PDF file - Department of Physics

More documents

Recommendations

Info

How does water vapor condense on ice particles? 5 s D * modified diffusion constant including limitation by mass accomodation () 10 20 CRYSTAL-FACE 600 300 120 s 60 .
How does water vapor condense on ice particles? Sedimentation How could supersaturation be maintained?
Page 1 and 2: The High Supersaturation Puzzle
Page 3 and 4: Saturation ratio with respect to ic
Page 5 and 6: Two questions central to our unders
Page 7 and 8: How do we expect S in a cirrus to d
Page 9 and 10: Jensen et al., Atmos. Chem. Phys.,
Page 11 and 12: Lee et al., JGR, 2004: Measured tem
Page 13 and 14: Increasing stratospheric humidity I
Page 15 and 16: “T hey live for a short tim e in
Page 17 and 18: Atmospheric Application Water Activ
Page 19: ice saturation ratio S What does th
Page 23 and 24: Steady-state S to a good approximat
Page 25 and 26: Steady-state S in cirrus: tradition
Page 27 and 28: Steady-state S in cirrus: tradition
Page 29 and 30: Several slides with unpublished dat
Page 31 and 32: Shilling et al., Vapor Pressure of
Page 33 and 34: Potential out-of-cloud effects: Lac
Page 35 and 36: ice saturation ratio S Potential ou
Page 37 and 38: Potential in-cloud effects: Mesosc
Page 40 and 41: Potential in-cloud effects: HNO 3
Page 42 and 43: ice saturation ratio S Potential in
Page 44 and 45: Summary of Potential Explanations:
Page 46: Summary of Potential Explanations:

PDF file - Department of Physics

Create successful ePaper yourself

Delete template?

Save as template?