- 2 days ago
- 6 min read
by Charlie Brown

July 29, 2026
Global warming is a global issue with global effects. Some of those effects are being felt regionally and locally. Solving the problem will require local, regional, state, and national action from individuals, companies, organizations, regulators, and legislators.
Increasing greenhouse gas concentrations upsets the overall global energy balance by reducing radiant energy loss to space and trapping it here on Earth. This causes accumulation of energy, warming, and climate change.
The data for Figure 1 illustrates that the local warming trend is consistent with global temperature warming. Blue temperature spikes are yearly differences from the baseline average temperature over the last 100-plus years.

The Climate Impacts Group at the University of Washington’s College of the Environment produced a comprehensive report (Mauger, et al., 2015) summarizing research on the likely effects of climate change on the lands, water and people of the Puget Sound region:
Looking to the future, the University of Washington’s Climate Impacts Group predicts that increased warming will result in more frequent and more severe climate change impacts in Washington.
Warming is causing glaciers in the North Cascades to melt. Declining glaciers have been measured and documented by the work led by Dr. Mauri Pelto, Science Director for the North Cascade Glacier Climate Project. From the Project’s web site:
All glaciers are losing mass rapidly and this has led to the retreat of all 47 glaciers we monitor, with five of those glaciers having disappeared. The reduction in volume and area is reducing summer contributions to streamflow.
Streamflow from glaciers, along with snowpack and rain, are the sources of water for residential, farming, and industrial applications. Warming temperatures and increasingly variable weather are affecting all three.
The “atmospheric river” event of November 2025 that flooded rivers in the Pacific Northwest, including the Nooksack, is one example of an extreme weather event made more probable by increasing temperature and evaporation in the Pacific Ocean and increasing variability in meteorological conditions. It followed another extreme rainfall and flooding event of the Nooksack in November of 2021, as well as another in November in 1990. The effect of global warming on the Nooksack is now well known, having been summarized in a nice 2-page “Quick Reference Guide for Local Decision Makers” by UW’s Climate Impact Group in 2018. This Guide describes the increased winter streamflow contributing to 100-year floods as well as reduced summer streamflow contributing to drought. A quick keyword search will produce more references on this topic that has been well-studied.
Despite the excess rainfall event last November on the western coast, western states have experienced drought and a very low snowpack during the winter of 2025-26. The USDA Natural Resources Conservation Services provides snowpack data illustrated in Figure 2 with Whatcom County at about 60% of the median snow water equivalent. That is better than most western states, which have values significantly less than 50% of the median.

The “heat dome” of June 2021 was an extreme event that was thoroughly studied by several researchers. An estimated 868 excess deaths were attributed to this event (White, et al., 2022). McKinnon and Simpson (2022) used advanced statistical analysis for variability of other regional temperature events, and modeling, to determine whether regional norms had shifted enough to explain the heat dome. Using the “Community Earth System Model version 2 Large Ensemble [CESM2-LE],” they concluded that “[i]n general, CESM2 can simulate temperature anomalies as extreme as those observed in 2021, but they are rare.”
In other words, science shows that extreme weather events such as floods, heat, and drought are becoming more common. And the use of probability statistics combined with sophisticated computer models has developed attribution science that links the probability of rare events, like extreme floods, heat, and drought, to causes that increase the probability of those events. (Swain, et al., (2020) provides an excellent primer of the developing science of attribution. A report on the subject recently was prepared by the National Academy of Sciences (2026).)
Another form of heat wave is ocean temperature. From 2014 to 2016 the Northeast Pacific experienced unprecedented warm temperatures that disrupted fisheries from Alaska to California. Of high concern is the threat of these heat waves to Chinook salmon, the primary food source for Southern Resident orca. Dr. Crozier, et al., (2021) found that not just warmer streams and rivers, that affect spawning fry and juvenile smolt, but also warmer open ocean threatens the survival of adult salmon. “Our results indicate that as one symptom of a changing ocean, rising SST (sea surface temperature) puts all of our study populations at high risk of extinction . . . .”
Wildfire risk is enhanced by drought, high temperature, wind, and the availability of fuel. Pine bark beetle infestations, enhanced by warm winters and trees that are stressed by drought, have created a vast amount of dead fuel in the region. Wind brings unhealthy smoke from wildfires in British Columbia to Whatcom County. While wildfires in central and eastern Washington are more common, western Washington is now seeing major wildfires more frequently. Recent major fires on the west side of the Cascades include the Bolt Creek fire near Skykomish in King County in 2022 and the Bear Gulch fire on the Olympic Peninsula in 2025.
In addition to the physical impacts, there are economic impacts due to preventing, repairing, and compensating for damage. Burke, et al., (2026) found that the damage cost from one ton of carbon dioxide (CO2) emissions will accumulate to $1,840 by 2100, far above the allowance pricing under the State’s carbon cap-and-invest program. The warming effect and cost are cumulative because CO2 emissions accumulate and last a long time in the atmosphere, having risen from 280 ppm before the industrial revolution to the current value of 430 ppm and rising. In addition, the concentration of methane (CH4), a greenhouse gas and is the primary component of natural gas, is increasing at a higher percentage rate than CO2. One ton of methane emission has about 80 times more global warming potential than one ton of CO2 emission over a 20-year period.
There are an increasing number of legal efforts to demand accountability. The 2021 PNW heat dome brought suits by Multnomah County, OR, and by the estate of Juliana Leon. Two separate suits in Washington are filed by the Makah and Shoalwater Bay Tribes. A key ruling in the case of Held v. Montana rejected the State's argument that greenhouse gases from Montana fossil fuel projects are minuscule on a global scale, so reducing them would have no effect on climate change. This concept of accountability proportional to contribution was also recognized by the Appeals Court of The Hague in Milieudefensie v. Shell. As reported by Tigre and Hesselman (2024), the international court “[e]stablished that companies have an obligation to reduce CO2 emissions and failing to take adequate reduction measures may constitute a violation of human rights and lead to liability.”
As greenhouse gas emissions continue and concentrations rise, the local and global effects and costs of global warming and climate change will get worse. It is well past time to pay attention to and act upon the solid science of global warming and the resulting effects of climate change.
References
Burke, et al, “Quantifying climate loss and damage consistent with a social cost of carbon,” Nature, March 2026.
Climate Impacts Group, “Climate Change in the Nooksack River: A Quick Reference Guide for Local Decision-makers,” University of Washington, 2018.
Crozier, et al., “Climate change threatens Chinook salmon throughout their life cycle” Communications Biology, Feb 2021.
Mauger, et al., “State of Knowledge: Climate Change in Puget Sound,” Climate Impacts Group, University of Washington, 2015.
McKinnon and Simpson, “How Unexpected Was the 2021 Pacific Northwest Heatwave?”, Geophysical Research Letters, 2022.
National Academy of Sciences, Engineering, and Medicine, “Attribution of Extreme Weather and Climate Events and Their Impacts,” 2026.
Pelto, “North Cascade Glacier Climate Project,” Nichols College, 2026. https://glaciers.nichols.edu/
Swain, et al., “Attributing Extreme Events to Climate Change: A New Frontier in a Warming World,” One Earth, June 2020.
Tigre and Hesselman, “Milieudefensie v. Shell: 3 Takeaways and Challenges on the Appeal’s Court Decision,” Sabin Center for Climate Law, Columbia Law School, Dec 2024. https://blogs.law.columbia.edu/climatechange/2024/12/12/milieudefensie-v-shell-3-takeaways-and-challenges-on-the-appeals-court-decision/
White, et al., “The unprecedented Pacific Northwest heatwave of June 2021,” Nature Communications, June 2022.





