Aerosol Composition in the Marine and Coastal Boundary Layer

This paper focuses on aerosol composition data obtained in the North Atlantic, in the Mediterranean, in the northern Gulf of Mexico, off the coasts of California, Nova Scotia and Portugal, and on shore on Cape Cod and on the North Sea Coast of West Germany. The data show that the marine aerosol popu...

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Main Authors: Mack, E. J., Hanley, J. T., Pilie, R. J., Akers, C. K., Wattle, B. J.
Other Authors: CALSPAN ADVANCED TECHNOLOGY CENTER BUFFALO NY
Format: Text
Language:English
Published: 1981
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA107308
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA107308
id ftdtic:ADA107308
record_format openpolar
spelling ftdtic:ADA107308 2023-05-15T17:29:57+02:00 Aerosol Composition in the Marine and Coastal Boundary Layer Mack, E. J. Hanley, J. T. Pilie, R. J. Akers, C. K. Wattle, B. J. CALSPAN ADVANCED TECHNOLOGY CENTER BUFFALO NY 1981-08 text/html http://www.dtic.mil/docs/citations/ADA107308 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA107308 en eng http://www.dtic.mil/docs/citations/ADA107308 Approved for public release; distribution is unlimited. Document partially illegible. DTIC AND NTIS Atmospheric Physics *COASTAL REGIONS *AEROSOLS *ATMOSPHERIC CHEMISTRY *MARINE ATMOSPHERES ELECTROOPTICS VISIBILITY PACIFIC OCEAN NORTH ATLANTIC OCEAN WEST GERMANY MEXICO GULF PORTUGAL NORTH SEA MASSACHUSETTS HUMIDITY MEDITERRANEAN SEA CALIFORNIA NOVA SCOTIA BOUNDARY LAYER CHEMICAL COMPOSITION Text 1981 ftdtic 2016-02-22T14:10:24Z This paper focuses on aerosol composition data obtained in the North Atlantic, in the Mediterranean, in the northern Gulf of Mexico, off the coasts of California, Nova Scotia and Portugal, and on shore on Cape Cod and on the North Sea Coast of West Germany. The data show that the marine aerosol population varies considerably in composition, particularly in coastal areas, and does not necessarily comprise primarily sea salt aerosols. As a result of these compositional differences, response of the aerosol to fluctuations in relative humidity is expected to differ from one locale or airmass to another. Therefore, aerosol size spectra alone are not sufficient for the prediction of visibility or the potential performance of EO systems under changing humidity conditions. Presented at the Annual SPIE Technical Symposium (25th), v305 n20 held on 24-28 Aug 1981 at San Diego, CA. Text North Atlantic Defense Technical Information Center: DTIC Technical Reports database Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Atmospheric Physics
*COASTAL REGIONS
*AEROSOLS
*ATMOSPHERIC CHEMISTRY
*MARINE ATMOSPHERES
ELECTROOPTICS
VISIBILITY
PACIFIC OCEAN
NORTH ATLANTIC OCEAN
WEST GERMANY
MEXICO GULF
PORTUGAL
NORTH SEA
MASSACHUSETTS
HUMIDITY
MEDITERRANEAN SEA
CALIFORNIA
NOVA SCOTIA
BOUNDARY LAYER
CHEMICAL COMPOSITION
spellingShingle Atmospheric Physics
*COASTAL REGIONS
*AEROSOLS
*ATMOSPHERIC CHEMISTRY
*MARINE ATMOSPHERES
ELECTROOPTICS
VISIBILITY
PACIFIC OCEAN
NORTH ATLANTIC OCEAN
WEST GERMANY
MEXICO GULF
PORTUGAL
NORTH SEA
MASSACHUSETTS
HUMIDITY
MEDITERRANEAN SEA
CALIFORNIA
NOVA SCOTIA
BOUNDARY LAYER
CHEMICAL COMPOSITION
Mack, E. J.
Hanley, J. T.
Pilie, R. J.
Akers, C. K.
Wattle, B. J.
Aerosol Composition in the Marine and Coastal Boundary Layer
topic_facet Atmospheric Physics
*COASTAL REGIONS
*AEROSOLS
*ATMOSPHERIC CHEMISTRY
*MARINE ATMOSPHERES
ELECTROOPTICS
VISIBILITY
PACIFIC OCEAN
NORTH ATLANTIC OCEAN
WEST GERMANY
MEXICO GULF
PORTUGAL
NORTH SEA
MASSACHUSETTS
HUMIDITY
MEDITERRANEAN SEA
CALIFORNIA
NOVA SCOTIA
BOUNDARY LAYER
CHEMICAL COMPOSITION
description This paper focuses on aerosol composition data obtained in the North Atlantic, in the Mediterranean, in the northern Gulf of Mexico, off the coasts of California, Nova Scotia and Portugal, and on shore on Cape Cod and on the North Sea Coast of West Germany. The data show that the marine aerosol population varies considerably in composition, particularly in coastal areas, and does not necessarily comprise primarily sea salt aerosols. As a result of these compositional differences, response of the aerosol to fluctuations in relative humidity is expected to differ from one locale or airmass to another. Therefore, aerosol size spectra alone are not sufficient for the prediction of visibility or the potential performance of EO systems under changing humidity conditions. Presented at the Annual SPIE Technical Symposium (25th), v305 n20 held on 24-28 Aug 1981 at San Diego, CA.
author2 CALSPAN ADVANCED TECHNOLOGY CENTER BUFFALO NY
format Text
author Mack, E. J.
Hanley, J. T.
Pilie, R. J.
Akers, C. K.
Wattle, B. J.
author_facet Mack, E. J.
Hanley, J. T.
Pilie, R. J.
Akers, C. K.
Wattle, B. J.
author_sort Mack, E. J.
title Aerosol Composition in the Marine and Coastal Boundary Layer
title_short Aerosol Composition in the Marine and Coastal Boundary Layer
title_full Aerosol Composition in the Marine and Coastal Boundary Layer
title_fullStr Aerosol Composition in the Marine and Coastal Boundary Layer
title_full_unstemmed Aerosol Composition in the Marine and Coastal Boundary Layer
title_sort aerosol composition in the marine and coastal boundary layer
publishDate 1981
url http://www.dtic.mil/docs/citations/ADA107308
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA107308
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA107308
op_rights Approved for public release; distribution is unlimited. Document partially illegible.
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