Convective Discussion
Two different convective initiation scenarios are envisioned today. North of the Maritimes, thunderstorms will form in an area of surface convergence ahead of a cold front analyzed from western Quebec to the Saguenay to Baie-Comeau. Based on the 12utc soundings from Sept-Isles and Maniwaki, the most energy available in this area is roughly 800-1200 J/kg which should be enough to push cumulonimbus development up to about 30,000 feet. The upper support points to multiple cells, and supercells are not out of the question given the available moisture and wind profile.
Over New Brunswick and Maine, a moisture-rich airmass with dew point temperatures in excess of 20 will probably generate isolated thunderstorms. Very warm surface temperatures will be required to over-come the low level stability, however, with a temperature of 31 and a dewpoint temperature of 22 the available energy spikes to 1,000 J/kg and pure convection develops leading to cumulonimbus with top near 40,000ft erupt. The storms are more likely to be widespread and stronger west of the region (i.e. over Maine)
Over Newfoundland, the airmass is becoming increasingly more humid over Newfoundland with dewpoint temperatures now reaching 17 or 18 in the southwest. A 30knot low level jet will push this moisture to other areas of the island during the afternoon however due energy available development will be limited to TCU and ACC clouds. Further north over Labrador, a low pressure system will maintain a vast area of cloud and rain.
Regional Impacts
Nova Scotia, PEI, Newfoundland and Labrador : No impacts expected
New Brunswick : Risk of isolated thunderstorms mostly north of a line from southeastern Maine to Miramichi. The development, if any, will occur during the middle to later part of the afternoon. Brief downpours and strong wind gusts are the main threat. Stronger cells are more likely to develop over area adjacent to the St. Lawrence valley and over southern Maine (North and West of NB)
Jean-Marc




