The role of the ocean in extreme weather from subseasonal to decadal timescales

Session ID#: 281220

Session Description:
Extreme weather events are shaped not only by atmospheric dynamics but also by ocean conditions that evolve from subseasonal to decadal timescales. Variability in the upper ocean modulates sea surface temperature patterns and air–sea exchanges of heat, moisture, and momentum. These coupled processes can precondition the atmosphere, influence storm development and persistence, and affect the likelihood, intensity, and duration of extremes such as heatwaves, heavy precipitation, droughts, tropical cyclones, and compound coastal flooding. This session invites contributions that advance understanding of how upper-ocean processes and air–sea interactions modulate extreme weather and ocean phenomena at subseasonal, seasonal, interannual, and decadal timescales. We welcome observational, modeling, and theory-based studies, including process diagnostics, coupled predictability experiments, case studies of notable extremes, and evaluations of model physics and parameterizations. Contributions that link ocean states to specific extreme-event mechanisms, and that identify pathways for improved prediction and risk assessment, are particularly encouraged.
Co-Sponsor(s):
  • A - Atmospheric Sciences
Index Terms:

3372 Tropical cyclones [ATMOSPHERIC PROCESSES]
4504 Air/sea interactions [OCEANOGRAPHY: PHYSICAL]
4520 Eddies and mesoscale processes [OCEANOGRAPHY: PHYSICAL]
4572 Upper ocean and mixed layer processes [OCEANOGRAPHY: PHYSICAL]
Primary Convener:  Gregory R Foltz, NOAA Miami, Miami, FL, United States
Conveners:  Karthik Balaguru, PNNL, Marine Sciences Laboratory, Seattle, United States, Hyodae Seo, University of Hawaii at Manoa, Honolulu, United States and Cong Gao, Princeton University, Department of Civil and Environmental Engineering, Princeton, NJ, United States
See more of: Ocean Sciences