Comment on “Thermal infrared observations of a western United States biomass burning aerosol plume” by Sorenson et al. (2024)

Abstract. Sorenson et al. (2024) studied fresh smoke plumes from the proximal Dixie fire in northern California and concluded that the smoke cooled the air and Earth surface below the smoke by shielding of incoming solar radiation. The so-attributed cooling was immediate, sudden and on par with diurnal temperature variations. This comment takes issue with their conclusions, reasoning, and method. By examining the same case and others, it is shown that the observed cooling within the smoke plume is caused by plume particulates sufficiently large to intercept and thereby alter upwelling thermal infrared radiation. The evidence presented is the same satellite and radar data employed by Sorenson et al. (2024), but expanded with temporal animations. A key element of the new analysis is the demonstration of smoke-associated cooling at nighttime, a circumstance decoupled from the solar-shielding explanation. The refutation of the proposed solar-shield-cooling in fresh smokes is an essential refinement of the constraints on the radiative cause-effect in such conditions.

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Publication Details

Journal
Atmospheric chemistry and physics
Published
2026-01-09
DOI
https://doi.org/10.5194/acp-26-515-2026
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
0.00

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Comment on “Thermal infrared observations of a western United States biomass burning aerosol plume” by Sorenson et al. (2024)

Michael D. Fromm
Atmospheric chemistry and physics
Atmospheric aerosols and clouds
article

Comment on “Thermal infrared observations of a western United States biomass burning aerosol plume” by Sorenson et al. (2024)

Michael D. Fromm
article en

Abstract

Abstract. Sorenson et al. (2024) studied fresh smoke plumes from the proximal Dixie fire in northern California and concluded that the smoke cooled the air and Earth surface below the smoke by shielding of incoming solar radiation. The so-attributed cooling was immediate, sudden and on par with diurnal temperature variations. This comment takes issue with their conclusions, reasoning, and method. By examining the same case and others, it is shown that the observed cooling within the smoke plume is caused by plume particulates sufficiently large to intercept and thereby alter upwelling thermal infrared radiation. The evidence presented is the same satellite and radar data employed by Sorenson et al. (2024), but expanded with temporal animations. A key element of the new analysis is the demonstration of smoke-associated cooling at nighttime, a circumstance decoupled from the solar-shielding explanation. The refutation of the proposed solar-shield-cooling in fresh smokes is an essential refinement of the constraints on the radiative cause-effect in such conditions.

Atmospheric chemistry and physicsVol. 26(1)
United States Naval Research Laboratory (US)
Office of Naval Research
Openalex Percentile: Top 95%
Atmospheric aerosols and clouds
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Comment on “Thermal infrared observations of a western United States biomass burning aerosol plume” by Sorenson et al. (2024) — Michael D. Fromm · Atmospheric chemistry and physics (2026) | TGRS Research Map | TGRS