UMD AOSC Seminar

How Well Do We Know Recent Climate Trends at the Tropical Tropopause?

Dr. James Wang

National Oceanic and Atmospheric Administration
Air Resources Laboratory

The tropical tropopause, a transition layer between the troposphere and stratosphere, is important for global climate and atmospheric chemistry. Several studies have reported multi-decadal tropical tropopause cooling and have suggested a correlation between observed tropopause temperature and stratospheric water vapor. Water vapor changes have in turn been linked to changes in surface warming rates. Our more rigorous and thorough examination of the observations on which trend estimates are based, especially at the tropopause, shows these trends have greater uncertainty than previously suggested and the cooling may not even be statistically significant. We used two approaches to adjust cold-point tropopause (the point of minimum temperature in a vertical profile) trends based on radiosonde observations for time-varying biases. Our results are consistent with expectations based on a conceptual model of tropopause changes and could resolve discrepancies between complex climate models and observations

November 10, 2011, Thursday

Seminar: 3:30-4:30pm

Computer and Space Sciences (CSS) Building, Auditorium (Room 2400)
Refreshment is served at 3:00pm in the adjoining Atrium

[Contact: Dr. Phil Arkin]
[ AOSC | Seminar | Directions and Parking ]

AOSC 818. Frontiers in Atmosphere, Ocean, Climate, and Synoptic Meteorology Research