Ratios of Extinction Coefficient, Mass, and Surface Area to Backscatter Coefficient and Mass to Extinction Coefficient Derived From Balloon‐Borne Stratospheric Aerosol Size Distribution Measurements From 1989–2025
Open Access
- 2 March 2026
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 131 (5)
Abstract
In situ measurements of stratospheric aerosol are the only measurements that provide sufficient detail to determine aerosol number, size, surface area, volume/mass, and effective radius; however, these measurements are limited in space and time. Remote sensing of stratospheric aerosol is both global (from satellite) and more frequent (from LiDAR), but not as detailed. The challenge is to use remote sensing data to infer geophysical quantities of interest. Here, over 35 years of in situ stratospheric aerosol measurements in the mid‐latitudes are used to derive ratios of extinction coefficient ( E ) to backscatter coefficient ( B ), mass ( m ) to backscatter coefficient, surface area ( s ) to backscatter coefficient, and mass and surface area to extinction coefficient. These ratios provide an avenue to convert remotely sensed aerosol measurements to geophysical quantities of interest. The results indicate that from 10 to 30 km m : B and m : E are nearly independent of altitude, while E : B and s : B have some altitude dependence. Still, all ratios have a nearly linear relationship in log space, independent of altitude, implying that these relationships can nearly be represented by a single value for the ratio. The results for: E : B , m : B , and m : E are 49.9, 17.6, and 0.39 for a wavelength of 532 nm. The ratios involving s cannot be represented by a single number, instead requiring an exponential relationship. More complicated dependencies in the form of exponential functions and for different altitude layers are derived for all ratios.Keywords
Funding Information
- National Aeronautics and Space Administration (80NSSC25K7182)
- National Aeronautics and Space Administration (80NSSC18K0709)
- National Aeronautics and Space Administration (80NSSC21K1198)
- National Science Foundation (1619632)
- National Science Foundation (1011827)
- National Science Foundation (0437406)
- National Science Foundation (0216558)
- Office of Naval Research
This publication has 43 references indexed in Scilit:
- Effects of Different Stratospheric SO2 Injection Altitudes on Stratospheric Chemistry and DynamicsJournal of Geophysical Research: Atmospheres, 2018
- Stratospheric Smoke With Unprecedentedly High Backscatter Observed by Lidars Above Southern FranceGeophysical Research Letters, 2018
- Stratospheric aerosol-Observations, processes, and impact on climateReviews of Geophysics, 2016
- On the accuracy of stratospheric aerosol extinction derived from in situ size distribution measurements and surface area density derived from remote SAGE II and HALOE extinction measurementsJournal of Geophysical Research: Atmospheres, 2015
- Total volcanic stratospheric aerosol optical depths and implications for global climate changeGeophysical Research Letters, 2014
- Quasi‐Lagrangian measurements of nitric acid trihydrate formation over AntarcticaJournal of Geophysical Research: Atmospheres, 2013
- Condensation nuclei measurements in the midlatitude (1982–2012) and Antarctic (1986–2010) stratosphere between 20 and 35 kmJournal of Geophysical Research: Atmospheres, 2013
- Observations of the chemical composition of stratospheric aerosol particlesQuarterly Journal of the Royal Meteorological Society, 2013
- Volcanic eruptions and climateReviews of Geophysics, 2000
- Stratospheric aerosol sulfuric acid: First direct in situ measurements using a novel balloon-based mass spectrometer apparatusJournal of Atmospheric Chemistry, 1998