Hi Fred,
Thank you for sharing that. That thunder crash was also very loud at about 12:30 in the video link!
Indeed, that was a ferocious rainfall from the very late-afternoon to early-evening thunderstorm of July 28th. The formation of this very isolated thunderstorm event is consistent with my reasoning behind finding it necessary to keep the risk for rainfall and isolated thunderstorms active until just slightly after sunset, as mentioned in my previous three postings. In addition, I stressed that some of the thunderstorms that do develop in Saturday’s environment would be capable of torrential rains (see the “Precipitation” section above), owing to the high humidity concentration in the air. Indeed, Paul did mention previously how soaked he was after/during that torrential rain!
The historical radar imagery supplied (6:14 to 6:30 in the video) also highlights well the timing, how isolated the thunderstorm realistically was, and the narrow trajectory it followed. It was really the only thunderstorm in the general area at the time, which justifies the 30% probability assigned for any given location, just that the island, and areas to the SW and immediately East, happened to fall in the 30%!
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A broad area of low pressure and series of embedded shortwave troughs will be advancing into S. Ontario to S. Quebec for the day Wednesday, August 1st. These systems will progressively allow for tropical air to return to the regions, circulating warm and very moist conditions and, for the greater Montreal area, creating potentially the highest humidity levels of all fireworks days so far this year. At first, the system’s warm front and the first of several shortwave troughs will yield sufficient lift for increased cloudiness, isolated pre-dawn to lunch time convective rain showers, and sparsely-distributed non-severe thunderstorms. As the day progresses, the low’s cold front will become more important for the afternoon to evening period.
While thunderstorms and/or (heavy) convective rainfall are favorable to develop in this very humid environment, notably by the mid-afternoon, the extensive cloud coverage early in the day does cast some uncertainty as to how particularly severe thunderstorms may become later in the day (especially close to 9:00 p.m.). That being said, latest data does support breaks in the cloud deck by late-morning that would allow for some brief sunny periods into principally the early-afternoon, enhancing instability. Depending on how much solar heating unfolds, the risk for stronger thunderstorms will increase into the late-afternoon to evening period and so will need to be carefully monitored. The potential for a line of thunderstorms will be possible in a worst-case situation, which will increase the damaging wind threat locally. Note that thunderstorms, regardless of their severity, will, like on July 28th, likely be capable of torrential rains in this environment, and so local flooding will also be hazard with some thunderstorms later in the day. The stronger thunderstorms will also generate intense lightning. Mid- to late-afternoon and evening convective coverage, collectively, is expected to be widespread in this situation, so “at least” a 60% probability is favored (this may be upgraded to 80% for late-afternoon to evening period). The probability for strong to severe thunderstorms should be 40% at this point, but an increased probability will be contingent on the degree of solar heating. For these reasons, I suspect that severe thunderstorm watches will be re-introduced at some point on August 1st.
Another area of concern would be the richness of the humidity into the late-afternoon to evening period as the aforementioned warm front lifts North. At the same time, because of the dampness of the air, the air itself is expected to be almost completely saturated over a great tropospheric depth. This is likely to encourage thicker smoke build up from the fireworks and also reduce color richness/vibrancy. Wind speeds are shown to be somewhat light (9-12 km/h), and mostly from the SSW, although higher altitude smoke should move a little faster, but still gently, in the same direction. The wind direction and speed, thus, should help a little, but it seems that smoke accumulation could, at times, be accumulating faster than displacing clear to the right of the La Ronde audience. At the very least, the hazy display appearance should not be as extensive as it was during the American show. ***Note, however, that if thunderstorms or a strong convective rainfall does occur during and/or slightly before display time, then the local wind fields will likely become more Westerly, causing the smoke to move towards the La Ronde audience directly, and quickly due to the potentially strong downbursts of wind.
It is also uncertain to what extent smoke-rich products will be used in the Italian display, or how numerous active segments might be. I suspect this will be lesser in extent than in the American display, which could allow the smoke the time to clear sufficiently during times of lighter activity, but periods of extensive smoke accumulation will still be favored.
Since the air is virtually saturated, temperatures will not be liable to drop much into the evening. Depending on how much solar heating occurs, maximum temperatures of 29-30 C are favorable by mid-afternoon, with a humidex of 35-36 C. Late-evening values should be closer to 24-25 C (humidex of 33-34 C).
Another update to follow by either late-evening July 31st into pre-dawn August 1st.
Trav.
