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The two major Canadian cities that fall outside the continental climate schema are Vancouver and Victoria. Vancouver experiences an oceanic climate, bordering warm-summer mediterranean with a marked summer dry season. Victoria, BC is the only major Canadian city entirely in a warm-summer mediterranean climate.
The World Urban Database and Access Portal Tools (WUDAPT) is a global initiative of tools to create local climate zone maps for a given city using a standard methodology. [1] It has both a database and a portal. The database has hierarchical layers of increasing detail, with data acquired via crowdsourcing methods such as Geo-Wiki. [2]
The Gulf and South Atlantic states have a humid subtropical climate with mostly mild winters and hot, humid summers. Most of the Florida peninsula including Tampa and Jacksonville, along with other coastal cities like Houston, New Orleans, Savannah, Charleston and Wilmington all have average summer highs from near 90 to the lower 90s F, and lows generally from 70 to 75 °F (21 to 24 °C ...
However the higher elevations of the Laurentian Mountains and the northern Appalachian Mountains in Canada constitute the Eastern Canadian forests ecoregion. The region has a humid continental climate (Dfb) consisting of warm summers and cold, snowy winters, and is warmer towards the south. [2]
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Province Extreme Rainfall Location Maximum Daily Rainfall (mm) Date British Columbia Ucluelet 489 1967-10 Yukon Quiet Lake 91 1972-7 Alberta Eckville
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Generally, Kelowna is the transition zone between the drier south and the wetter north. The Okanagan north of Kelowna has a humid continental climate (Köppen: Dfb) with warm, sometimes hot summers and cold winters with highs around freezing, though mild by Canadian standards. Precipitation is well distributed year round.