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NOAA G4

POLARCAT Pol ar Study using A ircraft, R emote Sensing, Surface Measurements and Models, of C limate, Chemistry, A erosols, and T ransport. March/April 2008. NOAA G4. Balloons. NASA DC8. NOAA WP3B. OASIS Ship. NOAA Ron Brown. ASTAR 2007. CNRS. Status on Funding Projects.

nathaniel-brock
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NOAA G4

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  1. POLARCATPolar Study using Aircraft, Remote Sensing, Surface Measurements and Models, ofClimate, Chemistry, Aerosols, and Transport 10th Anniversary Conference of the M-55 Geophysica

  2. March/April 2008 NOAA G4 Balloons NASA DC8 NOAA WP3B OASIS Ship NOAA Ron Brown ASTAR 2007 CNRS 10th Anniversary Conference of the M-55 Geophysica

  3. Status on Funding Projects France- French ANR funding (O3/aerosol lidars, in-situ aerosol, O3/CO on ATR) - 2 week summer campaign plus 1 week for YAK flights (Russian Antonov) over Siberia - forest fires (plus poss. spring 2008) Norway (Stohl) - funding expected (campaign coord., analysis etc.) Germany - DLR (Shlager) - summer 2008 (forest fires)? - looks promising plus spring 2007 (ASTAR campaign) Canada (Whiteway) - ECHO project - flights of 2 Twin Otters equipped with O3 & aerosol lidars - pyro-convection (2007 or 2008) (& Fromm, NRL, USA) USA NASA (Singh) - good feedback so far - summer 2008 - flights with DC8 - aerosol and chemistry; NOAA (Parrish) - possibly summer 2008 or spring 2008 with NOAA-P3 plus Ron Brown ship in spring 2008 10th Anniversary Conference of the M-55 Geophysica

  4. POLARCAT Objectives • tropospheric chemical composition - spring O3 max, • VOC/NOy reservoirs, halogen, chemistry, transport pathways • aerosols - radiative properties (direct/indirect), aerosol-cloud • interactions, optical properties • trace gas/ aerosol deposition - changes in surface albedo • Forest Fires and PyroCb: • Fate and effects of aerosols and chemical compounds injected into • the stratosphere by pyro-convection, • Their role for ozone formation and depletion • in the polar stratosphere http://zardoz.nilu.no/~andreas/POLARCAT/ 10th Anniversary Conference of the M-55 Geophysica

  5. MOPITT CO DATA - 6 to 12 August 500 hPa 350 hPa Attié - Laboratoire d’Aérologie (Toulouse), Edwards-NCAR 10th Anniversary Conference of the M-55 Geophysica

  6. High CO in LS from MOZAIC CO data High CO (> 250 ppb) in LS downwind of Siberia From Nedelec et al., 2005 10th Anniversary Conference of the M-55 Geophysica

  7. PyroCb Produced by the intense heating of the air from the surface and the convection it causes, usually in the presence of heavy moisture, from volcanic eruptions, forest fires, and occasionally industrial activities 10th Anniversary Conference of the M-55 Geophysica

  8. Fromm et al. JGR 2005 10th Anniversary Conference of the M-55 Geophysica

  9. 10th Anniversary Conference of the M-55 Geophysica

  10. Transport into the overworld Jost et al. GRL 204 10th Anniversary Conference of the M-55 Geophysica

  11. Trentmann et al. ACPD 2006 10th Anniversary Conference of the M-55 Geophysica

  12. rationale Storms form that often penetrate the local tropopause and send ashes through the tropopause to reach lower stratosphere Satellite images and data analysis show that sometimes ashes can reach very high into the stratosphere (e.g., Fromm et al., 2005a,b). Also model simulations indicate that fires can send ashes through the tropopause into the stratosphere (Wang, 2003; Winterrath et al., 2003). Pyro-Cb phenomenon in high latitude regions is of special importance because one usually do not associate these regions with strong convective activities. High latitude sources cannot be ignored when considering global chemical transport. What are the implications of such cross-tropopause transport? 10th Anniversary Conference of the M-55 Geophysica

  13. 23 August 10th Anniversary Conference of the M-55 Geophysica Jul 5 Aug 4 Two primary blowups: Mike Fromm et al. (NRL)

  14. NOy partitioning in the polar summer lower stratosphere NO2 mixing ratio NO2/HNO3 ratio NOx/NOy ratio Observations largely disagree with the photochemical models in the lower stratosphere Influence on the aerosol burden (Dufour et al. ACP 2005) 10th Anniversary Conference of the M-55 Geophysica

  15. Chemistry and mixing of polar vortex remnants in summer after the vortex spring breakdown (Hess and Holton, JAS 1985; Durry and Hauchechorne, ACP 2005; Konoptka et al. Acp 2003, Orsolini et al 1998) 10th Anniversary Conference of the M-55 Geophysica

  16. Summer stratospheric flights over and around the pole. Why? Study the impact of pyro cumulus stratospheric injection on stratospheric chemistry Investigate the lifetime, spatial distributions dynamics and chemistry of the winter vortex remnants Refine our knowledge on summertime ozone destruction induced by gas phase chemistry from NOx (dominant in the polar cap) and HOx (enhanced in midlatitude intrusions) catalytic cycles. 10th Anniversary Conference of the M-55 Geophysica

  17. 10th Anniversary Conference of the M-55 Geophysica

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