Wildfire smoke injection heights: Two perspectives from space

• Published in: Geophysical research letters Vol. 35; no. 4; pp. L04809 - n/a
• Main Authors: Kahn, Ralph A., Chen, Yang, Nelson, David L., Leung, Fok-Yan, Li, Qinbin, Diner, David J., Logan, Jennifer A.
• Format: Journal Article
• Language: English
• Published: Washington, DC American Geophysical Union 01.02.2008; Blackwell Publishing Ltd
• Subjects: Aerosols and particles; Atmospheric Composition and Structure; Atmospheric Processes; Constituent sources and sinks; constituent transport and chemistry; Earth sciences; Earth, ocean, space; Exact sciences and technology; Regional modeling; Remote sensing; remote sensing aerosol heights; smoke injection height; Troposphere; wildfire smoke; United States; Alaska; remote sensing aerosol heights; smoke injection height; wildfire smoke; atmosphere; models; strength; aerosols; plumes; boundary layer; sampling; Summer; accuracy; global; transport; troposphere; North America; buoyancy; Modeling; drill cores; fires; Radar observation; Lidar; Vegetation fire; Height; injection
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/2007GL032165

The elevation at which wildfire smoke is injected into the atmosphere has a strong influence on how the smoke is dispersed, and is a key input to aerosol transport models. Aerosol layer height is derived with great precision from space‐borne lidar, but horizontal sampling is very poor on a global basis. Aerosol height derived from space‐borne stereo imaging is limited to source plumes having discernable features. But coverage is vastly greater, and captures the cores of major fires, where buoyancy can be sufficient to lift smoke above the near‐surface boundary layer. Initial assessment of smoke injection from the Alaska‐Yukon region during summer 2004 finds at least about 10% of wildfire smoke plumes reached the free troposphere. Modeling of smoke environmental impacts can benefit from the combined strengths of the stereo and lidar observations.