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Climate Change Unpacked: What Caused the Texas Freeze?


As climate change continues to alter our atmosphere, extreme weather is becoming a more frequent occurrence across the world. From February 14 to 18, 2021, much of the U.S. experienced one of the coldest snaps on record. The National Weather Service reported frigid Arctic air and dangerously cold wind chills as far south as the northern Gulf Coast. This winter storm was an unusually cold event, with more than 1 in 6 housing units in the nation experiencing temperatures 40 degrees Fahrenheit below their respective averages.

Texas was hit especially hard, with over 4.5 million homes and businesses left without power for several days. The frigid temperatures and widespread power outages disrupted the water supply of over 12 million people. These combinations led to thousands of homes being impacted by frozen or busted pipes. Residents were even advised to boil their water before consumption due to lack of adequate water pressurization.

With so many people impacted, many are wondering: why did this bout of severe and unusually cold weather occur in the first place? To understand this, we first need to understand the nature of the Earth’s atmosphere.

The Polar Vortex

The Earth’s atmosphere is made up of many different layers. The stratosphere is the second major layer, above the troposphere and below the mesosphere. In the polar regions, the stratosphere is called the polar stratosphere. The polar stratosphere has a rapidly rotating region of cold air called the stratospheric polar vortex. During a year with normal winter conditions, the polar vortex is surrounded by the very strong winds of the jet stream, keeping it stable, more circular, and locked in the polar region.

But without these strong winds surrounding the vortex, the extremely cold air can escape and reach further south than before.

Figure 1: A graphic demonstrating the atmospheric drivers of the polar vortex[1]

The bout of extreme cold seen throughout the United States in February is linked to a meteorological phenomenon called Sudden Stratospheric Warming (SSW). This is when the polar stratosphere rapidly warms over the course of a few days, breaking down the jet stream winds that stabilize the polar vortex. Without these strong winds, the polar vortex begins to wobble, developing waves in the jet stream and spilling cold air southward across North America and parts of Asia and Europe.

Figure 2: The mean temperature departures from the 20th century average in February 2021[2]

In February, after the polar vortex broke apart, a piece of the polar low sat near the U.S.-Canada border. This polar low traveled further south than usual and allowed for this prolonged episode of cold air to take place.

The Impact

This phenomenon led to some of the coldest air that Texas has seen in the last 30 years and a snowpack, or snow-covered ground, that went from the U.S.-Canada border down to Texas.

There is still a lack of consensus within the scientific community on the relationship a warming climate will have with the occurrence of SSW events going forward.[3] However, many models have indicated that the occurrence of SSW events may increase.[4] [5]

It is becoming more critical than ever for insurers, regulators, construction contractors, utilities, and infrastructure to account for the changing climate and its unique challenges. Insurers, with their ability to provide a backup plan for when extreme events occur, have an important role to play when it comes to protecting the homes that we love. By incorporating the latest climate science and hazard models into their underwriting processes, insurers can be better prepared to help their policyholders in the face of more severe natural catastrophe events.

©2021 CoreLogic, Inc., All rights reserved.

[1] https://www.climate.gov/sites/default/files/PolarVortex_Feb2021_large.jpg

[2] https://www.ncdc.noaa.gov/monitoring-content/sotc/national/grid-temp/tave-anom-202102.png

[3] https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019JD032345

[4] https://journals.ametsoc.org/view/journals/clim/30/21/jcli-d-17-0044.1.xml

[5]https://scholarworks.sjsu.edu/cgi/viewcontent.cgi?referer=https://www.google.com/&httpsredir=1&article=8344&context=etd_theses

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