presentation I - MANHAZ

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Dry deposition for aerosol dCi ( zref ) Vg ⋅Ci ( zref = − dt ∆z Vg υs R R R R υ + 1 = + + a b Bounce-off effect is calculated for aerosols a b s )
Wet deposition: in-cloud in cloud scavenging For soluble component C: ∆C wet = Win ⋅ P −C ∆z ⋅ ρ w
Page 1 and 2: EMEP long range transport air pollu
Page 3 and 4: What is EMEP and why EMEP? EMEP -
Page 5 and 6: Beginning of EMEP 1977 - A new pro
Page 7 and 8: Major principles of CLTRAP: a) The
Page 10 and 11: Elements of the EMEP programme: pro
Page 12 and 13: Development of the EMEP models Traj
Page 14 and 15: EMEP UNIFIED model UNI - AERO EMEP
Page 16 and 17: Vertical structure σ - co-ordinate
Page 18 and 19: Model equation p − pT σ = p* * p
Page 20 and 21: Meteorological data
Page 22 and 23: Anthropogenic emissions Sulphur dio
Page 24 and 25: Emissions VOC - VOC emissions are s
Page 26 and 27: Initial and boundary conditions Fou
Page 28 and 29: Abbreviations
Page 30 and 31: Photolysis reactions
Page 32 and 33: Chemical reactions
Page 38 and 39: Chemical reactions Numerical soluti
Page 42 and 43: Wet deposition: below-cloud below c
Page 44 and 45: Computer implementation 1. Parallel
Page 46 and 47: POP model (MSCE-POP) (MSCE POP) Eul
Page 48: Future of EMEP models • Hemispher

presentation I - MANHAZ

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