust in the Met. UM Once dust is lifted: • Transported by SL advection

Dust in the Met. UM Once dust is lifted: • Transported by SL advection and • Interacts with radiation scheme via direct aerosol effect Can use climatological dust in radiation instead • Removed via dry/wet deposition Balkanski et al. (2007)

Operational dust models Global. Africa Southern North Model Asia Model • N 512 12

Operational dust models Global. Africa Southern North Model Asia Model • N 512 12 km (~25 km) 70 L (80 km 70 L lid)(80 km lid) • 4 D-Var 3 D-Var DA • 2 6 bin dust scheme since 2011 2008 • No dust DA • Radiation No dust inuses LBCsclimatology

Dust model validation © Crown copyright Met Office

Dust model validation © Crown copyright Met Office

Dust forecast validation

Dust forecast validation

Dust forecast validation • Dust Aerosol Optical Thickness (AOT) compared to AERONET

Dust forecast validation • Dust Aerosol Optical Thickness (AOT) compared to AERONET

Dust forecast performance ← → DUST ←… DUST

Dust forecast performance ← → DUST ←… DUST

Dust forecast validation Equitable Threat Score (ETS): fraction of observed events that were Demanding

Dust forecast validation Equitable Threat Score (ETS): fraction of observed events that were Demanding score for small correctly predicted, reduced by the numbers you would by chance. scale features asexpect correct prediction 0 – no skill means: • 1 exactly - perfect right place • right time (3 hour window)

Other validation methods • Subjective verification (including from theatre) • Verification of visibility against

Other validation methods • Subjective verification (including from theatre) • Verification of visibility against SYNOP/METAR • Model inter-comparison • Observational campaigns © Crown copyright Met Office

Global Model validation Pre-operational testing (April 2011) Met Office research news article on global

Global Model validation Pre-operational testing (April 2011) Met Office research news article on global dust forecasting: http: //www. metoffice. gov. uk/research/news/dust-forecasting

Global Model results Pre-operational testing Skill scores over SAM region: • beats the SAM

Global Model results Pre-operational testing Skill scores over SAM region: • beats the SAM for low severity events • capturing inflow into domain • misses high severity events • high res models still required? Model went operational in July 2011 Provide forecasts to SDS-WAS through MACC-II project from December 2011

Future developments © Crown copyright Met Office

Future developments © Crown copyright Met Office

Dust model developments • Validation show dust from areas with seasonal vegetation is important:

Dust model developments • Validation show dust from areas with seasonal vegetation is important: link dust emissions to “radiative bare soil fraction” • Dust DA currently being developed (to use SEVERI and MODIS AOD products) • Emissions sensitive to soil properties, soil moisture etc: further improvements required in these areas • Continuing to develop satellite products currently provided to WMO SDS-WAS Feedback on these products appreciated © Crown copyright Met Office

Summary Please take home the following points • Met Office dust forecasts operational since

Summary Please take home the following points • Met Office dust forecasts operational since 2008 • Model validation shows reasonable performance and has identified areas of potential improvement • Dust in 25 km global NWP since summer 2011 • Global model data to SDS-WAS from December 2011 © Crown copyright Met Office

Questions © Crown copyright Met Office

Questions © Crown copyright Met Office