As we had expected, smoke that is aloft in the atmosphere and was headed our way this morning is finding its way to the surface in areas of Colorado. In this scenario, the vertical mixing of the atmosphere is both hurting and helping us.
The low-level turbulence caused by warming daytime temperatures and our abundant Colorado sunshine, and its contrast with the relatively cooler air above the surface, is helping to draw smoke downward and is resulting in increases in particle pollution measured by surface monitors. Yet it is this same motion in the atmosphere that is creating a bank of cumulus clouds along the foothills. As the clouds move east off of the higher terrain, cooling is caused by cloud interactions with their surroundings, and helps to produce localized areas of sinking air that spreads out radially once it hits the ground. These areas of breezy outflow winds are helping to limit the overall impacts of the smoke, and are expected to help disperse surface concentrations as the afternoon progresses. Additionally, the clouds help to reduce the amount of surface heating, and decrease the vigor of up-and-down drafts, potentially limiting the amount of smoke that can be drawn down to surface level.
In addition to all of this, the dense plume of smoke that is the root of the issue continues to be fairly discrete, and is moving through the region... with emphasis on the word 'moving.'
The smoke drifting through northern Colorado in 2024 serves as a stark reminder of the ongoing wildfire challenges we face. Air quality is significantly affected, urging residents to stay informed and take precautions. It's crucial to prioritize health and safety during these events. Let’s continue to support efforts in fire prevention and recovery to protect our beautiful state.
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