Despite our unusually cool, wet, and rainy springs in the Pacific Northwest the past few years, we still remember and cannot forget the record-breaking heat wave that blasted us in late June of 2021 elevating day- time temperatures 40 degrees higher than usual for early summer. This extraordinary event broke all-time records for the hottest temperatures in our region.
A nearly stationary, high-pressure system parked atop western North America for several days, blocking the easterly flow of weather systems typical for our region, forcing warm air downward and preventing sur- face heat from escaping into the upper atmosphere. This exceptional heat dome of parched, stagnant air remained trapped over northwestern North America for less than a week but pushed temperatures in Lytton, British Columbia, to 121°F, the highest temperature ever recorded in Canada, and to highs of 108°F in Seattle and 116°F in Portland, Oregon. These oven-like temperatures, in combination with profoundly low relative humidity, meant little evaporative cooling as well, further contributing to punishing high surface temperatures and desiccated soils. More than a year later, many of the scars and casualties of the daunting heat dome of 2021 remain.
Download John J. Albers’ and David Perry ‘s article published in the Conifer Quarterly
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