1. Urban Aerosol Impacts on Downwind Convective Storms
Speaker:陳文彬
VAN DEN HEEVER,S. AND WILLIAM R. COTTON
J. Appl. Meteor. Climate.,46,

2. St .Louis 8 June 1999
雷達回波：contour:10dBZ

3. Grid1：37.5km Grid2：7.5km Grid3：1.5km

4. Aerosol initialization concentrations

5. 方形矩陣：downwind calculation

6. Shaded : T Contours: water vapor mixing ratio
Time evolution of the RURAL-H - NOCITY-H temperature and water vapor mixing ratio fields
Shaded : T
Contours: water vapor mixing ratio

7. Higher background aerosol concentration results

8. RURAL-H test
Contoured at 750m:
Updraft velocity
Shaded: CCN個數at 500m

9. NOCITY-H test

10. URBAN-H test.

11. Time series of the total hydrometeor mass

12. Time series of the accumulated volumetric precipitation

13. Lower background aerosol concentration results

14. RURAL-L simulation

15. URBAN-L simulation

16. Time series of (a) the maximum updraft within the downwind region and (b) the average of the
Maximum downdraft within the downwind region

18. Time series of the (left) cloud and (right) rain mixing ratios

21. RURAL-L URBAN-L accumulated surface precipitation

22. Conclusions
When GCCN or both CCN and GCCN concentrations were enhanced, cloud water and rain formed more rapidly. The updrafts were also stronger initially, and the downdrafts developed more quickly.
Greater amounts of surface precipitation were also produced in these cases during the first 1.25–1.5 h. When CCN alone were enhanced, the formation of cloud water, rain, and all of the ice species was delayed, as was the development of both the updrafts and downdrafts.
The surface precipitation was suppressed in the presence of urban-enhanced CCN concentrations.

23. Conclusions
GCCN and both GCCN and CCN are enhanced leads to earlier in the storm life cycle than in the control simulation.
Urban aerosol effects on downwind convection and precipitation could be expected to be greater in less industrialized regions of the United States, as well as in countries such as Canada and Australia, where the background aerosol concentrations are generally lower.
The extremely complex, nonlinear relationships between the microphysics and dynamics therefore make it difficult to make absolute statements regarding the impacts of urban-enhanced CCN and GCCN on downwind convection and precipitation.