Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution

A new scheme of droplet nucleation at cloud base is implemented into the Hebrew University Cloud Model (HUCM) with spectral (bin) microphysics. In this scheme, supersaturation maximum <i>S</i><sub><mo>max</mo></sub> near cloud base is calculated using theoreti...

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Main Authors: E. Ilotoviz, A. Khain
Format: Article
Language:English
Published: Copernicus Publications 2016-11-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/14317/2016/acp-16-14317-2016.pdf
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author E. Ilotoviz
A. Khain
author_facet E. Ilotoviz
A. Khain
author_sort E. Ilotoviz
collection DOAJ
description A new scheme of droplet nucleation at cloud base is implemented into the Hebrew University Cloud Model (HUCM) with spectral (bin) microphysics. In this scheme, supersaturation maximum <i>S</i><sub><mo>max</mo></sub> near cloud base is calculated using theoretical results according to which <i>S</i><sub><mo>max</mo></sub> ∼ <i>w</i><sup>3∕4</sup><i>N</i><sub>d</sub><sup>−1∕2</sup>, where <i>w</i> is the vertical velocity at cloud base and <i>N</i><sub>d</sub> is droplet concentration. Microphysical cloud structure obtained in the simulations of a midlatitude hail storm using the new scheme is compared with that obtained in the standard approach, in which droplet nucleation is calculated using supersaturation calculated in grid points. The simulations were performed with different concentrations of cloud condensational nuclei (CCN) and with different shapes of CCN size spectra. It is shown that the new nucleation scheme substantially improves the vertical profile of droplet concentration shifting the concentration maximum to cloud base. It is shown that the effect of the CCN size distribution shape on cloud microphysics is not less important than the effect of the total CCN concentration. It is shown that the smallest CCN with diameters less than about 0.015 µm have a substantial effect on mixed-phase and ice microphysics of deep convective clouds. Such CCN are not measured by standard CCN probes, which hinders understanding of cold microphysical processes.
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spelling doaj.art-a6f5bc6c6a3d4431a2ff395f9d9bcb642022-12-21T19:45:46ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-11-0116143171432910.5194/acp-16-14317-2016Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distributionE. Ilotoviz0A. Khain1Department of Atmospheric Sciences, The Hebrew University of Jerusalem, Jerusalem, IsraelDepartment of Atmospheric Sciences, The Hebrew University of Jerusalem, Jerusalem, IsraelA new scheme of droplet nucleation at cloud base is implemented into the Hebrew University Cloud Model (HUCM) with spectral (bin) microphysics. In this scheme, supersaturation maximum <i>S</i><sub><mo>max</mo></sub> near cloud base is calculated using theoretical results according to which <i>S</i><sub><mo>max</mo></sub> ∼ <i>w</i><sup>3∕4</sup><i>N</i><sub>d</sub><sup>−1∕2</sup>, where <i>w</i> is the vertical velocity at cloud base and <i>N</i><sub>d</sub> is droplet concentration. Microphysical cloud structure obtained in the simulations of a midlatitude hail storm using the new scheme is compared with that obtained in the standard approach, in which droplet nucleation is calculated using supersaturation calculated in grid points. The simulations were performed with different concentrations of cloud condensational nuclei (CCN) and with different shapes of CCN size spectra. It is shown that the new nucleation scheme substantially improves the vertical profile of droplet concentration shifting the concentration maximum to cloud base. It is shown that the effect of the CCN size distribution shape on cloud microphysics is not less important than the effect of the total CCN concentration. It is shown that the smallest CCN with diameters less than about 0.015 µm have a substantial effect on mixed-phase and ice microphysics of deep convective clouds. Such CCN are not measured by standard CCN probes, which hinders understanding of cold microphysical processes.https://www.atmos-chem-phys.net/16/14317/2016/acp-16-14317-2016.pdf
spellingShingle E. Ilotoviz
A. Khain
Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
Atmospheric Chemistry and Physics
title Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
title_full Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
title_fullStr Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
title_full_unstemmed Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
title_short Application of a new scheme of cloud base droplet nucleation in a spectral (bin) microphysics cloud model: sensitivity to aerosol size distribution
title_sort application of a new scheme of cloud base droplet nucleation in a spectral bin microphysics cloud model sensitivity to aerosol size distribution
url https://www.atmos-chem-phys.net/16/14317/2016/acp-16-14317-2016.pdf
work_keys_str_mv AT eilotoviz applicationofanewschemeofcloudbasedropletnucleationinaspectralbinmicrophysicscloudmodelsensitivitytoaerosolsizedistribution
AT akhain applicationofanewschemeofcloudbasedropletnucleationinaspectralbinmicrophysicscloudmodelsensitivitytoaerosolsizedistribution