Stratospheric ParticlesSource: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 005::page 910Author:Bigg, E. K.
DOI: 10.1175/1520-0469(1975)032<0910:SP>2.0.CO;2Publisher: American Meteorological Society
Abstract: Particles were collected from the stratosphere by impaction onto specially treated electron microscope screens during six balloon flights in Wyoming in 1972. The submicron diameter particles were predominantly ammonium sulfate near the tropopause and sulfuric acid at higher altitudes, though the ratio of acid to non-acid decreased rapidly with particle diameter, even at the higher altitudes. The acid particles were often, but not always, in a frozen state and aggregates joined in irregular groups were often observed near 20 km altitude. Number concentrations were usually in reasonable agreement with those found by the University of Wyoming's optical counter carried on the same flight, though conspicuously lower concentrations were found near 20 km on two occasions. This is attributed to incomplete collection of frozen aggregates. Size distributions suggested a relatively large number of particles smaller than 0.2? am diameter near the tropopause but few above about 20 km. The distribution of mass with particle diameter implies that an impactor may sometimes underestimate the total mass.
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contributor author | Bigg, E. K. | |
date accessioned | 2017-06-09T14:18:09Z | |
date available | 2017-06-09T14:18:09Z | |
date copyright | 1975/05/01 | |
date issued | 1975 | |
identifier issn | 0022-4928 | |
identifier other | ams-16813.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4152638 | |
description abstract | Particles were collected from the stratosphere by impaction onto specially treated electron microscope screens during six balloon flights in Wyoming in 1972. The submicron diameter particles were predominantly ammonium sulfate near the tropopause and sulfuric acid at higher altitudes, though the ratio of acid to non-acid decreased rapidly with particle diameter, even at the higher altitudes. The acid particles were often, but not always, in a frozen state and aggregates joined in irregular groups were often observed near 20 km altitude. Number concentrations were usually in reasonable agreement with those found by the University of Wyoming's optical counter carried on the same flight, though conspicuously lower concentrations were found near 20 km on two occasions. This is attributed to incomplete collection of frozen aggregates. Size distributions suggested a relatively large number of particles smaller than 0.2? am diameter near the tropopause but few above about 20 km. The distribution of mass with particle diameter implies that an impactor may sometimes underestimate the total mass. | |
publisher | American Meteorological Society | |
title | Stratospheric Particles | |
type | Journal Paper | |
journal volume | 32 | |
journal issue | 5 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1975)032<0910:SP>2.0.CO;2 | |
journal fristpage | 910 | |
journal lastpage | 917 | |
tree | Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 005 | |
contenttype | Fulltext |