presentation I - MANHAZ

More documents

Recommendations

Info

Model equation p − pT σ = p* * p = p − p S T
Advection Bott 4 th order - horizontal Bott 2 nd order with variable grid distance in vertical Pure air is also advected to conserve mass After each advection step the new mixing ratios are calculated: C p t+ ∆T x * = * t+ ∆t x = * t+ ∆t ( Cair p ) p S ( C − p T p )
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 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 40 and 41: Dry deposition for aerosol dCi ( zr
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

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?