Differential absorption lidar detection of ozone in the troposphere and lower stratosphere
The DIAL technique for deriving O3 profiles from lidar measurements is discussed. Examples of a variety of O3 and aerosol measurements are presented from studies of (1) photochemically produced O3 in the summertime over the eastern United States and in biomass burning plumes during the dry season ov...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19910054102 2023-05-15T13:53:23+02:00 Differential absorption lidar detection of ozone in the troposphere and lower stratosphere Browell, E. V. Unclassified, Unlimited, Publicly available JAN 1, 1990 http://ntrs.nasa.gov/search.jsp?R=19910054102 unknown http://ntrs.nasa.gov/search.jsp?R=19910054102 Accession ID: 91A38725 Copyright Other Sources 46 1990 ftnasantrs 2012-02-15T19:02:09Z The DIAL technique for deriving O3 profiles from lidar measurements is discussed. Examples of a variety of O3 and aerosol measurements are presented from studies of (1) photochemically produced O3 in the summertime over the eastern United States and in biomass burning plumes during the dry season over the Amazon Basin of Brazil; (2) vertical O3 transport from the mixed layer into the free troposphere via cloud dynamics and from the stratosphere into the troposphere via tropopause fold events; and (3) O3 depletion in the O3 hole over Antarctica. The NASA airborne DIAL system is considered to be an advanced field system. Other/Unknown Material Antarc* Antarctica NASA Technical Reports Server (NTRS) |
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NASA Technical Reports Server (NTRS) |
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unknown |
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46 |
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46 Browell, E. V. Differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
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46 |
description |
The DIAL technique for deriving O3 profiles from lidar measurements is discussed. Examples of a variety of O3 and aerosol measurements are presented from studies of (1) photochemically produced O3 in the summertime over the eastern United States and in biomass burning plumes during the dry season over the Amazon Basin of Brazil; (2) vertical O3 transport from the mixed layer into the free troposphere via cloud dynamics and from the stratosphere into the troposphere via tropopause fold events; and (3) O3 depletion in the O3 hole over Antarctica. The NASA airborne DIAL system is considered to be an advanced field system. |
author |
Browell, E. V. |
author_facet |
Browell, E. V. |
author_sort |
Browell, E. V. |
title |
Differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
title_short |
Differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
title_full |
Differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
title_fullStr |
Differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
title_full_unstemmed |
Differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
title_sort |
differential absorption lidar detection of ozone in the troposphere and lower stratosphere |
publishDate |
1990 |
url |
http://ntrs.nasa.gov/search.jsp?R=19910054102 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19910054102 Accession ID: 91A38725 |
op_rights |
Copyright |
_version_ |
1766258433564082176 |