Airborne Measurement of Aerosol Size Distributions Over Northern Europe

Airborne Measurement of Aerosol Size Distributions Over Northern Europe
Author: Ted S. Cress
Publisher:
Total Pages: 128
Release: 1980
Genre: Aeronautics in meteorology
ISBN:

Aerosol distributions measured with a Royco 220 particle counter over Northern Europe in Spring 1976, Fall 1976, and Summer 1977 are presented. The vertical aerosol structures were measured with an integrating nephelometer and are presented to give context to discrete aerosol size distribution and concentration measurements at altitudes near 500 m, 3000 m, and 6000 m. Analysis of aerosol data indicates that the aerosol distribution shapes at altitudes of 1.8 km and 6.0 km are very similar to distributions measured earlier over the midwestern U.S. using an impactor. Sampling analysis, and comparison to nephelometer measurements, indicate the aerosol measurements probably always represent the dry aerosol particle distribution vice the actual distribution (in balance with existing relative humidity) sensed by the nephelometer. These data provide an excellent picture of the relative changes that were found to occur in the vertical, and in space and time, with changing synoptic conditions.

Airborne Measurement of Aerosol Size Distributions Over Northern Europe. Volume 1. Spring and Fall 1976, Summer 1977

Airborne Measurement of Aerosol Size Distributions Over Northern Europe. Volume 1. Spring and Fall 1976, Summer 1977
Author:
Publisher:
Total Pages: 125
Release: 1980
Genre:
ISBN:

Aerosol distributions measured with a Royco 220 particle counter over Northern Europe in Spring 1976, Fall 1976, and Summer 1977 are presented. The vertical aerosol structures were measured with an integrating nephelometer and are presented to give context to discrete aerosol size distribution and concentration measurements at altitudes near 500 meters, 3000 meters, and 6000 meters. Analysis of aerosol data indicates that the aerosol distribution shapes at altitudes of 1.8 kilometers and 6.0 kilometers are very similar to distributions measured earlier over the midwestern U.S. using an impactor. Sampling analysis, and comparison to nephelometer measurements, indicate the aerosol measurements probably always represent the dry aerosol particle distribution vice the actual distribution (in balance with existing relative humidity) sensed by the nephelometer. These data provide an excellent picture of the relative changes that were found to occur in the vertical, and in space and time, with changing synoptic conditions.

A Review of Measured Atmospheric Optical Properties and Their Contemporary Aerosol Size Distributions

A Review of Measured Atmospheric Optical Properties and Their Contemporary Aerosol Size Distributions
Author: Richard William Johnson
Publisher:
Total Pages: 82
Release: 1981
Genre: Aerosols
ISBN:

Contents: Airborne Radiometric Measurements; Airborne Aerosol Measurements; Appendix B: Daytime Visibility and Nephelometer Measurements Related to its Determination; Appendix C: Effects of Reflection by Natural Surfaces on the Radiation Emerging from the Top of the Earth's Atmosphere; Appendix D: Measurements of Aerosol Size Distributions in the Lower Troposphere over Northern Europe.

Characteristics of Aerosol Volume Distributions Measured at Meppen, W. Germany

Characteristics of Aerosol Volume Distributions Measured at Meppen, W. Germany
Author: Bruce W. Fitch
Publisher:
Total Pages: 25
Release: 1983
Genre: Aerosols
ISBN:

Measurements of the number and size distribution of the atmospheric aerosol were made at ground level at Meppen, W. Germany using two optical particle counters. The aerosol was measured infrequently from July, 1977, through March, 1978, over the particle radius range 0.21-5.9 micrometers using a Royco model 220 particle counter. A Particle Measuring System ASAS 300B aerosol particle counter measured the aerosol over a similar radius range every hour and, often, every half-hour from 14 March through 9 May, 1978. This report discusses the behavior and characteristics of the Meppen aerosol distribution compared to an extensive set of airborne measurements of the aerosol in the lower troposphere at nine sites in Europe, including Meppen, and the use of local meteorological observations to estimate the local particle size distribution. Volume distribution plots and the results of a model fit using log-normal distributions show good agreement between the airborne and ground data sets. Both data sets show three volume modes, each well fit by a log-normal distribution. The behavior and values of the log-normal fit parameters for the accumulation and middle modes are in good agreement between the two data sets. The greater frequency of occurrence, and, generally, bigger size of the ground coarse modes compared to the airborne coarse modes indicates a larger average particle number concentration for the ground measured modes. The data show that each of the three modes is not equally affected by changes in relative humidity. The middle mode is the most sensitive and the coarse mode is the least sensitive. It appears that the relative humidity sensitive middle mode must be present for the formation of a mist or fog. (Author).