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Stratospheric Air Sampled at the Stratospheric Air Sampled at the Surface at Mauna Loa Surface at Mauna Loa Observatory Observatory G.S. Dutton, S.J. Oltmans, E.A. Ray, F.L. Moore & Mauna Loa personnel NOAA/ESRL Global Monitoring


  1. Stratospheric Air Sampled at the Stratospheric Air Sampled at the Surface at Mauna Loa Surface at Mauna Loa Observatory Observatory G.S. Dutton, S.J. Oltmans, E.A. Ray, F.L. Moore & Mauna Loa personnel • NOAA/ESRL Global Monitoring Division • NOAA/ESRL Chemical Sciences Division • University of Colorado, CIRES

  2. Conventional wisdom: NOAA baseline observatory near the top of Mauna Loa. 3397 meters above sea level. Mauna Loa, Hawaii

  3. Day time up-slope conditions bring warm air up Mauna Loa and raises boundary layer. Mauna Loa, Hawaii

  4. Night time down- slope conditions bring upper free tropospheric air to the observatory. Mauna Loa, Hawaii

  5. MLO in situ CFC- -11 11 MLO in situ CFC Cooper, O.R., et al. (2005), Direct transport of midlatitude stratospheric ozone into the lower troposphere and marine boundary layer of the tropical Pacific Ocean, J. Geophys. Res., 110 , D23310, doi:10.1029/2005JD005783

  6. Stratospheric Intrusions May 2006 Stratospheric Intrusions May 2006

  7. Potential Vorticity May 5, 2006 Potential Vorticity May 5, 2006

  8. NCEP Potential Vorticity NCEP Potential Vorticity April 28 to May 28, 2006 April 28 to May 28, 2006

  9. Halocarbon in situ measurements Halocarbon in situ measurements Periods with poor precision excluded from analysis

  10. Continuous surface Ozone measurement started at Mauna Continuous surface Ozone measurement started at Mauna Loa in 1973. Loa in 1973.

  11. Day and Night Comparison Day and Night Comparison Asian pollution Upper trop, lower stratospheric air Local pollution

  12. Spring Time Spring Time

  13. Same tracer- tracer relationship as mid-latitude stratospheric air sampled via WB- 57 aircraft.

  14. Other trace gases Other trace gases N 2 O N 2 O CCl 4 CCl 4 CFC- -12 12 CFC Slope of correlation proportional to the lifetime of the molecule.

  15. Nocturnal Spring Ozone Nocturnal Spring Ozone Skewed to higher ozone last 3 years. Change in transport?

  16. Summary… UTLS air is sampled at MLO almost every Spring and early Summer. Surface trace gas measurements may show signs of changes in strat-trop exchange related to climate Stratosphere-Troposphere Analyses of Regional change. Transport (2008)

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