z-logo
open-access-imgOpen Access
The Truncated Geometric Approximation and the Size Distribution of Small Atmospheric Particles
Author(s) -
John DeVore
Publication year - 2011
Publication title -
journal of atmospheric and oceanic technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.774
H-Index - 124
eISSN - 1520-0426
pISSN - 0739-0572
DOI - 10.1175/2010jtecha1513.1
Subject(s) - aeronet , wavelength , extinction (optical mineralogy) , power law , physics , mie scattering , optical depth , particle size , geometrical optics , aerosol , cirrus , particle size distribution , sun photometer , optics , mathematics , meteorology , statistics , light scattering , scattering , geology , paleontology
This paper describes a simple relationship between the slope of particulate optical depth as a function of wavelength and the size distribution of spherical particles. It is based on approximating extinction using a truncated geometric optics relationship and is applicable when optical depth decreases with wavelength. The new relationship suggests that extinction versus wavelength measurements are most sensitive to particles that are comparable in size to the wavelength. When optical depth is expressed as a power-law function of wavelength, the resulting particle size distribution is also a power-law function of size, with the two exponents reproducing the well-known relationship between the Ångström and Junge exponents. Examples of applying the new relationship are shown using both numerical calculations based on Mie theory and measurements from the Aerosol Robotic Network (AERONET) sun photometer at NASA Goddard Space Flight Center (GSFC). Since the truncated geometric approximation makes no assumptions per se concerning the form of the particle size distribution, it may find application in supplementing solar aureole profile measurements in retrieving the size distributions of particles in thin clouds—for example, cirrus—or when they are present.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here