when does it start to snow in nova scotia
Climate of Nova Scotia All of Nova Scotia has precipitation well distributed around the year, with a slight summer maximum in some northern/interior areas, but a slight fall to early winter (October to January) maximum in southern and coastal areas, where July or August is the driest month on average. Fall and winter storms, arriving in or near Nova Scotia from the U.S. Northeastern and New England states (called "nor'easters" in the US), often attain tremendous intensity across coastal areas, resulting in high winds, heavy rain, ice or snow and sometimes all of the above in a single storm. Average annual precipitation changes from 140 centimetres (55 in) in the south with its intense cold-season storm activity, to 100 centimetres (40 in) elsewhere. In the northeast, Sydney is an especially wet area, with an average annual precipitation of nearly 60 inches, with a noticeable fall to early winter (October to January) concentration, and December the wettest month on average. Nova Scotia is also very foggy in places, with Halifax averaging 196 foggy days per year[13] and Yarmouth 191.[14]
Daylight saving time in Canada In regions where daylight saving time is used, it commences on the second Sunday of March, and standard time restarts on the first Sunday in November.
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Ontario In the northeastern parts of Ontario, extending far as south as Kirkland Lake, the cold waters of Hudson Bay depress summer temperatures, making it cooler than other locations at similar latitudes. The same is true on the northern shore of Lake Superior, which cools hot humid air from the south, leading to cooler summer temperatures.[17] Along the eastern shores of Lake Superior and Lake Huron winter temperatures are slightly moderated but come with frequent heavy lake-effect snow squalls that increase seasonal snowfall totals upwards of 3 m (10 ft) in some places. These regions have higher annual precipitation in some case over 100 cm (39 in). The northernmost parts of Ontario – primarily north of 50°N – have a subarctic climate (Köppen Dfc) with long, severely cold winters and short, cool to warm summers with dramatic temperature changes possible in all seasons. With no major mountain ranges blocking sinking Arctic air masses, temperatures of −40 °C (−40 °F) are not uncommon; snowfall remains on the ground for sometimes over half the year. Snowfall accumulation can be high in some areas.[16] Precipitation is generally less than 70 cm (28 in) and peaks in the summer months in the form of showers or thunderstorms.[16]
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