Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol A (Atmospheric, Ocean, and Environmental Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS21_30AM2] Stratospheric Processes And their Role in Climate

Wed. Apr 30, 2014 11:00 AM - 12:45 PM 313 (3F)

Convener:*Kazuyuki Miyazaki(Research Institute for Global Change, JAMSTEC), Masakazu Taguchi(Aichi University of Education), Yoshio Kawatani(Japan Agency for Marine-Earth Science and Technology), Kaoru Sato(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Chair:Masakazu Taguchi(Aichi University of Education)

11:45 AM - 12:00 PM

[AAS21-10] Recent variability and zonal asymmetry in upper troposphere and lower stratosphere observed with GPS radio occultation m

*Sanjay MEHTA1, Toshitaka TSUDA1, Masatomo FUJIWARA2, Torsten SCHMIDT3, Jean-paul VERNIER4 (1.Research Institute for Sustainable Humanosphere (RISH), Kyoto University, Japan, 2.Faculty of Environmental Earth Science, Hokkaido University, Japan, 3.GFZ German Research Centre for Geosciences, Potsdam, Germany, 4.NASA Langley Research Center, Hampton, VA 23666, USA.)

Keywords:UTLS Temperature, Zonal Assymetry, GPS Radio Occultation, Moderate Volcanic Eruptions, Dynamical Changes

Tropical upper troposphere and lower stratosphere (UTLS) variability and zonal asymmetry are explored using global positioning system radio occultation (GPS-RO) measurements. GPS-RO offers global monitoring of fine structures of the UTLS temperature variability. GPS-RO continuous measurements from CHAMP (2001-2006) and COSMIC (2006-2013) for about 13 years allows us to study the interannual variability, trends (over the last decade) and its fine zonal structures. The warming of UTLS temperatures between 100 and 50 hPa, warming of tropopause and decrease in its height have been observed over the last decade. The possible reasons for such changes linking to the recent moderate volcanic eruptions and dynamical changes involving changes in sea surface temperature and Brewer Dobson circulation will discussed. The variability and structure observed in GPS-RO will be compared with existing conventional radiosonde and reanalysis datasets.