Nucleation and Growth of Stratospheric Aerosols

Abstract

Despite early evidence of the presence of small particles in regions above the troposphere, it was only about two decades ago that the existence of a globally distributed, temporally persistent, stratospheric aerosol layer was established. Early twilight measurements by Gruner & Kleinert and Gruner provided evidence that aerosols exist above the tropopause, but the first careful systematic direct measurements of the change in aerosol concentration with altitude were reported by Junge et al. Their in situ measurements showed the aerosol concentration to decrease monotonically up to and through the tropopause, a fact both expected and confirmed by other investigators.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1981
Accession Number
ADA103605

Entities

People

  • A. W. Castleman
  • Robert G. Keesee

Organizations

  • University of Colorado Boulder

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Atmospheric Sciences
  • Chemical Reaction Properties
  • Chemical Reactions
  • Chemical Synthesis
  • Chemistry
  • Dielectric Gases
  • Energy
  • Laser Radar
  • Partial Pressure
  • Particle Size
  • Particles
  • Physics Laboratories
  • Planetary Sciences
  • Sodium Hydroxide
  • Steady State
  • Thermodynamics
  • Vapor Pressure

Fields of Study

  • Environmental science

Readers

  • Aerosol Science/Aerosol Physics
  • Materials Science and Engineering.
  • Space/Atmospheric Physics.

Technology Areas

  • Space