Efficient In-Cloud Removal of Aerosols by Deep Convection
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2019
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Source Geophysical Research Letters, 46, 1061-1069.
Yu, P., Froyd, K. D., Portmann, R. W., Toon, O. B., Freitas, S. R., Bardeen, C. G., Brock, C., Fan, T., Gao, R., Katich, J. M., Kupc, A., Liu, S., Maloney, C., Murphy, D. M., Rosenlof, K. H., Schill, G., Schwarz, J. P., & Williamson, C. (2019). Efficient In-Cloud Removal of Aerosols by Deep Convection. Geophysical Research Letters, 46(2). https://doi.org/10.1029/2018GL080544
Yu, Pengfei, Karl D. Froyd, Robert W. Portmann, Owen B. Toon, Saulo R. Freitas, Charles G. Bardeen, and Charles Brock, et al.. "Efficient In-Cloud Removal of Aerosols by Deep Convection." Geophysical Research Letters 46, no. 2 (2019). https://doi.org/10.1029/2018GL080544.
Yu, Pengfei, et al. "Efficient In-Cloud Removal of Aerosols by Deep Convection." Geophysical Research Letters, vol. 46, no. 2, 2019. NOAA IR. https://doi.org/10.1029/2018GL080544.
Details
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Journal Title:Geophysical Research Letters
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Personal Author:Yu, Pengfei
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Froyd, Karl D.
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Portmann, Robert W.
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Toon, Owen B.
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Freitas, Saulo R.
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Bardeen, Charles G.
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Brock, Charles
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Fan, Tianyi
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Gao, Ru‐Shan
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Katich, Joseph M.
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Kupc, Agnieszka
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Liu, Shang
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Maloney, Christopher
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Murphy, Daniel M.
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Rosenlof, Karen H.
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Schill, Gregory
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Schwarz, Joshua P.
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Williamson, Christina
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NOAA Program & Office:
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Description:Convective systems dominate the vertical transport of aerosols and trace gases. The most recent in situ aerosol measurements presented here show that the concentrations of primary aerosols including sea salt and black carbon drop by factors of 10 to 10,000 from the surface to the upper troposphere. In this study we show that the default convective transport scheme in the National Science Foundation/Department of Energy Community Earth System Model results in a high bias of 10–1,000 times the measured aerosol mass for black carbon and sea salt in the middle and upper troposphere. A modified transport scheme, which considers aerosol activation from entrained air above the cloud base and aerosol‐cloud interaction associated with convection, dramatically improves model agreement with in situ measurements suggesting that deep convection can efficiently remove primary aerosols. We suggest that models that fail to consider secondary activation may overestimate black carbon's radiative forcing by a factor of 2.
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Source:Geophysical Research Letters, 46, 1061-1069.
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DOI:
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Document Type:
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Rights Information:CC BY
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Compliance:Submitted
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Download URL:
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File Type:
[PDF - 1.07 MB]
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Main Document Checksum:urn:sha-512:9012c4aa177829c0d9400aa6c963c2f90a1650d0b1f38a688a5261e292a25ed47c669cedc98343c5875031f6696cb81f3d2ec085c07aa402cdab63cfbbcd41a5
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Yu, P., Froyd, K. D., Portmann, R. W., Toon, O. B., Freitas, S. R., Bardeen, C. G., Brock, C., Fan, T., Gao, R., Katich, J. M., Kupc, A., Liu, S., Maloney, C., Murphy, D. M., Rosenlof, K. H., Schill, G., Schwarz, J. P., & Williamson, C. (2019). Efficient In-Cloud Removal of Aerosols by Deep Convection. Geophysical Research Letters, 46(2). https://doi.org/10.1029/2018GL080544
Yu, Pengfei, Karl D. Froyd, Robert W. Portmann, Owen B. Toon, Saulo R. Freitas, Charles G. Bardeen, and Charles Brock, et al.. "Efficient In-Cloud Removal of Aerosols by Deep Convection." Geophysical Research Letters 46, no. 2 (2019). https://doi.org/10.1029/2018GL080544.
Yu, Pengfei, et al. "Efficient In-Cloud Removal of Aerosols by Deep Convection." Geophysical Research Letters, vol. 46, no. 2, 2019. NOAA IR. https://doi.org/10.1029/2018GL080544.
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