A009-0008
Extreme Freezing Rain Events in the Province of New Brunswick, Canada, and their Evolution in the Future Using Convection-Permitting Simulations
Abstract:
Our analysis showed that extreme freezing rain accumulation in NB results typically from strong extra-tropical cyclones that form over southeastern US and travel toward Atlantic Canada. Also, the low-level wind field during individual freezing rain events showed that the presence of the Appalachian Mountains in NB enhances the differential temperature advection associated with veering winds through the process of cold air damming. This favors the development of strong temperature inversion in the lower-levels, which leads to an increase of freezing rain amounts in central NB. In the PGW climate projection, there is a major decrease of freezing rain event occurrence in the coastal regions of NB (southern and eastern NB), while it increases in northwestern NB, especially for long events (>6 hours). Overall, this study contributes to a better understanding of meteorological factors leading extreme freezing rain amounts in NB and to better anticipate the impact of climate change on those storms.