Evidence for the Predominance of Mid-Tropospheric Aerosols as Subtropical Anvil Cloud Nuclei

Author:

Fridlind Ann M.12345,Ackerman Andrew S.12345,Jensen Eric J.12345,Heymsfield Andrew J.12345,Poellot Michael R.12345,Stevens David E.12345,Wang Donghai12345,Miloshevich Larry M.12345,Baumgardner Darrel12345,Lawson R. Paul12345,Wilson James C.12345,Flagan Richard C.12345,Seinfeld John H.12345,Jonsson Haflidi H.12345,VanReken Timothy M.12345,Varutbangkul Varuntida12345,Rissman Tracey A.12345

Affiliation:

1. National Aeronautics and Space Administration (NASA) Ames Research Center, Moffett Field, CA 94035, USA.

2. National Center for Atmospheric Research, Boulder, CO 80307, USA.

3. Department of Atmospheric Sciences, University of North Dakota, Grand Forks, ND 58202, USA.

4. Lawrence Livermore National Laboratory, Livermore, CA 94552, USA.

5. Center for Atmospheric Sciences, Hampton University and NASA Langley Research Center, Hampton, VA 23681, USA.

Abstract

NASA's recent Cirrus Regional Study of Tropical Anvils and Cirrus Layers–Florida Area Cirrus Experiment focused on anvil cirrus clouds, an important but poorly understood element of our climate system. The data obtained included the first comprehensive measurements of aerosols and cloud particles throughout the atmospheric column during the evolution of multiple deep convective storm systems. Coupling these new measurements with detailed cloud simulations that resolve the size distributions of aerosols and cloud particles, we found several lines of evidence indicating that most anvil crystals form on mid-tropospheric rather than boundary-layer aerosols. This result defies conventional wisdom and suggests that distant pollution sources may have a greater effect on anvil clouds than do local sources.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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