240 likes | 247 Vues
Ozone Observations Analyses on Eastern Island La Serena, 22 Nov. 2004. Juan Quintana Dirección Meteorológica de Chile juaquin@meteochile.cl. Presentation:. Introduction (Campaign 2003) Typical ozone sounding at Eastern Island Relevant processes atmospheric observed Conclusions. 1. 3.
E N D
Ozone Observations Analyses on Eastern Island La Serena, 22 Nov. 2004 Juan Quintana Dirección Meteorológica de Chile juaquin@meteochile.cl
Presentation: • Introduction (Campaign 2003) • Typical ozone sounding at Eastern Island • Relevant processes atmospheric observed • Conclusions
1 3 2 4
Climatological Aspects on Eastern Island Climatological Zonal Wind – Spring (Sep-Nov) Anticiclonic Vorticity and Subsidence
Ozonosondes: Esatern Island Period: 1995-2001 1500m
Ozonosondes: Esatern Island Period: 1995-2001 38 Soundings 15 Soundings 15 Soundings 6 Soundings Cluster groups 1, 2, 3 and 4
Conditions Surface 08 to 13 Nov. 2003 Eastern Island Tº Max. Tº Min.
Subtropical Jet Stream (m/s), 200 hPa Day 08 Day 09 Day 10 (m/s) Day 11 Day 12 Day 13
Sinoptic Configuration08 to 13 Nov. 2003 Geopotencial Height 500 hPa Día 09 Day 08 Día 10 Día 11 Día 12 Día 13 Source: NCEP/NCAR
Temperature (°C)
Tropospheric Ozone 09-13 Nov 2003 Potencial Temperature 09—13 Nov. 2003
Conclusions • Maximun Ozone Tropospheric is observed during Spring in low troposphere and high troposphere on Eastern Island. • Extratropical cyclones, troughs and Subtropical Jet Stream Intense (>25m/s) favor significant Stratosphere-troposphere exchange (STE). • Marine Boundary Layer (MBL) seems to play a role important in tropospheric ozone maximum.