Smoking rain clouds over the Amazon.
نویسندگان
چکیده
Heavy smoke from forest fires in the Amazon was observed to reduce cloud droplet size and so delay the onset of precipitation from 1.5 kilometers above cloud base in pristine clouds to more than 5 kilometers in polluted clouds and more than 7 kilometers in pyro-clouds. Suppression of low-level rainout and aerosol washout allows transport of water and smoke to upper levels, where the clouds appear "smoking" as they detrain much of the pollution. Elevating the onset of precipitation allows invigoration of the updrafts, causing intense thunderstorms, large hail, and greater likelihood for overshooting cloud tops into the stratosphere. There, detrained pollutants and water vapor would have profound radiative impacts on the climate system. The invigorated storms release the latent heat higher in the atmosphere. This should substantially affect the regional and global circulation systems. Together, these processes affect the water cycle, the pollution burden of the atmosphere, and the dynamics of atmospheric circulation.
منابع مشابه
Interactive comment on “Aerosol concentrations determine the height of warm rain and ice initiation in convective clouds over the Amazon basin” by Ramon Campos Braga et al
Reviewer’s text: A strength of this paper is the presentation of cloud in-situ observations that addresses the question of how convective clouds are influenced by changing the concentration of aerosols. The authors have determined that the height of rain initiation given by D_i is approximately 5 * the number concentration of cloud droplets at cloud base, N_d. This type of study is needed for d...
متن کاملInteractive comment on “Aerosol concentrations determine the height of warm rain and ice initiation in convective clouds over the Amazon
A strength of this paper is the presentation of cloud in-situ observations that addresses the question of how convective clouds are influenced by changing the concentration of aerosols. The authors have determined that the height of rain initiation given by D_i is approximately 5 * the number concentration of cloud droplets at cloud base, N_d. This type of study is needed for developing paramet...
متن کاملManuscript review Further evidence for CCN aerosol concentrations determining the height of warm rain and ice initiation in convective clouds over the Amazon basin
This manuscript is a revised version of a previous submission. Although the content has been somewhat improved from the original version, it is still not ready to be released for publication until most of my previous comments are better addressed than they were in the authors’ original response. In addition, upon further evaluation of the paper, I have found other sections that need further cla...
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عنوان ژورنال:
- Science
دوره 303 5662 شماره
صفحات -
تاریخ انتشار 2004