alexa Determination of Kelvin Radii and Bulk Hygroscopicity of Volume Based Hygroscopicity for Atmospheric Aerosols
ISSN: 2476-2296

Fluid Mechanics: Open Access
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Research Article

Determination of Kelvin Radii and Bulk Hygroscopicity of Volume Based Hygroscopicity for Atmospheric Aerosols

Saadu B1*, Tijjani BI2 and Galadanci GSM2

1Department of Physics, Umaru Musa Yar’adua University, Katsina, Katsina state, Nigeria

2Department of Physics, Bayero University Kano, Kano state, Nigeria

*Corresponding Author:
Saadu B
Department of Physics
Umaru Musa Yar’adua University
Katsina, Katsina state, Nigeria
Tel: +2347039709888
E-mail: [email protected]

Received date: March 10, 2017; Accepted date: March 27, 2017; Published date: April 08, 2017

Citation: Saadu B, Tijjani BI, Galadanci GSM (2017) Determination of Kelvin Radii and Bulk Hygroscopicity of Volume Based Hygroscopicity for Atmospheric Aerosols. Fluid Mech Open Acc 4: 153. doi: 10.4172/2476-2296.1000153

Copyright: © 2017 Saadu B. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

 

Abstract

In this study, a volume based hygroscopicity (kv) model was applied to the data obtained from Optical Properties of Aerosol and Clouds (OPAC), the properties obtained were the radii of arctic, continental clean, continental polluted, maritime clean, maritime polluted, Sahara and urban at eight relative humidity of 0%, 50%, 70%, 80%, 90%, 95%, 98%, and 99%. The Kelvin radii (A) and bulk hygroscopicity (B) were determined using regression analysis, the result shows that B is more dominant than A for maritime clean and maritime polluted, also discovered that maritime clean and maritime polluted has higher value of kv while Saharan has lowest. We also discovered that R2 is greater than 90%, p-value and significance are less than 0.05, therefore the parameter kv is good for atmospheric modeling.

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