JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS09] [EE] Stratosphere - Troposphere Interaction

Wed. May 24, 2017 1:45 PM - 3:15 PM 303 (International Conference Hall 3F)

convener:Nawo Eguchi(Kyushu University), Rei Ueyama(NASA Ames Research Center), Sean M Davis(NOAA Boulder), Seok Woo Son(Seoul National University), Chairperson:Rei Ueyama(NASA Ames Research Center), Chairperson:Leonhard Pfister(NASA Ames Research Center), Chairperson:Nawo Eguchi(Kyushu University)

2:30 PM - 2:45 PM

[AAS09-16] Do stratospheric ozone measurements show large tropical width changes?

*Sean M Davis1,2, Birgit Hassler3, Karen H Rosenlof1 (1.NOAA Earth System Reserach Laboratory (ESRL), 2.Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado at Boulder, 3.Bodeker Scientific)

Keywords:Stratosphere, Tropical width, Tropical widening, Ozone, Satellite measurements

The total column ozone amount varies with latitude, in part due to the difference in tropopause height between the tropics and midlatitudes. This dependency of column ozone on latitude has been exploited by several studies to identify tropical edge latitudes and to compute their trends. The tropical widening trend over the past several decades from this method is greater than 3° latitude decade-1, a rate which is significantly larger than most other tropical widening estimates.

We assess the robustness of the previously used methodology by comparing it to a new objective gradient-based method of total column ozone. The total column ozone methodologies are then compared to a diagnostic based on vertically resolved satellite ozone data from the Stratospheric Water and OzOne Satellite Homogenized (SWOOSH) data set. Our results indicate a general lack of robustness of the previous estimates, and are more in line with other tropical widening estimates indicating poleward expansion rates of < 1° latitude decade-1.