1 / 12

Testable sensitivities of CTM simulations to meteorological fields

Testable sensitivities of CTM simulations to meteorological fields. Yuhang Wang Georgia Tech. Models. GEOS-CHEM: Used in some comparisons; provides chemical boundary conditions. Polar MM5 driven regional CTM: Boundary layer sensitivities MM5 driven RCTM (REAM): spring-summer transition

nhi
Download Presentation

Testable sensitivities of CTM simulations to meteorological fields

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Testable sensitivities of CTM simulations to meteorological fields Yuhang Wang Georgia Tech

  2. Models • GEOS-CHEM: Used in some comparisons; provides chemical boundary conditions. • Polar MM5 driven regional CTM: Boundary layer sensitivities • MM5 driven RCTM (REAM): spring-summer transition • MM5 and WRF driven REAM: convection and lightning in summer – INTEX-NA

  3. Arctic surface ozone depletion Default ETA MYJ 2.5-order closure Modified ETA (Zeng et al., 2006)

  4. Default ETA Modified ETA

  5. Boundary layer height at the South Pole, 2003 (Wang et al., 2007)

  6. Spring-summer transition:Trop NO2 column retrievals for February-May, 2000 (Choi et al, 2007)

  7. Surface O3 concentrations and afternoon mixing heights February-May, 2000

  8. Summer time convection and lightning MM5: Grell scheme WRF: new K-F scheme (Zhao et al., 2007)

  9. Lightning impact on NO2 column WRF-REAM MM5-REAM

  10. Lightning impact on NO2 at 500 hpa

  11. Convective scavenging of HNO3

  12. Surface O3 simulations

More Related