The unprecedented Pacific Northwest heatwave of June 2021

– By Cuiyi Fei, Rachel H. White, Chris Rodell – 

The extreme heatwave that occurred at the end of June 2021 across the Pacific Northwest region of North America was so unprecedented and impactful that it will likely continue to be studied for many years. In our cross-disciplinary study, led by researchers at the University of British Columbia (White et al. 2023), we summarize the conditions leading up to this record-shattering event, and provide insights into the impacts of such unprecedented heat. Understanding such events is particularly relevant in the context of our warming world.

The degree by which local records were broken during this heatwave is shown in Figure 1, with a comparison to two other notorious heatwaves: in Europe in 2003 and Russia in 2010. The Pacific Northwest heatwave broke 70-year temperature records by more than 6 degrees, making it far more unprecedented than most heatwaves (see also Thompson, et al., 2022). In fact, it became one of the most severe extreme weather events in the past decades around the world and broke the national temperature record of Canada by 4.6 degrees. Although the heatwave lasted only around five to six days, shorter than the other two events included in Figure 1, it was still devastating. The maximum heatwave temperature of 49.6C was reached in Lytton, a small town in an arid valley of BC, and much of the town of Lytton was tragically destroyed in a wildfire during the heatwave.

Figure 1. Exceedance of previous record high temperatures by the June 2021 Pacific Northwest heatwave (a), the July–August European heatwave of 2003 (b), and the July–August Russian heatwave of 2010 (c), Shading is re-analysis data (ERA5) from 1950; markers show individual stations with observational lengths of at least 71 years. Figure from White et al. 2023, Nature Communications.

Despite the unprecedented nature of the heatwave, our results show that record-breaking temperatures were successfully forecast at least three days before heatwave onset, consistent with previous work (Emerton et al., 2022). If we pull the perspective back to seven days before the heatwave, weather forecasts were able to predict a heatwave, although how extreme it would be was not clear. Even sub-seasonal forecasts initialized on June 7th showed an enhanced probability of atmospheric blocking, and associated high temperatures, although the forecast uncertainty at these timescales is significant.

Whilst no single comprehensive and quantitative theory can be universally applied to all extreme temperature events, heatwaves in summer can often be attributed to blocking highs — a high-pressure system that is stationary or propagating slowly. These blockings highs are often associated with subsidence, clear sky radiative warming and land-atmosphere feedbacks (Pfahl and Wernli, 2012), all contributing to high surface temperatures. The contribution of different factors varies from one event to another (Röthlisberger and Papritz, 2023). In the case of this heatwave, the preceding atmospheric conditions are shown in Figure 2, with a ridge and high mean sea level pressure just off the west coast of North America, which developed into a blocking pattern in the next few days. High upstream relative humidity (shown in the blue shading) provided latent heating from water vapor condensation, contributing to the anomalously high temperature and likely sustaining the high-pressure ridge (Oertel et al., 2023). Our findings demonstrate that approximately 78% (equivalent to around 14 degrees) of the near-surface temperature anomaly was due to the diabatic heating upstream of the blocking.

Figure 2. Meteorological conditions over the North Pacific for 00UTC 23 June. Data from ERA5 reanalysis showing: mean sea-level pressure (MSLP; contoured, hPa), 700 hPa relative humidity (RH; shaded, light blue >70%, dark blue >90%), and 250 hPa wind vectors (m/s, colored by wind speed). Coastlines and country borders are shown in black. Figure from White et al. 2023, Nature Communications.

The high temperatures of this heatwave, as illustrated in Figure 1, had a catastrophic impact on human health. A total of 868 deaths have, so far, been attributed to the heatwave, and emergency visits for heat-related illnesses in some impacted regions were 69 times higher compared to the same period in 2019.

Turning to the meteorological and oceanographic impacts, one direct consequence of the heatwave was a significant increase in wildfires. The number of wildfires in BC increased from six on June 20th before the heatwave to 175 on July 3rd, just after the heatwave, with the area affected by wildfires increasing by a factor of about 640 during this period. In addition to extremely high temperatures, the wildfires provided heat, smoke particles and water vapor for convective cloud formation. Upstream mid-troposphere moisture also had an indispensable contribution to the convective clouds. These convective clouds, in turn, produced a large amount of lightning, igniting and strengthening wildfires. According to the Canadian Interagency Forest Fire Centre (CIFFC), lightning triggered at least 127 wildfires from June 30th to July 2nd.

This event also had significant impacts on marine life, particularly intertidal species. Figure 3 shows thermal images of mussels and the rocky intertidal shoreline they were on. During the heatwave, the temperature of the rocks, as well as some of the mussels, exceeded 50°C, leading to significant deaths (as evidenced by the mussels gaping open). Such large-scale mortality occurred across various species from the southern end of Puget Sound, Washington State, to the BC Central Coast, with the total number of killed marine invertebrates almost certainly in the billions (Raymond et al., 2022).

Figure 3. Thermal images showing surface temperatures exceeding 50°C during low tide on 28 June, 2021, on a rocky intertidal shoreline (left) and within a mussel bed (right) in the vicinity of Vancouver, BC; the mussels in this picture have died and are gaping open. Scale bars indicate the range in temperature from the coolest to warmest parts of the image, while the value at the upper left indicates the temperature in the cross-hairs at the center. Figure from White et al. 2023, Nature Communications.

In addition to the direct temperature impacts, the extreme heatwave also increased streamflow in British Columbia by melting ice and snow. Figure 4 shows substantial peaks in streamflow coinciding with the heatwave in heavily or moderately glaciated basins (top and middle rows respectively), while areas with little glacier coverage (and therefore likely little snow cover) experienced minimal change during the heatwave (bottom row). After the heatwave, streamflow in areas with moderate or little glacier coverage was typically lower than climatological values (middle and bottom row). In contrast, the streamflow from glaciated basins remained close to the climatological average (top row); this was almost certainly achieved at the cost of potentially irreversible glacier mass loss. Managing water resources may be critical during and after extreme heatwaves in the future, as the ability of glaciers to sustain streamflow may diminish as glaciers continue to melt in response to climate change (Clarke et al., 2015).

Figure 4. Streamflow observations at nine stream gauge stations in 2021 (black line) relative to the 1979–2020 median (blue line) and one standard deviation range (shaded). Gauges are organized from top to bottom by basin glacier coverage: highly glaciated basins (a–c), lightly glaciated basins (d–f), and minimally or non-glaciated basins (g–i). See Supplementary Fig. S6 for the locations of these gauges. Figure from White et al. 2023, Nature Communications.

This unprecedented heatwave is a vivid example of a record-shattering mid-latitude heatwave, illustrating some potential effects of extreme heat. There is no doubt that increasing background temperatures due to anthropogenic climate change made this heatwave hotter and, therefore, more extreme; however, the recording-breaking temperatures of recent extreme weather events such as this heatwave are a combination of anthropogenic climate trends and internal variability that has always been able to cause large anomalies in temperature. Understanding of our complex interacting climate system remains incomplete and quantitative estimates of the contribution of anthropogenic factors to this heatwave have relatively large uncertainties due to the many interacting factors that may have played a role, including moisture and land-atmosphere feedbacks and possible anthropogenically-forced changes to atmospheric circulation patterns. Long-term adaptation in response to long-term climate change and the short-term response to extreme events have both overlapping and separate components (Dolan, 2021). To reduce the impacts of future heatwaves, it is imperative that we understand, mitigate, and adapt on both timescales.

While anthropogenic climate change was not the sole cause of this event, this heatwave presents an opportunity to enhance people’s awareness and preparedness. Even though many future extreme weather events may not be as unprecedented as this heatwave, it is undeniable that global warming will result in more record-shattering heatwaves in the future (Fischer et al. 2021). Hence, it is vital to take proactive measures toward climate adaptation, including building infrastructure, improving emergency response, and promoting sustainable strategies such as the use of clean energy in the industry, agriculture, and people’s daily lives. We must build resilience against extreme events and climate change for a safer and more sustainable future.

Cuiyi Fei is a PhD Candidate in the Department of Earth, Ocean and Atmospheric Sciences at University of British Columbia. She is working on understanding the mechanism of quasi-stationary waves, but she has a broad interest in general circulation in the atmosphere and ocean.

Rachel White is an Assistant Professor in Atmospheric Science in the Department of Earth, Ocean and Atmospheric Sciences at University of British Columbia. Her research interests include large-scale climate dynamics, connections between atmospheric circulation patterns and extreme weather events, and the subseasonal to seasonal predictability of extremes.

Chris Rodell is a PhD Candidate in Atmospheric Science at the University of British Colombia. His focus is on Fire Weather, Behaviour and Smoke forecasting.


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Emerton, R., Brimicombe, C., Magnusson, L., Roberts, C., Di Napoli, C., Cloke, H.L. and Pappenberger, F., 2022. Predicting the unprecedented: forecasting the June 2021 Pacific Northwest heatwave. Weather, 77(8), pp.272-279.

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Pfahl, S. and Wernli, H., 2012. Quantifying the relevance of atmospheric blocking for co‐located temperature extremes in the Northern Hemisphere on (sub‐) daily time scales. Geophysical Research Letters, 39(12).

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Thompson, V., Kennedy-Asser, A.T., Vosper, E., Lo, Y.E., Huntingford, C., Andrews, O., Collins, M., Hegerl, G.C. and Mitchell, D., 2022. The 2021 western North America heat wave among the most extreme events ever recorded globally. Science Advances, 8(18), p.eabm6860.

White, R.H., Anderson, S., Booth, J.F., Braich, G., Draeger, C., Fei, C., Harley, C.D., Henderson, S.B., Jakob, M., Lau, C.A., Mareshet Admasu, L., Narinesingh, V., Rodell, C., Roocroft, E., Weinberger, K.R., and West, G. 2023. The unprecedented Pacific Northwest heatwave of June 2021. Nature Communications, 14(1), p.727.

chris rodell, cuiyi fei, heatwave, pacific northwest, rachel white

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