Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic

Vertical and horizontal distributions of ozone, extinction due to aerosol light scattering, condensation nucleus concentrations, aerosol spectra, and meteorological parameters were measured with a NOAA WP-3D research aircraft over the Alaskan Arctic in March 1983. Multiple layers of haze, varying in...

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Bibliographic Details
Main Authors: Schnell, R. C., Raatz, W. E.
Format: Other/Unknown Material
Language:unknown
Published: 1984
Subjects:
45
Online Access:http://ntrs.nasa.gov/search.jsp?R=19840051491
id ftnasantrs:oai:casi.ntrs.nasa.gov:19840051491
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19840051491 2023-05-15T14:33:42+02:00 Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic Schnell, R. C. Raatz, W. E. Unclassified, Unlimited, Publicly available May 1, 1984 http://ntrs.nasa.gov/search.jsp?R=19840051491 unknown http://ntrs.nasa.gov/search.jsp?R=19840051491 Accession ID: 84A34278 Copyright Other Sources 45 Geophysical Research Letters; 11; 369-372 1984 ftnasantrs 2012-02-15T15:53:14Z Vertical and horizontal distributions of ozone, extinction due to aerosol light scattering, condensation nucleus concentrations, aerosol spectra, and meteorological parameters were measured with a NOAA WP-3D research aircraft over the Alaskan Arctic in March 1983. Multiple layers of haze, varying in thickness from a few 10's to 100's of meters, were observed throughout the troposphere. A maximum concentration of aerosols was located between 600 and 800 mb. Distribution of the haze layers was associated with distinct meteorological boundaries. The characteristics of the haze changed in response to stages in the progression of a major Arctic haze episode. On March 17, 1983, the Arctic anticyclone was penetrated and its meteorological and aerosol properties determined. Other/Unknown Material Arctic NASA Technical Reports Server (NTRS) Arctic
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic 45
spellingShingle 45
Schnell, R. C.
Raatz, W. E.
Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic
topic_facet 45
description Vertical and horizontal distributions of ozone, extinction due to aerosol light scattering, condensation nucleus concentrations, aerosol spectra, and meteorological parameters were measured with a NOAA WP-3D research aircraft over the Alaskan Arctic in March 1983. Multiple layers of haze, varying in thickness from a few 10's to 100's of meters, were observed throughout the troposphere. A maximum concentration of aerosols was located between 600 and 800 mb. Distribution of the haze layers was associated with distinct meteorological boundaries. The characteristics of the haze changed in response to stages in the progression of a major Arctic haze episode. On March 17, 1983, the Arctic anticyclone was penetrated and its meteorological and aerosol properties determined.
format Other/Unknown Material
author Schnell, R. C.
Raatz, W. E.
author_facet Schnell, R. C.
Raatz, W. E.
author_sort Schnell, R. C.
title Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic
title_short Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic
title_full Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic
title_fullStr Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic
title_full_unstemmed Vertical and horizontal characteristics of Arctic haze during AFASP - Alaskan Arctic
title_sort vertical and horizontal characteristics of arctic haze during afasp - alaskan arctic
publishDate 1984
url http://ntrs.nasa.gov/search.jsp?R=19840051491
op_coverage Unclassified, Unlimited, Publicly available
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Other Sources
op_relation http://ntrs.nasa.gov/search.jsp?R=19840051491
Accession ID: 84A34278
op_rights Copyright
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