Explores the possible responses of local- and regional-scale weather phenomena to enhanced global radiative forcing associated with elevated greenhouse gas concentrations.
The economic and social costs of extreme weather events are often dramatic and are likely to increase in future climates. Improved information will produce better climate projections and weather forecasts, decrease our vulnerability to extreme events, and allow us to devise strategies to adapt to climate changes.
A consistent result in global climate model projections of future climate change is that the frequency of extreme precipitation events will increase, particularly over North America. Not yet established, however, is whether the projected extreme precipitation will be manifested as locally intense rainfall and flash flooding over several-hour periods.
Intersest in the organized part of turbulent flows has increased considerably over the last thirty years. This is particularly true in atmospheric convective boundary layers, where observed fields of coherent structures (CSs) are seen to evolve from a background of microscale turbulent fluctuations.