1 / 16

The dynamical signal in stratospheric temperatures from satellites

The dynamical signal in stratospheric temperatures from satellites. Changes and interannual variability (1979-2005). Paul J Young 1,2 , S Solomon 1 , D W J Thompson 3 , K H Rosenlof 1 , J-F Lamarque 1,2,4 , S C Sherwood 5 , Q Fu 6.

saman
Download Presentation

The dynamical signal in stratospheric temperatures from satellites

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. The dynamical signal in stratospheric temperatures from satellites Changes and interannual variability (1979-2005) Paul J Young1,2, S Solomon1, D W J Thompson3, K H Rosenlof1, J-F Lamarque1,2,4, S C Sherwood5, Q Fu6 (1) NOAA-ESRL, (2) CIRES-CU, (3) CSU Fort Collins, (4) NCAR, (5) U. NSW, Aus. (6) U. Washington Thanks to Craig Long and Roger Lin (NOAA - data); Bill Randel & Fei Wu (NCAR - data); Eric Ray, Bob Portmann, Sean Davis (NOAA - discussions)

  2. Outline • Dynamical(Brewer-Dobson) temperature signal • The MSU/SSU temperature data • Horizontal patterns and interannual variability from Brewer-Dobsoncirculation • Long-term changes and the B-D circulation • Summary

  3. COOLS HEATS Opposite-sense anomalies from stronger/weaker than average How do we get a dynamical temperature signal? Holton et al. 1995

  4. Annual temperature cycle - Asymmetric wave driving = maximum wave driving (NH winter) (> 30°S/N) Ann cycle in extratropics (50%)… …balanced in tropics (50%) (30°S – 30°N) MSU T4 analysis from Yulaeva et al. 1994

  5. Temperature data: MSU and SSU Microwave/Stratospheric sounding units Monthly/zonal mean anomalies, 1979-2005 Tropical tropopause Polar tropopause Randel et al. 2009

  6. Horizontal patterns and interannual variability (De-trended data)

  7. Winter correlations: Spider on the mirror High lats (>50N) and tropics High lats (>50S) and tropics NH, DJF SH, JJA SSU 27 SSU 26 SSU 25 MSU T4 1979 2005 1979 2005 Individual signals of SH 2002 winter, ENSO, others….? Young et al. in prep

  8. Out-of-phase in hemispheric winter (B-DC signal) In-phase in NH summer (weak in SH summer) Tropics-S/N Pole correlations by month Local correlation with… > 60° N > 60° S SSU 27 SSU 26 Altitude SSU 25 MSU T4 Young et al. in prep

  9. Brewer-Dobson circulation signals 1979-2005 See also Fu et al. (in review) for MSU discussion

  10. ? ? = B-DC strengthening? = B-DC weakening? Tropical/extratropical linear trends, 1979-2005 SSU 27 Changes in Tropics and extratropics balance adiabatic process SSU 26 Altitude SSU 25 MSU T4 April  May Young et al. in prep

  11. B-DC seasonality change / weakening B-DC strengthening B-DC strengthening Ozone-related cooling SSU 27 SSU 26 Altitude SSU 25 MSU T4 Young et al. in prep

  12. Consistency with radiosonde trend Young et al. in prep

  13. Summary • Wintertime B-D signal clear through the vertical • “Seasonal memory” in NH summer? (model?) • Satellites/radiosondes & adiabatic arguments change in strength/seasonality of B-DC over last ~30 years • Evidence for long term tendency? Still looking at decadal patterns, but appears winter strengthening is robust

  14. Extras – “seasonal memory”

  15. Summer correlations: “seasonal memory”? Temperature data Ozone data Subtract F10.7cm regression

  16. Summer correlations: “seasonal memory”? Temperature data Ozone data High lat-tropical T correlation from ozone? O3 anomalies persist through, e.g., NOy transport (Tegtmeier et al. 2008) Subtract F10.7cm regression

More Related