Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model
Aerosol and Meteorological data from cruises in the East Pacific (CEWCOM-78) and the North Atlantic (JASIN) were used to evaluate the predictive performance of the Wells-Munn-Katz aerosol model. Under given meteorological conditions (wind speed and relative humidity), the model gave very good predic...
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ftdtic:ADA096599 2023-05-15T17:33:18+02:00 Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model Fairall, Christopher W. BDM CORP MONTEREY CA 1981-01-15 text/html http://www.dtic.mil/docs/citations/ADA096599 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA096599 en eng http://www.dtic.mil/docs/citations/ADA096599 Approved for public release; distribution is unlimited. Document partially illegible. DTIC AND NTIS Atmospheric Physics *INFRARED SPECTRA *ATMOSPHERE MODELS *AEROSOLS *METEOROLOGY *LIGHT TRANSMISSION *VISIBLE SPECTRA MARINE METEOROLOGY SEA WATER SPECTRAL ENERGY DISTRIBUTION AIR MASS ANALYSIS COEFFICIENTS GRAPHS EXTINCTION TABLES(DATA) WELLS-MUNN-KATZ MODEL Text 1981 ftdtic 2016-02-22T15:51:04Z Aerosol and Meteorological data from cruises in the East Pacific (CEWCOM-78) and the North Atlantic (JASIN) were used to evaluate the predictive performance of the Wells-Munn-Katz aerosol model. Under given meteorological conditions (wind speed and relative humidity), the model gave very good predictions of the average aerosol extinction coefficient at 10.6 micron wavelength (the standard deviation was about a factor of three). The model did not perform well when asked to predict specific aerosol extinction values. The model continental coefficient, B = 1.7, was found to be too large -- the average open ocean value should be B = 0.24. The continental coefficient was found to be important for predicting IR band extinction from visible band extinction estimates. Further analysis demonstrated that much of the variance of continental aerosol spectral density was due to air-mass history and that much of the variance of sea salt aerosol spectral density was due to changes in the marine layer mixing height. 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 *INFRARED SPECTRA *ATMOSPHERE MODELS *AEROSOLS *METEOROLOGY *LIGHT TRANSMISSION *VISIBLE SPECTRA MARINE METEOROLOGY SEA WATER SPECTRAL ENERGY DISTRIBUTION AIR MASS ANALYSIS COEFFICIENTS GRAPHS EXTINCTION TABLES(DATA) WELLS-MUNN-KATZ MODEL |
spellingShingle |
Atmospheric Physics *INFRARED SPECTRA *ATMOSPHERE MODELS *AEROSOLS *METEOROLOGY *LIGHT TRANSMISSION *VISIBLE SPECTRA MARINE METEOROLOGY SEA WATER SPECTRAL ENERGY DISTRIBUTION AIR MASS ANALYSIS COEFFICIENTS GRAPHS EXTINCTION TABLES(DATA) WELLS-MUNN-KATZ MODEL Fairall, Christopher W. Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model |
topic_facet |
Atmospheric Physics *INFRARED SPECTRA *ATMOSPHERE MODELS *AEROSOLS *METEOROLOGY *LIGHT TRANSMISSION *VISIBLE SPECTRA MARINE METEOROLOGY SEA WATER SPECTRAL ENERGY DISTRIBUTION AIR MASS ANALYSIS COEFFICIENTS GRAPHS EXTINCTION TABLES(DATA) WELLS-MUNN-KATZ MODEL |
description |
Aerosol and Meteorological data from cruises in the East Pacific (CEWCOM-78) and the North Atlantic (JASIN) were used to evaluate the predictive performance of the Wells-Munn-Katz aerosol model. Under given meteorological conditions (wind speed and relative humidity), the model gave very good predictions of the average aerosol extinction coefficient at 10.6 micron wavelength (the standard deviation was about a factor of three). The model did not perform well when asked to predict specific aerosol extinction values. The model continental coefficient, B = 1.7, was found to be too large -- the average open ocean value should be B = 0.24. The continental coefficient was found to be important for predicting IR band extinction from visible band extinction estimates. Further analysis demonstrated that much of the variance of continental aerosol spectral density was due to air-mass history and that much of the variance of sea salt aerosol spectral density was due to changes in the marine layer mixing height. |
author2 |
BDM CORP MONTEREY CA |
format |
Text |
author |
Fairall, Christopher W. |
author_facet |
Fairall, Christopher W. |
author_sort |
Fairall, Christopher W. |
title |
Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model |
title_short |
Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model |
title_full |
Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model |
title_fullStr |
Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model |
title_full_unstemmed |
Aerosol Extinction over the Ocean: A Field Evaluation of the Wells-Munn- Katz Model |
title_sort |
aerosol extinction over the ocean: a field evaluation of the wells-munn- katz model |
publishDate |
1981 |
url |
http://www.dtic.mil/docs/citations/ADA096599 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA096599 |
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/ADA096599 |
op_rights |
Approved for public release; distribution is unlimited. Document partially illegible. |
_version_ |
1766131764682555392 |