Temperature inversions to blame for Yampa Valley’s negative temps, dense fog | CraigDailyPress.com

Temperature inversions to blame for Yampa Valley’s negative temps, dense fog

Eleanor C. Hasenbeck/Steamboat Pilot & Today

Frost clings to the spokes of a vintage bike hanging on the front of the Wheels Bike Shop in downtown Steamboat Springs on Monday morning. The week got off to a cold start with temperatures dropping well below zero in the area overnight on Sunday.

STEAMBOAT SPRINGS — Early risers woke up to chilly temperatures Monday morning. The National Weather Service in Grand Junction documented a morning low of -13 degrees Fahrenheit just before 6 a.m. Monday in Steamboat Springs.

The cold temperatures are due to recent temperature inversions, in which the air at the earth’s surface is colder than the air higher in the atmosphere.

Inversions are common in river valleys, such as the Yampa Valley, according to local meteorologist Mike Weissbluth, who runs snowalarm.com.

“River basins tend to be good traps for cold air,” he said. “In the winter especially, there are other factors that help cold air pool near the surface.”

Fresh snowfall followed by a clear, dry evening contribute to inversions in multiple ways. Snow is efficient at radiating its temperature, so a clear, cold night can become even colder.

AT A GLANCE

Temperature inversions can impact air quality. To see current local air quality conditions and learn more about how air pollution can impact your health, visit http://www.co.routt.co.us/160/Air-Quality.

On a sunny, clear day, the snow reflects the sun’s heat, instead of absorbing it. In winter, the sun’s rays are weaker — its low angle in the sky doesn’t heat up the earth as much as it does in the summer.

Recommended Stories For You

Cloud cover can also help break up an inversion. Weissbluth said clouds act as a thermal blanket over the ground, which “blocks the strong cooling from the snow surface.”

All of these contribute to persistent cold temperatures in the valley.

Cold air holds less moisture than warm air. As temperatures fall in the evenings, the air squeezes that moisture out into the dense, frozen fog that socked in the Yampa Valley on Sunday evening. This also can create low-lying clouds at the top of the cold air dome, called a stratus layer. From the ground, this appears as a fog that hangs just above the earth.

“If you’re not actually driving through the cloud, if it’s not foggy — that’s a stratus cloud,” he said.

Because inversions trap air in valleys, they can also create pockets of denser air pollution.

Routt County Environmental Health Director Scott Cowman said he believes recent inversions have contributed to a slightly higher level of pollution in the air, though air quality in the Yampa Valley is still very good.

An air quality monitor at the Routt County Courthouse measures the air and color codes the air quality based on how many particles 2.5 micrometers or larger are in the air.

“We’re seeing higher readings,” he said.

“This is sort of what we expected — that when we do have these inversions and we trap the pollutants, that number goes up,” he added. “It’s proving true to what we’ve expected.”

Weissbluth anticipates that a storm rolling in on Tuesday evening could provide cloud cover and insulation that could break up the cold temperatures.

“I don’t expect strong winds with the storm on Wednesday, but temperatures in the valley will certainly warm because they're not going to get as cold at night,” he said.

A stronger storm is forecasted to hit at the end of the work week, and stronger winds will help “scour out” the inversion, he said.

“It physically mixes and forces those inversions to disappear,” he said.

It could also bring a few powder days — Weissbluth is calling for 6 to 12 inches of fresh snow from Thursday night through early Saturday.

To reach Eleanor Hasenbeck, call 970-871-4210, email ehasenbeck@SteamboatPilot.com or follow her on Twitter @elHasenbeck.