In June 2022, a team of atmospheric scientists conducted a study in New Mexico, utilizing the ER-2 high-altitude aircraft to collect data on wildfire smoke in the upper troposphere. The researchers found that the smoke from intense wildfires can persist in the atmosphere for weeks or months, forming large particles through a process known as coagulation, where smaller particles combine to form larger ones. These large smoke particles were discovered to increase outgoing radiation by 30-36%, resulting in a cooling effect on the atmosphere. The study's findings are particularly notable, as current climate models do not account for these large particles, highlighting the need for further research and refinement of these models.
The discovery of these large smoke particles is closely related to the formation of pyrocumulonimbus thunderstorms, a type of weather system created by intense wildfires. These storms can inject smoke and aerosols into the upper troposphere, where they can persist for extended periods and have a significant impact on the climate. The researchers' use of the ER-2 aircraft allowed them to collect direct measurements of the smoke particles in the upper troposphere, providing valuable insights into the behavior and effects of these particles.
The significance of this discovery extends beyond the field of atmospheric science, with implications for the broader aerospace industry. As climate models are refined to account for these large smoke particles, they will become more accurate and reliable, allowing for better prediction and mitigation of the effects of wildfires on the environment. Additionally, the study's findings highlight the importance of continued research and development in the field of atmospheric science, particularly in relation to the impact of human activities on the climate.
The use of advanced aircraft like the ER-2, which can collect data at high altitudes, is crucial for studies such as this one. The data collected by these aircraft can provide valuable insights into the behavior and effects of aerosols and other particles in the upper troposphere, allowing researchers to refine their models and make more accurate predictions about the impact of wildfires and other environmental phenomena on the climate.
In conclusion, the discovery of large smoke particles formed by wildfire smoke in the upper troposphere is a significant finding with important implications for climate modeling and our understanding of the impact of wildfires on the environment. Further research and refinement of climate models will be necessary to fully account for these particles and their effects, but the study's findings represent an important step forward in our understanding of the complex relationships between wildfires, aerosols, and the climate.