Here is my personal weather outlook and corresponding analysis for Spring-Summer 2011, specifically for eastern Canada and focused on the Montreal area. This outlook can also be found on my Facebook homepage, but I had also wanted to share it here.

The introduction emphasizes the average weather patterns that were observed this past Winter, which is followed by the Spring-Summer 2011 outlook. Towards the end, you will find some statistics that broadly define what was previously described in the introduction.
*A near-average temperature and average to above average precipitation trend is possible for the Spring-Summer period in much of eastern Canada this year (more details below).
After the typical Winter season of 2010-2011 and Spring’s refusal to commence appropriately, many are curious as to what sort of weather patterns could be awaiting for the Spring to Summer 2011 period. For those of you who recall my prediction for this past Winter, I predicted a typical end-Fall to Winter season - that is, a Winter showing average to slightly below average temperatures and average to above average snowfall. This outlook did not necessarily imply a harsh Winter season by any means but rather a more Winter-like one. As compared to the previous Winter of 2009-2010, which was directed by strong El Nino conditions, it turned out that Winter 2011 was, as expected, quite the sharp contrast, where we had seen temperatures closer to average and snowfall that was well above the seasonal mean. For a closer examination and comparative analysis of Winter 2009-2010 versus Winter 2010-2011 for Montreal, please refer to the compiled statistics below following my personal “Spring-Summer outlook” section.
For this past season, we had markedly seen an increase in bitterly cold episodes (especially towards the end of January where consecutive overnight lows reached near -30 C), while major snowfall episodes (characterized as near 15 cm or more of
accumulating snow) also showed a defined increase from last year. Individually, many days, most notably in February, had appreciable snowfall. If we consider each of the Winter months in terms of monthly maximum and minimum temperatures (all monthly max and min temperatures averaged), values have been slightly above average (relative to 1971-2000 climatology). However, average daily maximums by themselves were conversely normal to slightly below normal. Therefore, the overall slightly above average temperature trend was attributed to the generally above average daily minimum temperatures, which was enough to offset the pattern exhibited by the daily maximums. At the very end, this was more of a Canadian-like Winter.
The borderline moderate-strong La Nina that had been in place was the basis of my predictions for this past Winter. La Nina conditions, again, are observed when sea-surface temperatures (SSTs) in the eastern and central equatorial Pacific decline to below average values (negative anomalies) to certain thresholds and last for at least seven consecutive months. As represented in the ENSO (El Nino Southern Oscillation) models, this La Nina phase, however, has been rapidly dwindling through the Winter season, to the point where slightly above normal values (positive anomalies) have surfaced in the extreme eastern equatorial Pacific through February - this suggests that we could see a continued gradual weakening of La Nina during the Spring until near-neutral, though still slightly negative, conditions are present by this Summer. This rapid warming that had taken place in February was likely partly due to a strong Kelvin wave (as suggested by NOAA), which is a fast and enormous (large North-South extent) eastward propagating wave of warm water that travels along the equator from the western Pacific. The Kelvin wave seems to have been triggered by recent activity associated with the MJO (Madden Julian Oscillation), which is the common mechanism that generates these waves. In either case, a waning La Nina transitioning to near-neutral conditions is likely going to have at least some effect on our weather this Spring and Summer. Despite this current weakening, though, it is to my belief that La Nina’s influence will continue to have a grasp on the Spring to Summer period this year. As such, this is what I think could occur as far as temperature and precipitation are concerned:
Spring-Summer 2011 outlook
Temperature
In general, I don’t believe that both Spring and Summer 2011 will be as warm as what we had witnessed last year in 2010. Given the average jet stream configurations associated with the oceanic temperature patterns in the eastern and central equatorial Pacific, a weakening La Nina tends to produce a Spring that has average to slightly below average temperatures (in terms of average monthly daily maximums) for April to most of June. From the end of June through to August, it is with a fair likelihood that monthly temperatures could follow similar average tendencies, though a potentially warm August (under the assumption that a developing El Nino forms later in the Summer) is possible. This overall average temperature pattern suggests fewer heat waves and a reduction in days reaching 30 C or more as compared to Spring-Summer 2010, likely because of a more southerly-bound subtropical jet stream towards eastern Canada. I hope that my temperature assessment is largely incorrect, so that we receive a very warm Summer!
Precipitation
Predicting precipitation is always much more of a challenging task than it is for temperature for any given year. Previous years that entailed a transition from La Nina to near-neutral conditions in time for the Spring-Summer period have expressed considerable variability in rainfall from one year to another, especially for the Summer. That said, Spring precipitation has a tendency to be average to above average running from April to June, and it is possible that Spring 2011 could follow a similar pattern – this is, in part, because of the current moisture-rich soil surface (after a fairly snowy Winter) contributing to an increase in evaporation, and, therefore, an increased probability for enhanced precipitation. Thunderstorms may also contribute to the potentially above average rainfall mid-way to later in the season. It is equally probable that Summer 2011 could trace this trend, though more closer to average. Precipitation abundance is largely governed by the track of the jet stream, but if the subtropical jet stream maintains La Nina-like configurations and remains strong (and, therefore, more variable), it could signify a slight increase in severe weather in southern Ontario, southern Quebec and the U.S northeast because of increased directional and speed wind shear (winds that change in direction and speed with increasing altitude) in these regions, particularly from the end of June spanning towards mid August. Depending on the number of thunderstorms received, this could mean significantly more or less monthly rainfall at a local scale, simply because of the stochastic nature of thunderstorms.
Closing comments
To briefly synthesize the above, given the average atmospheric setup in response to a weakening La Nina, overall, we could see an average to below average temperature regime for Spring 2011, while precipitation follows an average to above average pathway. Summer 2011 could display monthly temperatures and rainfall that are about average, though monthly temperatures (in terms of daytime highs) could, at times, be slightly below average. Going a little further, some of the models are currently indicating that the equatorial Pacific could maintain ENSO-neutral conditions to even possibly weak El Nino configurations by the end of Summer. If neutral conditions are observed by that point in time, we can expect an average to slightly above average Atlantic and eastern Pacific hurricane season. Alternatively, if El Nino conditions develop and persist, then this activity would be below average with respect to total named storms. Kelvin waves, especially strong Kelvin waves, are believed to sometimes initiate an El Nino event following the warming in the eastern equatorial Pacific directly caused by the waves, so if an El Nino, even if weak in nature, does in fact form by late Summer and persists thereafter, it could signal a more forgiving end-Fall to Winter period (2011-2012), or, at the very least, for the duration of the first half of the Winter. All that said, large uncertainties exist in the models as to the overall status of the equatorial Pacific SST anomalies beyond Summer 2011, so it is still clearly something that needs to be closely monitored in the coming months.
I believe that there will be a fairly active tornado season in the U.S Midwest and southeast from April to June and for the northeast from later June to August. Tornado activity has already taken an unusually early active start this year in the U.S. Both El Nino and La Nina do not generate tornadoes themselves, but they can shift their overall geographic distribution because of differences in the average location of the jet stream when they are present. However, recent studies have suggested that La Nina years have a tendency of promoting more active and enduring tornado seasons, though these findings are inconclusive, principally because of the relatively short and inconsistent climate data records currently available to work with.
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Here are some statistics that I've tabulated to summarize a little of what was described above. The figures essentially serve to make a comparative analysis between Winter 2009-2010 and Winter 2010-2011 in order to see the contrast between the two very different seasons – you will see that, with the exception of December, these two seasons virtually mirrored each other. Particularly noticeable is how much degrees centigrade warmer January-March 2010 was as compared to January-March 2011. “Actual” temperature and precipitation values are compared for each month for the 2009-2010 and 2010-2011 seasons – that is, relevant figures for both seasons are separated by a “/” (read as 2009/2010 values for December and 2010/2011 values for the following months where applicable) for a given attribute for each respective month. Note that March has an extra figure that I threw in (represented by a “*”) showing the number of days reaching 10 C or more for the month in 2010 and 2011. “Normal” monthly values are reflected upon 1971-2000 climatology for the Montreal area.
December (2009 vs. 2010):
Normal December snowfall: 48.3 cm
Actual snowfall: 56.4 cm/70.6 cm
Monthly normal temperature (all daily maximums and minimums averaged): -6.3 C
Actual monthly average temperature (all daily maximums and minimums averaged): -5.4 C/-5.8 C
Monthly normal daily maximum: -2.2 C
Actual monthly average daily maximum: -2.1 C/-2.7 C
Normal average monthly snow depth: 8 cm
Actual average monthly snow depth: 10.5 cm/ 7.5 cm
Highest snow depth: 18 cm/13 cm
Number of days with a daily maximum at or above 0 C: 14/8
Highest daily maximum temperature: 8.1 C/12.6 C
Coldest daily minimum: -18.7 C/-21.6 C
January (2010 vs. 2011):
Normal January snowfall: 44.8 cm
Actual snowfall: 52.5 cm/33.0 cm
Monthly normal temperature (all daily maximums and minimums averaged): -10.4 C
Actual monthly average temperature (all daily maximums and minimums averaged): -6.4 C/-9.5 C
Monthly normal daily maximum: -5.7 C
Actual monthly average daily maximum: -3.2 C/-6.1 C
Normal average monthly snow depth: 15 cm
Actual average monthly snow depth: 10.5 cm/ 5.6 cm
Highest snow depth: 19 cm/9 cm
Number of days at or above 0 C: 10/3
Highest daily maximum temperature: 8.4 C/8.4 C
Coldest daily minimum: -21.4 C/-27.9 C
February (2010 vs. 2011):
Normal February snowfall: 43.3 cm
Actual snowfall: 47.8 cm/76.4 cm
Monthly normal temperature (all daily maximums and minimums averaged): -8.4 C
Actual monthly average temperature (all daily maximums and minimums averaged): -4.7 C/-7.6 C
Monthly normal daily maximum: -3.9 C
Actual monthly average daily maximum: -1.9 C/-3.2 C
Normal average monthly snow depth: 18 cm
Actual average monthly snow depth: 3.2 cm/19.1 cm
Highest snow depth: 8 cm/32 cm
Number of days at or above 0 C: 14/8
Highest daily maximum temperature: 4.6 C/9.6 C
Coldest daily minimum: -15.7 C/-19.0 C
March (2010 vs. 2011):
Normal March snowfall: 36 cm
Actual snowfall: 3.6 cm/43.2 cm
Monthly normal temperature (all daily maximums and minimums averaged): -2.3 C
Actual monthly average temperature (all daily maximums and minimums averaged): 3.3 C/-2.0 C
Monthly normal daily maximum: 2.2 C
Actual monthly average daily maximum: 7.8 C/2.5 C
Normal average monthly snow depth: 13 cm
Actual average monthly snow depth: 0.2 cm/7.3 cm
Highest snow depth: 2 cm/29 cm
Number of days at or above 0 C: 30/24
*Number of days at or above 10 C: 11/1
Highest daily maximum temperature: 15.7 C/11.2 C
Coldest daily minimum: -10.2 C/-20.4 C
Trav.
