GFDI 50th Anniversary Workshop
7th Floor Keen Building Seminar Room
May 15 and 16, 2017
DAY I: FLUID DYNAMICS OF THE ENVIRONMENT
8:30 Coffee and pastries
09:00 AM – 09:15 AM Welcome (K. Speer) and Background of GFDI (Dr. R. Pfeffer)
09:15 AM – 10:00 AM Dr. Peter Read (Oxford)
10:00 AM – 10:45 AM Dr. David Collins (Astrophysics)
10:45 AM – 11:15 AM Coffee Break
11:15 AM – 12:00 PM Dr. Bryan Quaife (Scientific Computing)
12:00 PM – 01:30 PM Catered Lunch on the 7th floor Keen
01:30 PM – 02:15 PM Dr. Neda Yaghoobian (Mechanical Engineering)
02:15 PM – 03:00 PM Dr. Jeff Chagnon (Meteorology/EOAS)
03:00 PM – 03:30 PM Coffee Break
03:30 PM – 04:00 PM Dr. Mathew N. Moore (Mathematics)
04:00 PM – 04:30 PM Closing remarks, poster viewing
Day 2: GROUNDWATER AND SURFACE WATER REACTIVE TRANSPORT
8:30 Coffee and pastries
9:00 Welcome - Dr. Ming Ye
9:30 Dr. Gang Chen (Civil and Environmental Engineering)
10:00 Dr. Ming Ye (Scientific Computing)
10:30 Dr. Jiazhong Qian (Visiting Professor from University of Nevada)
11:00 Dr. Tang (Civil and Environmental Engineering)
Posters put up the week before, available for viewing during lunch afternoon
“Water-mass characteristics, transport and tidal-induced mixing in the southwestern Mariana Trench”
Speaker: Dr. Hongzhou Xu
Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences
Time: Tuesday, October 11, 2016 at 1:00PM
Place: Melvin Stern Seminar Room, Room 18 Keen Bldg.
Refreshments will be served at 12:45PM
Identifications of water-mass characteristic and vertical mixing intensity can help oceanographers to better understand ocean circulation structures and transport processes in open oceans. They were recognized well by extensive observations and simulations in the upper ocean. Nevertheless, rare related studies were conducted in deep oceans, especially for deep trench range from 6,000 m to 10,000 m in depth. In this talk, two topics in the world deepest trench will be presented and discussed.
- Water-mass distributions and transport in the southwestern Mariana Trench of the northwestern Pacific Ocean by CTD dataset. The preliminary results show complex vertical structures of water mass in this trench. And the transport of AABW can reach about 2.5 SV which is much larger than previous studies.
- Simulations of internal tide and it-induced turbulent mixing in the trench by MITgcm numerical model. It can be found strong vertical mixing are motivated by interaction between internal tide and trench topography.
Illinois at Urbnan-Champaign before joining FAMU-FSU College of Engineering. His primary research interests lie in sustainable microbial processes in environmental engineering.